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Soil - Wikipedia

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id="toc-Composition-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Formation" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Formation"> <div class="vector-toc-text"> <span class="vector-toc-numb">3</span> <span>Formation</span> </div> </a> <ul id="toc-Formation-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Physical_properties" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Physical_properties"> <div class="vector-toc-text"> <span class="vector-toc-numb">4</span> <span>Physical properties</span> </div> </a> <ul id="toc-Physical_properties-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Soil_moisture" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Soil_moisture"> <div class="vector-toc-text"> <span class="vector-toc-numb">5</span> <span>Soil moisture</span> </div> </a> <ul id="toc-Soil_moisture-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Soil_gas" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Soil_gas"> <div class="vector-toc-text"> <span class="vector-toc-numb">6</span> <span>Soil gas</span> </div> </a> <ul id="toc-Soil_gas-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Solid_phase_(soil_matrix)" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Solid_phase_(soil_matrix)"> <div class="vector-toc-text"> <span class="vector-toc-numb">7</span> <span>Solid phase (soil matrix)</span> </div> </a> <ul id="toc-Solid_phase_(soil_matrix)-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Soil_biodiversity" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Soil_biodiversity"> <div class="vector-toc-text"> <span class="vector-toc-numb">8</span> <span>Soil biodiversity</span> </div> </a> <ul id="toc-Soil_biodiversity-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Chemistry" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Chemistry"> <div class="vector-toc-text"> <span class="vector-toc-numb">9</span> <span>Chemistry</span> </div> </a> <button aria-controls="toc-Chemistry-sublist" class="cdx-button cdx-button--weight-quiet cdx-button--icon-only vector-toc-toggle"> <span class="vector-icon mw-ui-icon-wikimedia-expand"></span> <span>Toggle Chemistry subsection</span> </button> <ul id="toc-Chemistry-sublist" class="vector-toc-list"> <li id="toc-Cation_and_anion_exchange" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Cation_and_anion_exchange"> <div class="vector-toc-text"> <span class="vector-toc-numb">9.1</span> <span>Cation and anion exchange</span> </div> </a> <ul id="toc-Cation_and_anion_exchange-sublist" class="vector-toc-list"> <li id="toc-Cation_exchange_capacity_(CEC)" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Cation_exchange_capacity_(CEC)"> <div class="vector-toc-text"> <span class="vector-toc-numb">9.1.1</span> <span>Cation exchange capacity (CEC)</span> </div> </a> <ul id="toc-Cation_exchange_capacity_(CEC)-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Anion_exchange_capacity_(AEC)" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Anion_exchange_capacity_(AEC)"> <div class="vector-toc-text"> <span class="vector-toc-numb">9.1.2</span> <span>Anion exchange capacity (AEC)</span> </div> </a> <ul id="toc-Anion_exchange_capacity_(AEC)-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Reactivity_(pH)" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Reactivity_(pH)"> <div class="vector-toc-text"> <span class="vector-toc-numb">9.2</span> <span>Reactivity (pH)</span> </div> </a> <ul id="toc-Reactivity_(pH)-sublist" class="vector-toc-list"> <li id="toc-Base_saturation_percentage" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Base_saturation_percentage"> <div class="vector-toc-text"> <span class="vector-toc-numb">9.2.1</span> <span>Base saturation percentage</span> </div> </a> <ul id="toc-Base_saturation_percentage-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Buffering" class="vector-toc-list-item vector-toc-level-3"> <a class="vector-toc-link" href="#Buffering"> <div class="vector-toc-text"> <span class="vector-toc-numb">9.2.2</span> <span>Buffering</span> </div> </a> <ul id="toc-Buffering-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Redox" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Redox"> <div class="vector-toc-text"> <span class="vector-toc-numb">9.3</span> <span>Redox</span> </div> </a> <ul id="toc-Redox-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Nutrients" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Nutrients"> <div class="vector-toc-text"> <span class="vector-toc-numb">10</span> <span>Nutrients</span> </div> </a> <ul id="toc-Nutrients-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Soil_organic_matter" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Soil_organic_matter"> <div class="vector-toc-text"> <span class="vector-toc-numb">11</span> <span>Soil organic matter</span> </div> </a> <button aria-controls="toc-Soil_organic_matter-sublist" class="cdx-button cdx-button--weight-quiet cdx-button--icon-only vector-toc-toggle"> <span class="vector-icon mw-ui-icon-wikimedia-expand"></span> <span>Toggle Soil organic matter subsection</span> </button> <ul id="toc-Soil_organic_matter-sublist" class="vector-toc-list"> <li id="toc-Humus" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Humus"> <div class="vector-toc-text"> <span class="vector-toc-numb">11.1</span> <span>Humus</span> </div> </a> <ul id="toc-Humus-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Climatological_influence" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Climatological_influence"> <div class="vector-toc-text"> <span class="vector-toc-numb">11.2</span> <span>Climatological influence</span> </div> </a> <ul id="toc-Climatological_influence-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Plant_residue" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Plant_residue"> <div class="vector-toc-text"> <span class="vector-toc-numb">11.3</span> <span>Plant residue</span> </div> </a> <ul id="toc-Plant_residue-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Horizons" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Horizons"> <div class="vector-toc-text"> <span class="vector-toc-numb">12</span> <span>Horizons</span> </div> </a> <ul id="toc-Horizons-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Classification" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Classification"> <div class="vector-toc-text"> <span class="vector-toc-numb">13</span> <span>Classification</span> </div> </a> <ul id="toc-Classification-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Uses" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Uses"> <div class="vector-toc-text"> <span class="vector-toc-numb">14</span> <span>Uses</span> </div> </a> <ul id="toc-Uses-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Degradation" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Degradation"> <div class="vector-toc-text"> <span class="vector-toc-numb">15</span> <span>Degradation</span> </div> </a> <button aria-controls="toc-Degradation-sublist" class="cdx-button cdx-button--weight-quiet cdx-button--icon-only vector-toc-toggle"> <span class="vector-icon mw-ui-icon-wikimedia-expand"></span> <span>Toggle Degradation subsection</span> </button> <ul id="toc-Degradation-sublist" class="vector-toc-list"> <li id="toc-Acidification" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Acidification"> <div class="vector-toc-text"> <span class="vector-toc-numb">15.1</span> <span>Acidification</span> </div> </a> <ul id="toc-Acidification-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Contamination" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Contamination"> <div class="vector-toc-text"> <span class="vector-toc-numb">15.2</span> <span>Contamination</span> </div> </a> <ul id="toc-Contamination-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Desertification" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Desertification"> <div class="vector-toc-text"> <span class="vector-toc-numb">15.3</span> <span>Desertification</span> </div> </a> <ul id="toc-Desertification-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Erosion" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Erosion"> <div class="vector-toc-text"> <span class="vector-toc-numb">15.4</span> <span>Erosion</span> </div> </a> <ul id="toc-Erosion-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Salination" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Salination"> <div class="vector-toc-text"> <span class="vector-toc-numb">15.5</span> <span>Salination</span> </div> </a> <ul id="toc-Salination-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Reclamation" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Reclamation"> <div class="vector-toc-text"> <span class="vector-toc-numb">16</span> <span>Reclamation</span> </div> </a> <ul id="toc-Reclamation-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-History_of_studies_and_research" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#History_of_studies_and_research"> <div class="vector-toc-text"> <span class="vector-toc-numb">17</span> <span>History of studies and research</span> </div> </a> <button aria-controls="toc-History_of_studies_and_research-sublist" class="cdx-button cdx-button--weight-quiet cdx-button--icon-only vector-toc-toggle"> <span class="vector-icon mw-ui-icon-wikimedia-expand"></span> <span>Toggle History of studies and research subsection</span> </button> <ul id="toc-History_of_studies_and_research-sublist" class="vector-toc-list"> <li id="toc-Studies_of_soil_fertility" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Studies_of_soil_fertility"> <div class="vector-toc-text"> <span class="vector-toc-numb">17.1</span> <span>Studies of soil fertility</span> </div> </a> <ul id="toc-Studies_of_soil_fertility-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Studies_of_soil_formation" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Studies_of_soil_formation"> <div class="vector-toc-text"> <span class="vector-toc-numb">17.2</span> <span>Studies of soil formation</span> </div> </a> <ul id="toc-Studies_of_soil_formation-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-See_also" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#See_also"> <div class="vector-toc-text"> <span class="vector-toc-numb">18</span> <span>See also</span> </div> </a> <ul id="toc-See_also-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-References" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#References"> <div class="vector-toc-text"> <span class="vector-toc-numb">19</span> <span>References</span> </div> </a> <ul id="toc-References-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Sources" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Sources"> <div class="vector-toc-text"> <span class="vector-toc-numb">20</span> <span>Sources</span> </div> </a> <ul id="toc-Sources-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Bibliography" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Bibliography"> <div class="vector-toc-text"> <span class="vector-toc-numb">21</span> <span>Bibliography</span> </div> </a> <ul id="toc-Bibliography-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Further_reading" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#Further_reading"> <div class="vector-toc-text"> <span class="vector-toc-numb">22</span> <span>Further reading</span> </div> </a> <ul id="toc-Further_reading-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-External_links" class="vector-toc-list-item vector-toc-level-1"> <a class="vector-toc-link" href="#External_links"> <div class="vector-toc-text"> <span class="vector-toc-numb">23</span> <span>External links</span> </div> </a> <ul id="toc-External_links-sublist" class="vector-toc-list"> </ul> </li> </ul> </div> </div> </nav> </div> </div> <div class="mw-content-container"> <main id="content" class="mw-body"> <header class="mw-body-header vector-page-titlebar"> <nav aria-label="Contents" class="vector-toc-landmark"> <div id="vector-page-titlebar-toc" class="vector-dropdown vector-page-titlebar-toc vector-button-flush-left" > <input type="checkbox" id="vector-page-titlebar-toc-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-vector-page-titlebar-toc" class="vector-dropdown-checkbox " aria-label="Toggle the table of contents" > <label id="vector-page-titlebar-toc-label" for="vector-page-titlebar-toc-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--icon-only " aria-hidden="true" ><span class="vector-icon mw-ui-icon-listBullet mw-ui-icon-wikimedia-listBullet"></span> <span class="vector-dropdown-label-text">Toggle the table of contents</span> </label> <div class="vector-dropdown-content"> <div id="vector-page-titlebar-toc-unpinned-container" class="vector-unpinned-container"> </div> </div> </div> </nav> <h1 id="firstHeading" class="firstHeading mw-first-heading"><span class="mw-page-title-main">Soil</span></h1> <div id="p-lang-btn" class="vector-dropdown mw-portlet mw-portlet-lang" > <input type="checkbox" id="p-lang-btn-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-p-lang-btn" class="vector-dropdown-checkbox mw-interlanguage-selector" aria-label="Go to an article in another language. Available in 135 languages" > <label id="p-lang-btn-label" for="p-lang-btn-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--action-progressive mw-portlet-lang-heading-135" aria-hidden="true" ><span class="vector-icon mw-ui-icon-language-progressive mw-ui-icon-wikimedia-language-progressive"></span> <span class="vector-dropdown-label-text">135 languages</span> </label> <div class="vector-dropdown-content"> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li class="interlanguage-link interwiki-af mw-list-item"><a href="https://af.wikipedia.org/wiki/Grond" title="Grond – Afrikaans" lang="af" hreflang="af" data-title="Grond" data-language-autonym="Afrikaans" data-language-local-name="Afrikaans" class="interlanguage-link-target"><span>Afrikaans</span></a></li><li class="interlanguage-link interwiki-ar mw-list-item"><a href="https://ar.wikipedia.org/wiki/%D8%AA%D8%B1%D8%A8%D8%A9" title="تربة – Arabic" lang="ar" hreflang="ar" data-title="تربة" data-language-autonym="العربية" data-language-local-name="Arabic" class="interlanguage-link-target"><span>العربية</span></a></li><li class="interlanguage-link interwiki-an mw-list-item"><a href="https://an.wikipedia.org/wiki/Suelo" title="Suelo – Aragonese" lang="an" hreflang="an" data-title="Suelo" data-language-autonym="Aragonés" data-language-local-name="Aragonese" class="interlanguage-link-target"><span>Aragonés</span></a></li><li class="interlanguage-link interwiki-roa-rup mw-list-item"><a href="https://roa-rup.wikipedia.org/wiki/Pimintu" title="Pimintu – Aromanian" lang="rup" hreflang="rup" data-title="Pimintu" data-language-autonym="Armãneashti" data-language-local-name="Aromanian" class="interlanguage-link-target"><span>Armãneashti</span></a></li><li class="interlanguage-link interwiki-as mw-list-item"><a href="https://as.wikipedia.org/wiki/%E0%A6%AE%E0%A6%BE%E0%A6%9F%E0%A6%BF" title="মাটি – Assamese" lang="as" hreflang="as" data-title="মাটি" data-language-autonym="অসমীয়া" data-language-local-name="Assamese" class="interlanguage-link-target"><span>অসমীয়া</span></a></li><li class="interlanguage-link interwiki-ast mw-list-item"><a href="https://ast.wikipedia.org/wiki/Suelu" title="Suelu – Asturian" lang="ast" hreflang="ast" data-title="Suelu" data-language-autonym="Asturianu" data-language-local-name="Asturian" class="interlanguage-link-target"><span>Asturianu</span></a></li><li class="interlanguage-link interwiki-ay mw-list-item"><a href="https://ay.wikipedia.org/wiki/Laq%27a" title="Laq&#039;a – Aymara" lang="ay" hreflang="ay" data-title="Laq&#039;a" data-language-autonym="Aymar aru" data-language-local-name="Aymara" class="interlanguage-link-target"><span>Aymar aru</span></a></li><li class="interlanguage-link interwiki-az mw-list-item"><a href="https://az.wikipedia.org/wiki/Torpaq" title="Torpaq – Azerbaijani" lang="az" hreflang="az" data-title="Torpaq" data-language-autonym="Azərbaycanca" data-language-local-name="Azerbaijani" class="interlanguage-link-target"><span>Azərbaycanca</span></a></li><li class="interlanguage-link interwiki-azb mw-list-item"><a href="https://azb.wikipedia.org/wiki/%D8%AA%D9%88%D9%BE%D8%B1%D8%A7%D9%82" title="توپراق – South Azerbaijani" lang="azb" hreflang="azb" data-title="توپراق" data-language-autonym="تۆرکجه" data-language-local-name="South Azerbaijani" class="interlanguage-link-target"><span>تۆرکجه</span></a></li><li class="interlanguage-link interwiki-bn mw-list-item"><a href="https://bn.wikipedia.org/wiki/%E0%A6%AE%E0%A6%BE%E0%A6%9F%E0%A6%BF" title="মাটি – Bangla" lang="bn" hreflang="bn" data-title="মাটি" data-language-autonym="বাংলা" data-language-local-name="Bangla" class="interlanguage-link-target"><span>বাংলা</span></a></li><li class="interlanguage-link interwiki-zh-min-nan mw-list-item"><a href="https://zh-min-nan.wikipedia.org/wiki/Th%C3%B4%CD%98" title="Thô͘ – Minnan" lang="nan" hreflang="nan" data-title="Thô͘" data-language-autonym="閩南語 / Bân-lâm-gú" data-language-local-name="Minnan" class="interlanguage-link-target"><span>閩南語 / Bân-lâm-gú</span></a></li><li class="interlanguage-link interwiki-ba mw-list-item"><a href="https://ba.wikipedia.org/wiki/%D0%A2%D1%83%D0%BF%D1%80%D0%B0%D2%A1" title="Тупраҡ – Bashkir" lang="ba" hreflang="ba" data-title="Тупраҡ" data-language-autonym="Башҡортса" data-language-local-name="Bashkir" class="interlanguage-link-target"><span>Башҡортса</span></a></li><li class="interlanguage-link interwiki-be mw-list-item"><a href="https://be.wikipedia.org/wiki/%D0%93%D0%BB%D0%B5%D0%B1%D0%B0" title="Глеба – Belarusian" lang="be" hreflang="be" data-title="Глеба" data-language-autonym="Беларуская" data-language-local-name="Belarusian" class="interlanguage-link-target"><span>Беларуская</span></a></li><li class="interlanguage-link interwiki-be-x-old mw-list-item"><a href="https://be-tarask.wikipedia.org/wiki/%D0%93%D0%BB%D0%B5%D0%B1%D0%B0" title="Глеба – Belarusian (Taraškievica orthography)" lang="be-tarask" hreflang="be-tarask" data-title="Глеба" data-language-autonym="Беларуская (тарашкевіца)" data-language-local-name="Belarusian (Taraškievica orthography)" class="interlanguage-link-target"><span>Беларуская (тарашкевіца)</span></a></li><li class="interlanguage-link interwiki-bh mw-list-item"><a href="https://bh.wikipedia.org/wiki/%E0%A4%AE%E0%A4%BE%E0%A4%9F%E0%A5%80" title="माटी – Bhojpuri" lang="bh" hreflang="bh" data-title="माटी" data-language-autonym="भोजपुरी" data-language-local-name="Bhojpuri" class="interlanguage-link-target"><span>भोजपुरी</span></a></li><li class="interlanguage-link interwiki-bcl mw-list-item"><a href="https://bcl.wikipedia.org/wiki/Daga" title="Daga – Central Bikol" lang="bcl" hreflang="bcl" data-title="Daga" data-language-autonym="Bikol Central" data-language-local-name="Central Bikol" class="interlanguage-link-target"><span>Bikol Central</span></a></li><li class="interlanguage-link interwiki-bg mw-list-item"><a href="https://bg.wikipedia.org/wiki/%D0%9F%D0%BE%D1%87%D0%B2%D0%B0" title="Почва – Bulgarian" lang="bg" hreflang="bg" data-title="Почва" data-language-autonym="Български" data-language-local-name="Bulgarian" class="interlanguage-link-target"><span>Български</span></a></li><li class="interlanguage-link interwiki-bs mw-list-item"><a href="https://bs.wikipedia.org/wiki/Tlo" title="Tlo – Bosnian" lang="bs" hreflang="bs" data-title="Tlo" data-language-autonym="Bosanski" data-language-local-name="Bosnian" class="interlanguage-link-target"><span>Bosanski</span></a></li><li class="interlanguage-link interwiki-br mw-list-item"><a href="https://br.wikipedia.org/wiki/Douar" title="Douar – Breton" lang="br" hreflang="br" data-title="Douar" data-language-autonym="Brezhoneg" data-language-local-name="Breton" class="interlanguage-link-target"><span>Brezhoneg</span></a></li><li class="interlanguage-link interwiki-ca mw-list-item"><a href="https://ca.wikipedia.org/wiki/S%C3%B2l" title="Sòl – Catalan" lang="ca" hreflang="ca" data-title="Sòl" data-language-autonym="Català" data-language-local-name="Catalan" class="interlanguage-link-target"><span>Català</span></a></li><li class="interlanguage-link interwiki-cv mw-list-item"><a href="https://cv.wikipedia.org/wiki/%D0%A2%C4%83%D0%BF%D1%80%D0%B0" title="Тăпра – Chuvash" lang="cv" hreflang="cv" data-title="Тăпра" data-language-autonym="Чӑвашла" data-language-local-name="Chuvash" class="interlanguage-link-target"><span>Чӑвашла</span></a></li><li class="interlanguage-link interwiki-cs mw-list-item"><a href="https://cs.wikipedia.org/wiki/P%C5%AFda" title="Půda – Czech" lang="cs" hreflang="cs" data-title="Půda" data-language-autonym="Čeština" data-language-local-name="Czech" class="interlanguage-link-target"><span>Čeština</span></a></li><li class="interlanguage-link interwiki-sn mw-list-item"><a href="https://sn.wikipedia.org/wiki/Dhaga" title="Dhaga – Shona" lang="sn" hreflang="sn" data-title="Dhaga" data-language-autonym="ChiShona" data-language-local-name="Shona" class="interlanguage-link-target"><span>ChiShona</span></a></li><li class="interlanguage-link interwiki-co mw-list-item"><a href="https://co.wikipedia.org/wiki/Terra" title="Terra – Corsican" lang="co" hreflang="co" data-title="Terra" data-language-autonym="Corsu" data-language-local-name="Corsican" class="interlanguage-link-target"><span>Corsu</span></a></li><li class="interlanguage-link interwiki-cy mw-list-item"><a href="https://cy.wikipedia.org/wiki/Pridd" title="Pridd – Welsh" lang="cy" hreflang="cy" data-title="Pridd" data-language-autonym="Cymraeg" data-language-local-name="Welsh" class="interlanguage-link-target"><span>Cymraeg</span></a></li><li class="interlanguage-link interwiki-da mw-list-item"><a href="https://da.wikipedia.org/wiki/Jord" title="Jord – Danish" lang="da" hreflang="da" data-title="Jord" data-language-autonym="Dansk" data-language-local-name="Danish" class="interlanguage-link-target"><span>Dansk</span></a></li><li class="interlanguage-link interwiki-de mw-list-item"><a href="https://de.wikipedia.org/wiki/Boden_(Bodenkunde)" title="Boden (Bodenkunde) – German" lang="de" hreflang="de" data-title="Boden (Bodenkunde)" data-language-autonym="Deutsch" data-language-local-name="German" class="interlanguage-link-target"><span>Deutsch</span></a></li><li class="interlanguage-link interwiki-et mw-list-item"><a href="https://et.wikipedia.org/wiki/Muld" title="Muld – Estonian" lang="et" hreflang="et" data-title="Muld" data-language-autonym="Eesti" data-language-local-name="Estonian" class="interlanguage-link-target"><span>Eesti</span></a></li><li class="interlanguage-link interwiki-el mw-list-item"><a href="https://el.wikipedia.org/wiki/%CE%88%CE%B4%CE%B1%CF%86%CE%BF%CF%82" title="Έδαφος – Greek" lang="el" hreflang="el" data-title="Έδαφος" data-language-autonym="Ελληνικά" data-language-local-name="Greek" class="interlanguage-link-target"><span>Ελληνικά</span></a></li><li class="interlanguage-link interwiki-myv mw-list-item"><a href="https://myv.wikipedia.org/wiki/%D0%9C%D0%BE%D0%B4%D0%B0" title="Мода – Erzya" lang="myv" hreflang="myv" data-title="Мода" data-language-autonym="Эрзянь" data-language-local-name="Erzya" class="interlanguage-link-target"><span>Эрзянь</span></a></li><li class="interlanguage-link interwiki-es mw-list-item"><a href="https://es.wikipedia.org/wiki/Suelo" title="Suelo – Spanish" lang="es" hreflang="es" data-title="Suelo" data-language-autonym="Español" data-language-local-name="Spanish" class="interlanguage-link-target"><span>Español</span></a></li><li class="interlanguage-link interwiki-eo mw-list-item"><a href="https://eo.wikipedia.org/wiki/Grundo" title="Grundo – Esperanto" lang="eo" hreflang="eo" data-title="Grundo" data-language-autonym="Esperanto" data-language-local-name="Esperanto" class="interlanguage-link-target"><span>Esperanto</span></a></li><li class="interlanguage-link interwiki-eu mw-list-item"><a href="https://eu.wikipedia.org/wiki/Lurzoru" title="Lurzoru – Basque" lang="eu" hreflang="eu" data-title="Lurzoru" data-language-autonym="Euskara" data-language-local-name="Basque" class="interlanguage-link-target"><span>Euskara</span></a></li><li class="interlanguage-link interwiki-fa mw-list-item"><a href="https://fa.wikipedia.org/wiki/%D8%AE%D8%A7%DA%A9" title="خاک – Persian" lang="fa" hreflang="fa" data-title="خاک" data-language-autonym="فارسی" data-language-local-name="Persian" class="interlanguage-link-target"><span>فارسی</span></a></li><li class="interlanguage-link interwiki-fr mw-list-item"><a href="https://fr.wikipedia.org/wiki/Sol_(p%C3%A9dologie)" title="Sol (pédologie) – French" lang="fr" hreflang="fr" data-title="Sol (pédologie)" data-language-autonym="Français" data-language-local-name="French" class="interlanguage-link-target"><span>Français</span></a></li><li class="interlanguage-link interwiki-fy mw-list-item"><a href="https://fy.wikipedia.org/wiki/Boaiem_(ierde)" title="Boaiem (ierde) – Western Frisian" lang="fy" hreflang="fy" data-title="Boaiem (ierde)" data-language-autonym="Frysk" data-language-local-name="Western Frisian" class="interlanguage-link-target"><span>Frysk</span></a></li><li class="interlanguage-link interwiki-ga mw-list-item"><a href="https://ga.wikipedia.org/wiki/Ithir" title="Ithir – Irish" lang="ga" hreflang="ga" data-title="Ithir" data-language-autonym="Gaeilge" data-language-local-name="Irish" class="interlanguage-link-target"><span>Gaeilge</span></a></li><li class="interlanguage-link interwiki-gd mw-list-item"><a href="https://gd.wikipedia.org/wiki/%C3%99ir" title="Ùir – Scottish Gaelic" lang="gd" hreflang="gd" data-title="Ùir" data-language-autonym="Gàidhlig" data-language-local-name="Scottish Gaelic" class="interlanguage-link-target"><span>Gàidhlig</span></a></li><li class="interlanguage-link interwiki-gl mw-list-item"><a href="https://gl.wikipedia.org/wiki/Solo" title="Solo – Galician" lang="gl" hreflang="gl" data-title="Solo" data-language-autonym="Galego" data-language-local-name="Galician" class="interlanguage-link-target"><span>Galego</span></a></li><li class="interlanguage-link interwiki-hak mw-list-item"><a href="https://hak.wikipedia.org/wiki/Th%C3%BA" title="Thú – Hakka Chinese" lang="hak" hreflang="hak" data-title="Thú" data-language-autonym="客家語 / Hak-kâ-ngî" data-language-local-name="Hakka Chinese" class="interlanguage-link-target"><span>客家語 / Hak-kâ-ngî</span></a></li><li class="interlanguage-link interwiki-ko mw-list-item"><a href="https://ko.wikipedia.org/wiki/%ED%9D%99" title="흙 – Korean" lang="ko" hreflang="ko" data-title="흙" data-language-autonym="한국어" data-language-local-name="Korean" class="interlanguage-link-target"><span>한국어</span></a></li><li class="interlanguage-link interwiki-ha mw-list-item"><a href="https://ha.wikipedia.org/wiki/%C6%98asa_(shinfidar_%C6%99asa)" title="Ƙasa (shinfidar ƙasa) – Hausa" lang="ha" hreflang="ha" data-title="Ƙasa (shinfidar ƙasa)" data-language-autonym="Hausa" data-language-local-name="Hausa" class="interlanguage-link-target"><span>Hausa</span></a></li><li class="interlanguage-link interwiki-hy mw-list-item"><a href="https://hy.wikipedia.org/wiki/%D5%80%D5%B8%D5%B2" title="Հող – Armenian" lang="hy" hreflang="hy" data-title="Հող" data-language-autonym="Հայերեն" data-language-local-name="Armenian" class="interlanguage-link-target"><span>Հայերեն</span></a></li><li class="interlanguage-link interwiki-hi mw-list-item"><a href="https://hi.wikipedia.org/wiki/%E0%A4%AE%E0%A5%83%E0%A4%A6%E0%A4%BE" title="मृदा – Hindi" lang="hi" hreflang="hi" data-title="मृदा" data-language-autonym="हिन्दी" data-language-local-name="Hindi" class="interlanguage-link-target"><span>हिन्दी</span></a></li><li class="interlanguage-link interwiki-hr mw-list-item"><a href="https://hr.wikipedia.org/wiki/Tlo" title="Tlo – Croatian" lang="hr" hreflang="hr" data-title="Tlo" data-language-autonym="Hrvatski" data-language-local-name="Croatian" class="interlanguage-link-target"><span>Hrvatski</span></a></li><li class="interlanguage-link interwiki-io mw-list-item"><a href="https://io.wikipedia.org/wiki/Sulo" title="Sulo – Ido" lang="io" hreflang="io" data-title="Sulo" data-language-autonym="Ido" data-language-local-name="Ido" class="interlanguage-link-target"><span>Ido</span></a></li><li class="interlanguage-link interwiki-id mw-list-item"><a href="https://id.wikipedia.org/wiki/Tanah" title="Tanah – Indonesian" lang="id" hreflang="id" data-title="Tanah" data-language-autonym="Bahasa Indonesia" data-language-local-name="Indonesian" class="interlanguage-link-target"><span>Bahasa Indonesia</span></a></li><li class="interlanguage-link interwiki-xh mw-list-item"><a href="https://xh.wikipedia.org/wiki/Umhlaba" title="Umhlaba – Xhosa" lang="xh" hreflang="xh" data-title="Umhlaba" data-language-autonym="IsiXhosa" data-language-local-name="Xhosa" class="interlanguage-link-target"><span>IsiXhosa</span></a></li><li class="interlanguage-link interwiki-is mw-list-item"><a href="https://is.wikipedia.org/wiki/Jar%C3%B0vegur" title="Jarðvegur – Icelandic" lang="is" hreflang="is" data-title="Jarðvegur" data-language-autonym="Íslenska" data-language-local-name="Icelandic" class="interlanguage-link-target"><span>Íslenska</span></a></li><li class="interlanguage-link interwiki-it mw-list-item"><a href="https://it.wikipedia.org/wiki/Suolo" title="Suolo – Italian" lang="it" hreflang="it" data-title="Suolo" data-language-autonym="Italiano" data-language-local-name="Italian" class="interlanguage-link-target"><span>Italiano</span></a></li><li class="interlanguage-link interwiki-he mw-list-item"><a href="https://he.wikipedia.org/wiki/%D7%A7%D7%A8%D7%A7%D7%A2" title="קרקע – Hebrew" lang="he" hreflang="he" data-title="קרקע" data-language-autonym="עברית" data-language-local-name="Hebrew" class="interlanguage-link-target"><span>עברית</span></a></li><li class="interlanguage-link interwiki-jv mw-list-item"><a href="https://jv.wikipedia.org/wiki/Lemah" title="Lemah – Javanese" lang="jv" hreflang="jv" data-title="Lemah" data-language-autonym="Jawa" data-language-local-name="Javanese" class="interlanguage-link-target"><span>Jawa</span></a></li><li class="interlanguage-link interwiki-kn mw-list-item"><a href="https://kn.wikipedia.org/wiki/%E0%B2%AE%E0%B2%A3%E0%B3%8D%E0%B2%A3%E0%B3%81" title="ಮಣ್ಣು – Kannada" lang="kn" hreflang="kn" data-title="ಮಣ್ಣು" data-language-autonym="ಕನ್ನಡ" data-language-local-name="Kannada" class="interlanguage-link-target"><span>ಕನ್ನಡ</span></a></li><li class="interlanguage-link interwiki-ka mw-list-item"><a href="https://ka.wikipedia.org/wiki/%E1%83%9C%E1%83%98%E1%83%90%E1%83%93%E1%83%90%E1%83%92%E1%83%98" title="ნიადაგი – Georgian" lang="ka" hreflang="ka" data-title="ნიადაგი" data-language-autonym="ქართული" data-language-local-name="Georgian" class="interlanguage-link-target"><span>ქართული</span></a></li><li class="interlanguage-link interwiki-kk mw-list-item"><a href="https://kk.wikipedia.org/wiki/%D0%A2%D0%BE%D0%BF%D1%8B%D1%80%D0%B0%D2%9B" title="Топырақ – Kazakh" lang="kk" hreflang="kk" data-title="Топырақ" data-language-autonym="Қазақша" data-language-local-name="Kazakh" class="interlanguage-link-target"><span>Қазақша</span></a></li><li class="interlanguage-link interwiki-sw mw-list-item"><a href="https://sw.wikipedia.org/wiki/Udongo" title="Udongo – Swahili" lang="sw" hreflang="sw" data-title="Udongo" data-language-autonym="Kiswahili" data-language-local-name="Swahili" class="interlanguage-link-target"><span>Kiswahili</span></a></li><li class="interlanguage-link interwiki-ku mw-list-item"><a href="https://ku.wikipedia.org/wiki/Ax" title="Ax – Kurdish" lang="ku" hreflang="ku" data-title="Ax" data-language-autonym="Kurdî" data-language-local-name="Kurdish" class="interlanguage-link-target"><span>Kurdî</span></a></li><li class="interlanguage-link interwiki-ky mw-list-item"><a href="https://ky.wikipedia.org/wiki/%D0%A2%D0%BE%D0%BF%D1%83%D1%80%D0%B0%D0%BA" title="Топурак – Kyrgyz" lang="ky" hreflang="ky" data-title="Топурак" data-language-autonym="Кыргызча" data-language-local-name="Kyrgyz" class="interlanguage-link-target"><span>Кыргызча</span></a></li><li class="interlanguage-link interwiki-la mw-list-item"><a href="https://la.wikipedia.org/wiki/Terra_(solum)" title="Terra (solum) – Latin" lang="la" hreflang="la" data-title="Terra (solum)" data-language-autonym="Latina" data-language-local-name="Latin" class="interlanguage-link-target"><span>Latina</span></a></li><li class="interlanguage-link interwiki-lv mw-list-item"><a href="https://lv.wikipedia.org/wiki/Augsne" title="Augsne – Latvian" lang="lv" hreflang="lv" data-title="Augsne" data-language-autonym="Latviešu" data-language-local-name="Latvian" class="interlanguage-link-target"><span>Latviešu</span></a></li><li class="interlanguage-link interwiki-lt mw-list-item"><a href="https://lt.wikipedia.org/wiki/Dirvo%C5%BEemis" title="Dirvožemis – Lithuanian" lang="lt" hreflang="lt" data-title="Dirvožemis" data-language-autonym="Lietuvių" data-language-local-name="Lithuanian" class="interlanguage-link-target"><span>Lietuvių</span></a></li><li class="interlanguage-link interwiki-li mw-list-item"><a href="https://li.wikipedia.org/wiki/Aerdbaom" title="Aerdbaom – Limburgish" lang="li" hreflang="li" data-title="Aerdbaom" data-language-autonym="Limburgs" data-language-local-name="Limburgish" class="interlanguage-link-target"><span>Limburgs</span></a></li><li class="interlanguage-link interwiki-hu mw-list-item"><a href="https://hu.wikipedia.org/wiki/Talaj" title="Talaj – Hungarian" lang="hu" hreflang="hu" data-title="Talaj" data-language-autonym="Magyar" data-language-local-name="Hungarian" class="interlanguage-link-target"><span>Magyar</span></a></li><li class="interlanguage-link interwiki-mk mw-list-item"><a href="https://mk.wikipedia.org/wiki/%D0%9F%D0%BE%D1%87%D0%B2%D0%B0" title="Почва – Macedonian" lang="mk" hreflang="mk" data-title="Почва" data-language-autonym="Македонски" data-language-local-name="Macedonian" class="interlanguage-link-target"><span>Македонски</span></a></li><li class="interlanguage-link interwiki-mg mw-list-item"><a href="https://mg.wikipedia.org/wiki/Nofon-tany" title="Nofon-tany – Malagasy" lang="mg" hreflang="mg" data-title="Nofon-tany" data-language-autonym="Malagasy" data-language-local-name="Malagasy" class="interlanguage-link-target"><span>Malagasy</span></a></li><li class="interlanguage-link interwiki-ml mw-list-item"><a href="https://ml.wikipedia.org/wiki/%E0%B4%AE%E0%B4%A3%E0%B5%8D%E0%B4%A3%E0%B5%8D" title="മണ്ണ് – Malayalam" lang="ml" hreflang="ml" data-title="മണ്ണ്" data-language-autonym="മലയാളം" data-language-local-name="Malayalam" class="interlanguage-link-target"><span>മലയാളം</span></a></li><li class="interlanguage-link interwiki-mr mw-list-item"><a href="https://mr.wikipedia.org/wiki/%E0%A4%AE%E0%A4%BE%E0%A4%A4%E0%A5%80" title="माती – Marathi" lang="mr" hreflang="mr" data-title="माती" data-language-autonym="मराठी" data-language-local-name="Marathi" class="interlanguage-link-target"><span>मराठी</span></a></li><li class="interlanguage-link interwiki-mnw mw-list-item"><a href="https://mnw.wikipedia.org/wiki/%E1%80%90%E1%80%AD" title="တိ – Mon" lang="mnw" hreflang="mnw" data-title="တိ" data-language-autonym="ဘာသာမန်" data-language-local-name="Mon" class="interlanguage-link-target"><span>ဘာသာမန်</span></a></li><li class="interlanguage-link interwiki-ms mw-list-item"><a href="https://ms.wikipedia.org/wiki/Tanah" title="Tanah – Malay" lang="ms" hreflang="ms" data-title="Tanah" data-language-autonym="Bahasa Melayu" data-language-local-name="Malay" class="interlanguage-link-target"><span>Bahasa Melayu</span></a></li><li class="interlanguage-link interwiki-min mw-list-item"><a href="https://min.wikipedia.org/wiki/Tanah" title="Tanah – Minangkabau" lang="min" hreflang="min" data-title="Tanah" data-language-autonym="Minangkabau" data-language-local-name="Minangkabau" class="interlanguage-link-target"><span>Minangkabau</span></a></li><li class="interlanguage-link interwiki-cdo mw-list-item"><a href="https://cdo.wikipedia.org/wiki/T%C3%B9" title="Tù – Mindong" lang="cdo" hreflang="cdo" data-title="Tù" data-language-autonym="閩東語 / Mìng-dĕ̤ng-ngṳ̄" data-language-local-name="Mindong" class="interlanguage-link-target"><span>閩東語 / Mìng-dĕ̤ng-ngṳ̄</span></a></li><li class="interlanguage-link interwiki-mn mw-list-item"><a href="https://mn.wikipedia.org/wiki/%D0%A5%D3%A9%D1%80%D1%81" title="Хөрс – Mongolian" lang="mn" hreflang="mn" data-title="Хөрс" data-language-autonym="Монгол" data-language-local-name="Mongolian" class="interlanguage-link-target"><span>Монгол</span></a></li><li class="interlanguage-link interwiki-nah mw-list-item"><a href="https://nah.wikipedia.org/wiki/Tlalli" title="Tlalli – Nahuatl" lang="nah" hreflang="nah" data-title="Tlalli" data-language-autonym="Nāhuatl" data-language-local-name="Nahuatl" class="interlanguage-link-target"><span>Nāhuatl</span></a></li><li class="interlanguage-link interwiki-pcm mw-list-item"><a href="https://pcm.wikipedia.org/wiki/Soil" title="Soil – Nigerian Pidgin" lang="pcm" hreflang="pcm" data-title="Soil" data-language-autonym="Naijá" data-language-local-name="Nigerian Pidgin" class="interlanguage-link-target"><span>Naijá</span></a></li><li class="interlanguage-link interwiki-fj mw-list-item"><a href="https://fj.wikipedia.org/wiki/Qele" title="Qele – Fijian" lang="fj" hreflang="fj" data-title="Qele" data-language-autonym="Na Vosa Vakaviti" data-language-local-name="Fijian" class="interlanguage-link-target"><span>Na Vosa Vakaviti</span></a></li><li class="interlanguage-link interwiki-nl mw-list-item"><a href="https://nl.wikipedia.org/wiki/Bodem" title="Bodem – Dutch" lang="nl" hreflang="nl" data-title="Bodem" data-language-autonym="Nederlands" data-language-local-name="Dutch" class="interlanguage-link-target"><span>Nederlands</span></a></li><li class="interlanguage-link interwiki-ne mw-list-item"><a href="https://ne.wikipedia.org/wiki/%E0%A4%AE%E0%A4%BE%E0%A4%9F%E0%A5%8B" title="माटो – Nepali" lang="ne" hreflang="ne" data-title="माटो" data-language-autonym="नेपाली" data-language-local-name="Nepali" class="interlanguage-link-target"><span>नेपाली</span></a></li><li class="interlanguage-link interwiki-ja mw-list-item"><a href="https://ja.wikipedia.org/wiki/%E5%9C%9F%E5%A3%8C" title="土壌 – Japanese" lang="ja" hreflang="ja" data-title="土壌" data-language-autonym="日本語" data-language-local-name="Japanese" class="interlanguage-link-target"><span>日本語</span></a></li><li class="interlanguage-link interwiki-ce mw-list-item"><a href="https://ce.wikipedia.org/wiki/%D0%9B%D0%B0%D1%82%D1%82%D0%B0" title="Латта – Chechen" lang="ce" hreflang="ce" data-title="Латта" data-language-autonym="Нохчийн" data-language-local-name="Chechen" class="interlanguage-link-target"><span>Нохчийн</span></a></li><li class="interlanguage-link interwiki-no mw-list-item"><a href="https://no.wikipedia.org/wiki/Jord" title="Jord – Norwegian Bokmål" lang="nb" hreflang="nb" data-title="Jord" data-language-autonym="Norsk bokmål" data-language-local-name="Norwegian Bokmål" class="interlanguage-link-target"><span>Norsk bokmål</span></a></li><li class="interlanguage-link interwiki-nn mw-list-item"><a href="https://nn.wikipedia.org/wiki/Jord" title="Jord – Norwegian Nynorsk" lang="nn" hreflang="nn" data-title="Jord" data-language-autonym="Norsk nynorsk" data-language-local-name="Norwegian Nynorsk" class="interlanguage-link-target"><span>Norsk nynorsk</span></a></li><li class="interlanguage-link interwiki-uz mw-list-item"><a href="https://uz.wikipedia.org/wiki/Tuproq" title="Tuproq – Uzbek" lang="uz" hreflang="uz" data-title="Tuproq" data-language-autonym="Oʻzbekcha / ўзбекча" data-language-local-name="Uzbek" class="interlanguage-link-target"><span>Oʻzbekcha / ўзбекча</span></a></li><li class="interlanguage-link interwiki-pa mw-list-item"><a href="https://pa.wikipedia.org/wiki/%E0%A8%AE%E0%A8%BF%E0%A9%B1%E0%A8%9F%E0%A9%80" title="ਮਿੱਟੀ – Punjabi" lang="pa" hreflang="pa" data-title="ਮਿੱਟੀ" data-language-autonym="ਪੰਜਾਬੀ" data-language-local-name="Punjabi" class="interlanguage-link-target"><span>ਪੰਜਾਬੀ</span></a></li><li class="interlanguage-link interwiki-pnb mw-list-item"><a href="https://pnb.wikipedia.org/wiki/%D9%85%D9%B9%DB%8C" title="مٹی – Western Punjabi" lang="pnb" hreflang="pnb" data-title="مٹی" data-language-autonym="پنجابی" data-language-local-name="Western Punjabi" class="interlanguage-link-target"><span>پنجابی</span></a></li><li class="interlanguage-link interwiki-ps mw-list-item"><a href="https://ps.wikipedia.org/wiki/%D8%AE%D8%A7%D9%88%D8%B1%D9%87" title="خاوره – Pashto" lang="ps" hreflang="ps" data-title="خاوره" data-language-autonym="پښتو" data-language-local-name="Pashto" class="interlanguage-link-target"><span>پښتو</span></a></li><li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Gleba" title="Gleba – Polish" lang="pl" hreflang="pl" data-title="Gleba" data-language-autonym="Polski" data-language-local-name="Polish" class="interlanguage-link-target"><span>Polski</span></a></li><li class="interlanguage-link interwiki-pt mw-list-item"><a href="https://pt.wikipedia.org/wiki/Solo" title="Solo – Portuguese" lang="pt" hreflang="pt" data-title="Solo" data-language-autonym="Português" data-language-local-name="Portuguese" class="interlanguage-link-target"><span>Português</span></a></li><li class="interlanguage-link interwiki-ro mw-list-item"><a href="https://ro.wikipedia.org/wiki/Sol_(strat_al_P%C4%83m%C3%A2ntului)" title="Sol (strat al Pământului) – Romanian" lang="ro" hreflang="ro" data-title="Sol (strat al Pământului)" data-language-autonym="Română" data-language-local-name="Romanian" class="interlanguage-link-target"><span>Română</span></a></li><li class="interlanguage-link interwiki-rm mw-list-item"><a href="https://rm.wikipedia.org/wiki/Terren" title="Terren – Romansh" lang="rm" hreflang="rm" data-title="Terren" data-language-autonym="Rumantsch" data-language-local-name="Romansh" class="interlanguage-link-target"><span>Rumantsch</span></a></li><li class="interlanguage-link interwiki-qu mw-list-item"><a href="https://qu.wikipedia.org/wiki/Allpa" title="Allpa – Quechua" lang="qu" hreflang="qu" data-title="Allpa" data-language-autonym="Runa Simi" data-language-local-name="Quechua" class="interlanguage-link-target"><span>Runa Simi</span></a></li><li class="interlanguage-link interwiki-ru mw-list-item"><a href="https://ru.wikipedia.org/wiki/%D0%9F%D0%BE%D1%87%D0%B2%D0%B0" title="Почва – Russian" lang="ru" hreflang="ru" data-title="Почва" data-language-autonym="Русский" data-language-local-name="Russian" class="interlanguage-link-target"><span>Русский</span></a></li><li class="interlanguage-link interwiki-sah mw-list-item"><a href="https://sah.wikipedia.org/wiki/%D0%91%D1%83%D0%BE%D1%80" title="Буор – Yakut" lang="sah" hreflang="sah" data-title="Буор" data-language-autonym="Саха тыла" data-language-local-name="Yakut" class="interlanguage-link-target"><span>Саха тыла</span></a></li><li class="interlanguage-link interwiki-szy mw-list-item"><a href="https://szy.wikipedia.org/wiki/lala%27" title="lala&#039; – Sakizaya" lang="szy" hreflang="szy" data-title="lala&#039;" data-language-autonym="Sakizaya" data-language-local-name="Sakizaya" class="interlanguage-link-target"><span>Sakizaya</span></a></li><li class="interlanguage-link interwiki-sat mw-list-item"><a href="https://sat.wikipedia.org/wiki/%E1%B1%A6%E1%B1%9F%E1%B1%A5%E1%B1%9F" title="ᱦᱟᱥᱟ – Santali" lang="sat" hreflang="sat" data-title="ᱦᱟᱥᱟ" data-language-autonym="ᱥᱟᱱᱛᱟᱲᱤ" data-language-local-name="Santali" class="interlanguage-link-target"><span>ᱥᱟᱱᱛᱟᱲᱤ</span></a></li><li class="interlanguage-link interwiki-sco mw-list-item"><a href="https://sco.wikipedia.org/wiki/Syle" title="Syle – Scots" lang="sco" hreflang="sco" data-title="Syle" data-language-autonym="Scots" data-language-local-name="Scots" class="interlanguage-link-target"><span>Scots</span></a></li><li class="interlanguage-link interwiki-sq mw-list-item"><a href="https://sq.wikipedia.org/wiki/Dheu" title="Dheu – Albanian" lang="sq" hreflang="sq" data-title="Dheu" data-language-autonym="Shqip" data-language-local-name="Albanian" class="interlanguage-link-target"><span>Shqip</span></a></li><li class="interlanguage-link interwiki-scn mw-list-item"><a href="https://scn.wikipedia.org/wiki/Tirrinu" title="Tirrinu – Sicilian" lang="scn" hreflang="scn" data-title="Tirrinu" data-language-autonym="Sicilianu" data-language-local-name="Sicilian" class="interlanguage-link-target"><span>Sicilianu</span></a></li><li class="interlanguage-link interwiki-simple mw-list-item"><a href="https://simple.wikipedia.org/wiki/Soil" title="Soil – Simple English" lang="en-simple" hreflang="en-simple" data-title="Soil" data-language-autonym="Simple English" data-language-local-name="Simple English" class="interlanguage-link-target"><span>Simple English</span></a></li><li class="interlanguage-link interwiki-sd mw-list-item"><a href="https://sd.wikipedia.org/wiki/%D9%85%D9%BD%D9%8A" title="مٽي – Sindhi" lang="sd" hreflang="sd" data-title="مٽي" data-language-autonym="سنڌي" data-language-local-name="Sindhi" class="interlanguage-link-target"><span>سنڌي</span></a></li><li class="interlanguage-link interwiki-sk mw-list-item"><a href="https://sk.wikipedia.org/wiki/P%C3%B4da" title="Pôda – Slovak" lang="sk" hreflang="sk" data-title="Pôda" data-language-autonym="Slovenčina" data-language-local-name="Slovak" class="interlanguage-link-target"><span>Slovenčina</span></a></li><li class="interlanguage-link interwiki-sl mw-list-item"><a href="https://sl.wikipedia.org/wiki/Prst_(pedologija)" title="Prst (pedologija) – Slovenian" lang="sl" hreflang="sl" data-title="Prst (pedologija)" data-language-autonym="Slovenščina" data-language-local-name="Slovenian" class="interlanguage-link-target"><span>Slovenščina</span></a></li><li class="interlanguage-link interwiki-ckb mw-list-item"><a href="https://ckb.wikipedia.org/wiki/%D8%AE%DB%86%DA%B5" title="خۆڵ – Central Kurdish" lang="ckb" hreflang="ckb" data-title="خۆڵ" data-language-autonym="کوردی" data-language-local-name="Central Kurdish" class="interlanguage-link-target"><span>کوردی</span></a></li><li class="interlanguage-link interwiki-sr mw-list-item"><a href="https://sr.wikipedia.org/wiki/%D0%A2%D0%BB%D0%BE" title="Тло – Serbian" lang="sr" hreflang="sr" data-title="Тло" data-language-autonym="Српски / srpski" data-language-local-name="Serbian" class="interlanguage-link-target"><span>Српски / srpski</span></a></li><li class="interlanguage-link interwiki-sh mw-list-item"><a href="https://sh.wikipedia.org/wiki/Tlo" title="Tlo – Serbo-Croatian" lang="sh" hreflang="sh" data-title="Tlo" data-language-autonym="Srpskohrvatski / српскохрватски" data-language-local-name="Serbo-Croatian" class="interlanguage-link-target"><span>Srpskohrvatski / српскохрватски</span></a></li><li class="interlanguage-link interwiki-su mw-list-item"><a href="https://su.wikipedia.org/wiki/Taneuh" title="Taneuh – Sundanese" lang="su" hreflang="su" data-title="Taneuh" data-language-autonym="Sunda" data-language-local-name="Sundanese" class="interlanguage-link-target"><span>Sunda</span></a></li><li class="interlanguage-link interwiki-fi mw-list-item"><a href="https://fi.wikipedia.org/wiki/Maaper%C3%A4" title="Maaperä – Finnish" lang="fi" hreflang="fi" data-title="Maaperä" data-language-autonym="Suomi" data-language-local-name="Finnish" class="interlanguage-link-target"><span>Suomi</span></a></li><li class="interlanguage-link interwiki-sv mw-list-item"><a href="https://sv.wikipedia.org/wiki/Jord" title="Jord – Swedish" lang="sv" hreflang="sv" data-title="Jord" data-language-autonym="Svenska" data-language-local-name="Swedish" class="interlanguage-link-target"><span>Svenska</span></a></li><li class="interlanguage-link interwiki-tl mw-list-item"><a href="https://tl.wikipedia.org/wiki/Lupa" title="Lupa – Tagalog" lang="tl" hreflang="tl" data-title="Lupa" data-language-autonym="Tagalog" data-language-local-name="Tagalog" class="interlanguage-link-target"><span>Tagalog</span></a></li><li class="interlanguage-link interwiki-ta mw-list-item"><a href="https://ta.wikipedia.org/wiki/%E0%AE%AE%E0%AE%A3%E0%AF%8D" title="மண் – Tamil" lang="ta" hreflang="ta" data-title="மண்" data-language-autonym="தமிழ்" data-language-local-name="Tamil" class="interlanguage-link-target"><span>தமிழ்</span></a></li><li class="interlanguage-link interwiki-shi mw-list-item"><a href="https://shi.wikipedia.org/wiki/Akal" title="Akal – Tachelhit" lang="shi" hreflang="shi" data-title="Akal" data-language-autonym="Taclḥit" data-language-local-name="Tachelhit" class="interlanguage-link-target"><span>Taclḥit</span></a></li><li class="interlanguage-link interwiki-kab mw-list-item"><a href="https://kab.wikipedia.org/wiki/Akal_(tasnakalt)" title="Akal (tasnakalt) – Kabyle" lang="kab" hreflang="kab" data-title="Akal (tasnakalt)" data-language-autonym="Taqbaylit" data-language-local-name="Kabyle" class="interlanguage-link-target"><span>Taqbaylit</span></a></li><li class="interlanguage-link interwiki-tt mw-list-item"><a href="https://tt.wikipedia.org/wiki/%D0%A2%D1%83%D1%84%D1%80%D0%B0%D0%BA" title="Туфрак – Tatar" lang="tt" hreflang="tt" data-title="Туфрак" data-language-autonym="Татарча / tatarça" data-language-local-name="Tatar" class="interlanguage-link-target"><span>Татарча / tatarça</span></a></li><li class="interlanguage-link interwiki-tay mw-list-item"><a href="https://tay.wikipedia.org/wiki/rhzyal(%E5%9C%9F%E5%9C%B0)" title="rhzyal(土地) – Tayal" lang="tay" hreflang="tay" data-title="rhzyal(土地)" data-language-autonym="Tayal" data-language-local-name="Tayal" class="interlanguage-link-target"><span>Tayal</span></a></li><li class="interlanguage-link interwiki-te mw-list-item"><a href="https://te.wikipedia.org/wiki/%E0%B0%AE%E0%B0%9F%E0%B1%8D%E0%B0%9F%E0%B0%BF" title="మట్టి – Telugu" lang="te" hreflang="te" data-title="మట్టి" data-language-autonym="తెలుగు" data-language-local-name="Telugu" class="interlanguage-link-target"><span>తెలుగు</span></a></li><li class="interlanguage-link interwiki-th mw-list-item"><a href="https://th.wikipedia.org/wiki/%E0%B8%94%E0%B8%B4%E0%B8%99" title="ดิน – Thai" lang="th" hreflang="th" data-title="ดิน" data-language-autonym="ไทย" data-language-local-name="Thai" class="interlanguage-link-target"><span>ไทย</span></a></li><li class="interlanguage-link interwiki-tg mw-list-item"><a href="https://tg.wikipedia.org/wiki/%D0%A5%D0%BE%D0%BA" title="Хок – Tajik" lang="tg" hreflang="tg" data-title="Хок" data-language-autonym="Тоҷикӣ" data-language-local-name="Tajik" class="interlanguage-link-target"><span>Тоҷикӣ</span></a></li><li class="interlanguage-link interwiki-to mw-list-item"><a href="https://to.wikipedia.org/wiki/Kelekele" title="Kelekele – Tongan" lang="to" hreflang="to" data-title="Kelekele" data-language-autonym="Lea faka-Tonga" data-language-local-name="Tongan" class="interlanguage-link-target"><span>Lea faka-Tonga</span></a></li><li class="interlanguage-link interwiki-tcy mw-list-item"><a href="https://tcy.wikipedia.org/wiki/%E0%B2%AE%E0%B2%A3%E0%B3%8D%E0%B2%A3%E0%B3%8D" title="ಮಣ್ಣ್ – Tulu" lang="tcy" hreflang="tcy" data-title="ಮಣ್ಣ್" data-language-autonym="ತುಳು" data-language-local-name="Tulu" class="interlanguage-link-target"><span>ತುಳು</span></a></li><li class="interlanguage-link interwiki-tr mw-list-item"><a href="https://tr.wikipedia.org/wiki/Toprak" title="Toprak – Turkish" lang="tr" hreflang="tr" data-title="Toprak" data-language-autonym="Türkçe" data-language-local-name="Turkish" class="interlanguage-link-target"><span>Türkçe</span></a></li><li class="interlanguage-link interwiki-uk mw-list-item"><a href="https://uk.wikipedia.org/wiki/%D2%90%D1%80%D1%83%D0%BD%D1%82" title="Ґрунт – Ukrainian" lang="uk" hreflang="uk" data-title="Ґрунт" data-language-autonym="Українська" data-language-local-name="Ukrainian" class="interlanguage-link-target"><span>Українська</span></a></li><li class="interlanguage-link interwiki-ur mw-list-item"><a href="https://ur.wikipedia.org/wiki/%D9%85%D9%B9%DB%8C" title="مٹی – Urdu" lang="ur" hreflang="ur" data-title="مٹی" data-language-autonym="اردو" data-language-local-name="Urdu" class="interlanguage-link-target"><span>اردو</span></a></li><li class="interlanguage-link interwiki-ug mw-list-item"><a href="https://ug.wikipedia.org/wiki/%D8%AA%DB%87%D9%BE%D8%B1%D8%A7%D9%82" title="تۇپراق – Uyghur" lang="ug" hreflang="ug" data-title="تۇپراق" data-language-autonym="ئۇيغۇرچە / Uyghurche" data-language-local-name="Uyghur" class="interlanguage-link-target"><span>ئۇيغۇرچە / Uyghurche</span></a></li><li class="interlanguage-link interwiki-za mw-list-item"><a href="https://za.wikipedia.org/wiki/Namh" title="Namh – Zhuang" lang="za" hreflang="za" data-title="Namh" data-language-autonym="Vahcuengh" data-language-local-name="Zhuang" class="interlanguage-link-target"><span>Vahcuengh</span></a></li><li class="interlanguage-link interwiki-vep mw-list-item"><a href="https://vep.wikipedia.org/wiki/Mahuz" title="Mahuz – Veps" lang="vep" hreflang="vep" data-title="Mahuz" data-language-autonym="Vepsän kel’" data-language-local-name="Veps" class="interlanguage-link-target"><span>Vepsän kel’</span></a></li><li class="interlanguage-link interwiki-vi mw-list-item"><a href="https://vi.wikipedia.org/wiki/%C4%90%E1%BA%A5t" title="Đất – Vietnamese" lang="vi" hreflang="vi" data-title="Đất" data-language-autonym="Tiếng Việt" data-language-local-name="Vietnamese" class="interlanguage-link-target"><span>Tiếng Việt</span></a></li><li class="interlanguage-link interwiki-vls mw-list-item"><a href="https://vls.wikipedia.org/wiki/Eirde_(ground)" title="Eirde (ground) – West Flemish" lang="vls" hreflang="vls" data-title="Eirde (ground)" data-language-autonym="West-Vlams" data-language-local-name="West Flemish" class="interlanguage-link-target"><span>West-Vlams</span></a></li><li class="interlanguage-link interwiki-war mw-list-item"><a href="https://war.wikipedia.org/wiki/Tuna" title="Tuna – Waray" lang="war" hreflang="war" data-title="Tuna" data-language-autonym="Winaray" data-language-local-name="Waray" class="interlanguage-link-target"><span>Winaray</span></a></li><li class="interlanguage-link interwiki-wuu mw-list-item"><a href="https://wuu.wikipedia.org/wiki/%E5%A0%87%E6%B3%A5" title="堇泥 – Wu" lang="wuu" hreflang="wuu" data-title="堇泥" data-language-autonym="吴语" data-language-local-name="Wu" class="interlanguage-link-target"><span>吴语</span></a></li><li class="interlanguage-link interwiki-yi mw-list-item"><a href="https://yi.wikipedia.org/wiki/%D7%91%D7%90%D7%93%D7%9F" title="באדן – Yiddish" lang="yi" hreflang="yi" data-title="באדן" data-language-autonym="ייִדיש" data-language-local-name="Yiddish" class="interlanguage-link-target"><span>ייִדיש</span></a></li><li class="interlanguage-link interwiki-zh-yue mw-list-item"><a href="https://zh-yue.wikipedia.org/wiki/%E6%B3%A5%E5%9C%9F" title="泥土 – Cantonese" lang="yue" hreflang="yue" data-title="泥土" data-language-autonym="粵語" data-language-local-name="Cantonese" class="interlanguage-link-target"><span>粵語</span></a></li><li class="interlanguage-link interwiki-bat-smg mw-list-item"><a href="https://bat-smg.wikipedia.org/wiki/D%C4%97rva" title="Dėrva – Samogitian" lang="sgs" hreflang="sgs" data-title="Dėrva" data-language-autonym="Žemaitėška" data-language-local-name="Samogitian" class="interlanguage-link-target"><span>Žemaitėška</span></a></li><li class="interlanguage-link interwiki-zh mw-list-item"><a href="https://zh.wikipedia.org/wiki/%E5%9C%9F%E5%A3%A4" title="土壤 – Chinese" lang="zh" hreflang="zh" data-title="土壤" data-language-autonym="中文" data-language-local-name="Chinese" class="interlanguage-link-target"><span>中文</span></a></li><li class="interlanguage-link interwiki-bbc mw-list-item"><a href="https://bbc.wikipedia.org/wiki/Tano" title="Tano – Batak Toba" lang="bbc" hreflang="bbc" data-title="Tano" data-language-autonym="Batak Toba" data-language-local-name="Batak Toba" class="interlanguage-link-target"><span>Batak Toba</span></a></li><li class="interlanguage-link interwiki-bew mw-list-item"><a href="https://bew.wikipedia.org/wiki/Tana" title="Tana – Betawi" lang="bew" hreflang="bew" data-title="Tana" data-language-autonym="Betawi" data-language-local-name="Betawi" class="interlanguage-link-target"><span>Betawi</span></a></li><li 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div.hatnote{padding-left:1.6em;margin-bottom:0.5em}.mw-parser-output .hatnote i{font-style:normal}.mw-parser-output .hatnote+link+.hatnote{margin-top:-0.5em}@media print{body.ns-0 .mw-parser-output .hatnote{display:none!important}}</style><div role="note" class="hatnote navigation-not-searchable">For other uses, see <a href="/wiki/Soil_(disambiguation)" class="mw-disambig" title="Soil (disambiguation)">Soil (disambiguation)</a>.</div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Stagnogley.JPG" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/4/46/Stagnogley.JPG/330px-Stagnogley.JPG" decoding="async" width="330" height="257" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/4/46/Stagnogley.JPG/495px-Stagnogley.JPG 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/4/46/Stagnogley.JPG/660px-Stagnogley.JPG 2x" data-file-width="1511" data-file-height="1179" /></a><figcaption>Surface-water-<a href="/wiki/Gley_soil" class="mw-redirect" title="Gley soil">gley</a> developed in <a href="/wiki/Glacial_till" class="mw-redirect" title="Glacial till">glacial till</a> in <a href="/wiki/Northern_Ireland" title="Northern Ireland">Northern Ireland</a></figcaption></figure> <p><b>Soil</b>, also commonly referred to as <b>earth</b>, is a <a href="/wiki/Mixture" title="Mixture">mixture</a> of <a href="/wiki/Organic_matter" title="Organic matter">organic matter</a>, <a href="/wiki/Minerals" class="mw-redirect" title="Minerals">minerals</a>, <a href="/wiki/Gas" title="Gas">gases</a>, <a href="/wiki/Liquid" title="Liquid">liquids</a>, and <a href="/wiki/Organism" title="Organism">organisms</a> that together support the <a href="/wiki/Life" title="Life">life</a> of <a href="/wiki/Plant" title="Plant">plants</a> and <a href="/wiki/Soil_biology" title="Soil biology">soil organisms</a>. Some scientific definitions distinguish <a href="/wiki/Dirt" title="Dirt">dirt</a> from <i>soil</i> by restricting the former term specifically to displaced soil. </p> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:EAgronom_4okt2023_L-1120.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/a/a8/EAgronom_4okt2023_L-1120.jpg/220px-EAgronom_4okt2023_L-1120.jpg" decoding="async" width="220" height="330" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/a/a8/EAgronom_4okt2023_L-1120.jpg/330px-EAgronom_4okt2023_L-1120.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/a/a8/EAgronom_4okt2023_L-1120.jpg/440px-EAgronom_4okt2023_L-1120.jpg 2x" data-file-width="4367" data-file-height="6550" /></a><figcaption>Soil measuring and surveying device</figcaption></figure> <p>Soil consists of a solid phase of minerals and organic matter (the soil matrix), as well as a <a href="/wiki/Porosity" title="Porosity">porous</a> phase that holds <a href="/wiki/Soil_gas" title="Soil gas">gases</a> (the soil atmosphere) and <a href="/wiki/Water" title="Water">water</a> (the soil solution).<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">&#91;</span>1<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-2" class="reference"><a href="#cite_note-2"><span class="cite-bracket">&#91;</span>2<span class="cite-bracket">&#93;</span></a></sup> Accordingly, soil is a three-<a href="/wiki/State_of_matter" title="State of matter">state</a> system of solids, liquids, and gases.<sup id="cite_ref-3" class="reference"><a href="#cite_note-3"><span class="cite-bracket">&#91;</span>3<span class="cite-bracket">&#93;</span></a></sup> Soil is a product of several factors: the influence of <a href="/wiki/Climate" title="Climate">climate</a>, <a href="/wiki/Terrain" title="Terrain">relief</a> (elevation, orientation, and slope of terrain), organisms, and the soil's <a href="/wiki/Parent_material" title="Parent material">parent materials</a> (original minerals) interacting over time.<sup id="cite_ref-Gilluly1975_4-0" class="reference"><a href="#cite_note-Gilluly1975-4"><span class="cite-bracket">&#91;</span>4<span class="cite-bracket">&#93;</span></a></sup> It continually undergoes development by way of numerous physical, chemical and biological processes, which include <a href="/wiki/Weathering" title="Weathering">weathering</a> with associated <a href="/wiki/Erosion" title="Erosion">erosion</a>.<sup id="cite_ref-5" class="reference"><a href="#cite_note-5"><span class="cite-bracket">&#91;</span>5<span class="cite-bracket">&#93;</span></a></sup> Given its complexity and strong internal <a href="/wiki/Connectedness" title="Connectedness">connectedness</a>, <a href="/wiki/Soil_ecology" title="Soil ecology">soil ecologists</a> regard soil as an <a href="/wiki/Ecosystem" title="Ecosystem">ecosystem</a>.<sup id="cite_ref-6" class="reference"><a href="#cite_note-6"><span class="cite-bracket">&#91;</span>6<span class="cite-bracket">&#93;</span></a></sup> </p><p>Most soils have a dry <a href="/wiki/Bulk_density" title="Bulk density">bulk density</a> (density of soil taking into account voids when dry) between 1.1 and 1.6&#160;g/cm<sup>3</sup>, though the soil <a href="/wiki/Particle_density_(packed_density)" class="mw-redirect" title="Particle density (packed density)">particle density</a> is much higher, in the range of 2.6 to 2.7&#160;g/cm<sup>3</sup>.<sup id="cite_ref-Yu2015_7-0" class="reference"><a href="#cite_note-Yu2015-7"><span class="cite-bracket">&#91;</span>7<span class="cite-bracket">&#93;</span></a></sup> Little of the soil of <a href="/wiki/Planet_Earth" class="mw-redirect" title="Planet Earth">planet Earth</a> is older than the <a href="/wiki/Pleistocene" title="Pleistocene">Pleistocene</a> and none is older than the <a href="/wiki/Cenozoic" title="Cenozoic">Cenozoic</a>,<sup id="cite_ref-Buol_8-0" class="reference"><a href="#cite_note-Buol-8"><span class="cite-bracket">&#91;</span>8<span class="cite-bracket">&#93;</span></a></sup> although <a href="/wiki/Paleopedological_record" title="Paleopedological record">fossilized soils</a> are preserved from as far back as the <a href="/wiki/Archean" title="Archean">Archean</a>.<sup id="cite_ref-9" class="reference"><a href="#cite_note-9"><span class="cite-bracket">&#91;</span>9<span class="cite-bracket">&#93;</span></a></sup> </p><p>Collectively the Earth's body of soil is called the <a href="/wiki/Pedosphere" title="Pedosphere">pedosphere</a>. The pedosphere interfaces with the <a href="/wiki/Lithosphere" title="Lithosphere">lithosphere</a>, the <a href="/wiki/Hydrosphere" title="Hydrosphere">hydrosphere</a>, the <a href="/wiki/Atmosphere" title="Atmosphere">atmosphere</a>, and the <a href="/wiki/Biosphere" title="Biosphere">biosphere</a>.<sup id="cite_ref-ches_10-0" class="reference"><a href="#cite_note-ches-10"><span class="cite-bracket">&#91;</span>10<span class="cite-bracket">&#93;</span></a></sup> Soil has four important <a href="/wiki/Soil_functions" title="Soil functions">functions</a>: </p> <ul><li>as a medium for plant growth</li> <li>as a means of <a href="/wiki/Water_storage" title="Water storage">water storage</a>, supply, and purification</li> <li>as a modifier of <a href="/wiki/Atmosphere_of_Earth" title="Atmosphere of Earth">Earth's atmosphere</a></li> <li>as a habitat for organisms</li></ul> <p>All of these functions, in their turn, modify the soil and its properties. </p><p><a href="/wiki/Soil_science" title="Soil science">Soil science</a> has two basic branches of study: <a href="/wiki/Edaphology" title="Edaphology">edaphology</a> and <a href="/wiki/Pedology" title="Pedology">pedology</a>. <i>Edaphology</i> studies the influence of soils on living things.<sup id="cite_ref-11" class="reference"><a href="#cite_note-11"><span class="cite-bracket">&#91;</span>11<span class="cite-bracket">&#93;</span></a></sup> <i>Pedology</i> focuses on the formation, description (morphology), and classification of soils in their natural environment.<sup id="cite_ref-12" class="reference"><a href="#cite_note-12"><span class="cite-bracket">&#91;</span>12<span class="cite-bracket">&#93;</span></a></sup> In engineering terms, soil is included in the broader concept of <a href="/wiki/Regolith" title="Regolith">regolith</a>, which also includes other loose material that lies above the bedrock, as can be found on the <a href="/wiki/Moon" title="Moon">Moon</a> and other <a href="/wiki/Astronomical_object" title="Astronomical object">celestial objects</a>.<sup id="cite_ref-13" class="reference"><a href="#cite_note-13"><span class="cite-bracket">&#91;</span>13<span class="cite-bracket">&#93;</span></a></sup> </p> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Processes">Processes</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=1" title="Edit section: Processes"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Soil is a major component of the <a href="/wiki/Earth" title="Earth">Earth</a>'s <a href="/wiki/Ecosystem" title="Ecosystem">ecosystem</a>. The world's ecosystems are impacted in far-reaching ways by the processes carried out in the soil, with effects ranging from <a href="/wiki/Ozone_depletion" title="Ozone depletion">ozone depletion</a> and <a href="/wiki/Global_warming" class="mw-redirect" title="Global warming">global warming</a> to <a href="/wiki/Rainforest_destruction" class="mw-redirect" title="Rainforest destruction">rainforest destruction</a> and <a href="/wiki/Water_pollution" title="Water pollution">water pollution</a>. With respect to Earth's <a href="/wiki/Carbon_cycle" title="Carbon cycle">carbon cycle</a>, soil acts as an important <a href="/wiki/Carbon_sink" title="Carbon sink">carbon reservoir</a>,<sup id="cite_ref-14" class="reference"><a href="#cite_note-14"><span class="cite-bracket">&#91;</span>14<span class="cite-bracket">&#93;</span></a></sup> and it is potentially one of the most reactive to human disturbance<sup id="cite_ref-15" class="reference"><a href="#cite_note-15"><span class="cite-bracket">&#91;</span>15<span class="cite-bracket">&#93;</span></a></sup> and <a href="/wiki/Climate_change" title="Climate change">climate change</a>.<sup id="cite_ref-Davidson_16-0" class="reference"><a href="#cite_note-Davidson-16"><span class="cite-bracket">&#91;</span>16<span class="cite-bracket">&#93;</span></a></sup> As the planet warms, it has been predicted that soils will add carbon dioxide to the atmosphere due to increased <a href="/wiki/Soil_biology" title="Soil biology">biological</a> activity at higher temperatures, a <a href="/wiki/Positive_feedback" title="Positive feedback">positive feedback</a> (amplification).<sup id="cite_ref-17" class="reference"><a href="#cite_note-17"><span class="cite-bracket">&#91;</span>17<span class="cite-bracket">&#93;</span></a></sup> This prediction has, however, been questioned on consideration of more recent knowledge on <a href="/wiki/Soil_carbon" title="Soil carbon">soil carbon</a> turnover.<sup id="cite_ref-18" class="reference"><a href="#cite_note-18"><span class="cite-bracket">&#91;</span>18<span class="cite-bracket">&#93;</span></a></sup> </p><p>Soil acts as an engineering medium, a habitat for <a href="/wiki/Soil_organisms" class="mw-redirect" title="Soil organisms">soil organisms</a>, a recycling system for <a href="/wiki/Nutrients" class="mw-redirect" title="Nutrients">nutrients</a> and <a href="/wiki/Organic_waste" class="mw-redirect" title="Organic waste">organic wastes</a>, a regulator of <a href="/wiki/Water_quality" title="Water quality">water quality</a>, a modifier of <a href="/wiki/Atmospheric_chemistry" title="Atmospheric chemistry">atmospheric composition</a>, and a medium for <a href="/wiki/Plant_growth" class="mw-redirect" title="Plant growth">plant growth</a>, making it a critically important provider of <a href="/wiki/Ecosystem_services" class="mw-redirect" title="Ecosystem services">ecosystem services</a>.<sup id="cite_ref-19" class="reference"><a href="#cite_note-19"><span class="cite-bracket">&#91;</span>19<span class="cite-bracket">&#93;</span></a></sup> Since soil has a tremendous range of available <a href="/wiki/Ecological_niche" title="Ecological niche">niches</a> and <a href="/wiki/Habitat" title="Habitat">habitats</a>, it contains a prominent part of the Earth's <a href="/wiki/Genetic_diversity" title="Genetic diversity">genetic diversity</a>. A gram of soil can contain billions of organisms, belonging to thousands of species, mostly microbial and largely still unexplored.<sup id="cite_ref-20" class="reference"><a href="#cite_note-20"><span class="cite-bracket">&#91;</span>20<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-21" class="reference"><a href="#cite_note-21"><span class="cite-bracket">&#91;</span>21<span class="cite-bracket">&#93;</span></a></sup> Soil has a <a href="/wiki/Mean" title="Mean">mean</a> <a href="/wiki/Prokaryote" title="Prokaryote">prokaryotic</a> density of roughly 10<sup>8</sup> organisms per gram,<sup id="cite_ref-22" class="reference"><a href="#cite_note-22"><span class="cite-bracket">&#91;</span>22<span class="cite-bracket">&#93;</span></a></sup> whereas the ocean has no more than 10<sup>7</sup> prokaryotic organisms per milliliter (gram) of seawater.<sup id="cite_ref-23" class="reference"><a href="#cite_note-23"><span class="cite-bracket">&#91;</span>23<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Soil_organic_matter" title="Soil organic matter">Organic carbon</a> held in soil is eventually returned to the atmosphere through the process of <a href="/wiki/Cellular_respiration" title="Cellular respiration">respiration</a> carried out by <a href="/wiki/Heterotrophic" class="mw-redirect" title="Heterotrophic">heterotrophic</a> organisms, but a substantial part is retained in the soil in the form of soil organic matter; <a href="/wiki/Tillage" title="Tillage">tillage</a> usually increases the rate of <a href="/wiki/Soil_respiration" title="Soil respiration">soil respiration</a>, leading to the depletion of soil organic matter.<sup id="cite_ref-24" class="reference"><a href="#cite_note-24"><span class="cite-bracket">&#91;</span>24<span class="cite-bracket">&#93;</span></a></sup> Since plant roots need oxygen, <a href="/wiki/Aeration" title="Aeration">aeration</a> is an important characteristic of soil. This ventilation can be accomplished via networks of interconnected <a href="/wiki/Pore_space_in_soil" title="Pore space in soil">soil pores</a>, which also absorb and hold rainwater making it readily available for uptake by plants. Since plants require a nearly continuous supply of water, but most regions receive sporadic rainfall, the <a href="/wiki/Soil_water_(retention)" title="Soil water (retention)">water-holding capacity</a> of soils is vital for plant survival.<sup id="cite_ref-25" class="reference"><a href="#cite_note-25"><span class="cite-bracket">&#91;</span>25<span class="cite-bracket">&#93;</span></a></sup> </p><p>Soils can effectively remove impurities,<sup id="cite_ref-26" class="reference"><a href="#cite_note-26"><span class="cite-bracket">&#91;</span>26<span class="cite-bracket">&#93;</span></a></sup> kill disease agents,<sup id="cite_ref-27" class="reference"><a href="#cite_note-27"><span class="cite-bracket">&#91;</span>27<span class="cite-bracket">&#93;</span></a></sup> and degrade <a href="/wiki/Contaminants" class="mw-redirect" title="Contaminants">contaminants</a>, this latter property being called <a href="/wiki/Natural_attenuation" class="mw-redirect" title="Natural attenuation">natural attenuation</a>.<sup id="cite_ref-28" class="reference"><a href="#cite_note-28"><span class="cite-bracket">&#91;</span>28<span class="cite-bracket">&#93;</span></a></sup> Typically, soils maintain a net absorption of <a href="/wiki/Oxygen" title="Oxygen">oxygen</a> and <a href="/wiki/Methane" title="Methane">methane</a> and undergo a net release of <a href="/wiki/Carbon_dioxide" title="Carbon dioxide">carbon dioxide</a> and <a href="/wiki/Nitrous_oxide" title="Nitrous oxide">nitrous oxide</a>.<sup id="cite_ref-29" class="reference"><a href="#cite_note-29"><span class="cite-bracket">&#91;</span>29<span class="cite-bracket">&#93;</span></a></sup> Soils offer plants physical support, air, water, temperature moderation, nutrients, and protection from toxins.<sup id="cite_ref-30" class="reference"><a href="#cite_note-30"><span class="cite-bracket">&#91;</span>30<span class="cite-bracket">&#93;</span></a></sup> Soils provide readily available nutrients to plants and animals by converting dead organic matter into various nutrient forms.<sup id="cite_ref-31" class="reference"><a href="#cite_note-31"><span class="cite-bracket">&#91;</span>31<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Composition">Composition</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=2" title="Edit section: Composition"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size mw-halign-right" typeof="mw:File/Thumb"><a href="/wiki/File:Estructura-suelo.jpg" class="mw-file-description"><img alt="This is a diagram and related photograph of soil layers from bedrock to soil." src="//upload.wikimedia.org/wikipedia/commons/thumb/d/d3/Estructura-suelo.jpg/220px-Estructura-suelo.jpg" decoding="async" width="220" height="232" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/d/d3/Estructura-suelo.jpg/330px-Estructura-suelo.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/d/d3/Estructura-suelo.jpg/440px-Estructura-suelo.jpg 2x" data-file-width="513" data-file-height="541" /></a><figcaption>A, B, and C represent the <a href="/wiki/Soil_horizon" title="Soil horizon">soil profile</a>, a notation firstly coined by <a href="/wiki/Vasily_Dokuchaev" title="Vasily Dokuchaev">Vasily Dokuchaev</a> (1846–1903), the father of pedology. Here, A is the <a href="/wiki/Topsoil" title="Topsoil">topsoil</a>; B is a <a href="/wiki/Regolith" title="Regolith">regolith</a>; C is a <a href="/wiki/Saprolite" title="Saprolite">saprolite</a> (a less-weathered regolith); the bottom-most layer represents the <a href="/wiki/Bedrock" title="Bedrock">bedrock</a>.</figcaption></figure> <div class="PieChartTemplate thumb tright"><div class="thumbinner" style="width:202px"> <div class="mw-no-invert" style="background-color:white;margin:auto;position:relative;width:200px;height:200px;overflow:hidden;border-radius:100px;border:1px solid black;transform:scaleX(-1)rotate(-90deg)"> <div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;left:0; top:0; border-width:0 200px 200px 0; border-color:black; z-index:-1"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;left:100px; top:100px; border-width:100px 0 0 307.76835371753px; border-left-color:grey"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 200px 100px 0;border-color:grey"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 100px 200px 0;border-color:grey"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;left:100px; top:100px; border-width:100px 0 0 82.727194597248px; border-left-color:brown"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 200px 100px 0;border-color:brown"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 100px 200px 0;border-color:brown"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;right:100px; top:100px; border-width:90.482705246602px 42.577929156507px 0 0; border-top-color:yellow"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 200px 100px 0;border-color:yellow"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;right:100px; top:100px; border-width:0px 100px 0 0; border-top-color:cyan"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 200px 100px 0;border-color:cyan"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;right:100px; top:0; border-width:0 0px 100px 0; border-right-color:blue"></div> <div style="position:absolute;line-height:0;border-style:solid;right:0;top:0;border-width:0 100px 100px 0;border-color:blue"></div> </div> <div class="thumbcaption"> <p>Components of a silt loam soil by percent volume </p> <style data-mw-deduplicate="TemplateStyles:r981673959">.mw-parser-output .legend{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .legend-color{display:inline-block;min-width:1.25em;height:1.25em;line-height:1.25;margin:1px 0;text-align:center;border:1px solid black;background-color:transparent;color:black}.mw-parser-output .legend-text{}</style><div class="legend"><span class="legend-color mw-no-invert" style="background-color:blue; color:white;">&#160;</span>&#160;Water (25%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:cyan; color:black;">&#160;</span>&#160;Gases (25%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:yellow; color:black;">&#160;</span>&#160;Sand (18%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:brown; color:white;">&#160;</span>&#160;Silt (18%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:grey; color:black;">&#160;</span>&#160;Clay (9%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:black; color:white;">&#160;</span>&#160;Organic matter (5%)</div> </div> </div></div> <p>A typical soil is about 50% solids (45% mineral and 5% organic matter), and 50% voids (or pores) of which half is occupied by water and half by gas.<sup id="cite_ref-McClellan2017_32-0" class="reference"><a href="#cite_note-McClellan2017-32"><span class="cite-bracket">&#91;</span>32<span class="cite-bracket">&#93;</span></a></sup> The percent soil mineral and organic content can be treated as a constant (in the short term), while the percent soil water and gas content is considered highly variable whereby a rise in one is simultaneously balanced by a reduction in the other.<sup id="cite_ref-33" class="reference"><a href="#cite_note-33"><span class="cite-bracket">&#91;</span>33<span class="cite-bracket">&#93;</span></a></sup> The <a href="/wiki/Pore_space" class="mw-redirect" title="Pore space">pore space</a> allows for the infiltration and movement of air and water, both of which are critical for life existing in soil.<sup id="cite_ref-Vannier1987_34-0" class="reference"><a href="#cite_note-Vannier1987-34"><span class="cite-bracket">&#91;</span>34<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Soil_compaction" title="Soil compaction">Compaction</a>, a common problem with soils, reduces this space, preventing air and water from reaching plant roots and soil organisms.<sup id="cite_ref-35" class="reference"><a href="#cite_note-35"><span class="cite-bracket">&#91;</span>35<span class="cite-bracket">&#93;</span></a></sup> </p><p>Given sufficient time, an undifferentiated soil will evolve a <a href="/wiki/Soil_horizon" title="Soil horizon">soil profile</a> that consists of two or more layers, referred to as soil horizons. These differ in one or more properties such as in their <a href="/wiki/Soil_texture" title="Soil texture">texture</a>, <a href="/wiki/Structure" title="Structure">structure</a>, <a href="/wiki/Density" title="Density">density</a>, porosity, consistency, temperature, color, and <a href="/wiki/Reactivity_(chemistry)" title="Reactivity (chemistry)">reactivity</a>.<sup id="cite_ref-Buol_8-1" class="reference"><a href="#cite_note-Buol-8"><span class="cite-bracket">&#91;</span>8<span class="cite-bracket">&#93;</span></a></sup> The horizons differ greatly in thickness and generally lack sharp boundaries; their development is dependent on the type of <a href="/wiki/Parent_material" title="Parent material">parent material</a>, the processes that modify those parent materials, and the <a href="#soil-forming_factors">soil-forming factors</a> that influence those processes. The biological influences on soil properties are strongest near the surface, though the geochemical influences on soil properties increase with depth. Mature soil profiles typically include three basic master horizons: A, B, and C. The <a href="/wiki/Solum" title="Solum">solum</a> normally includes the A and B horizons. The living component of the soil is largely confined to the solum, and is generally more prominent in the A horizon.<sup id="cite_ref-FOOTNOTESimonson195717_36-0" class="reference"><a href="#cite_note-FOOTNOTESimonson195717-36"><span class="cite-bracket">&#91;</span>36<span class="cite-bracket">&#93;</span></a></sup> It has been suggested that the <i>pedon</i>, a column of soil extending vertically from the surface to the underlying parent material and large enough to show the characteristics of all its horizons, could be subdivided in the <i>humipedon</i> (the living part, where most soil organisms are dwelling, corresponding to the <i>humus form</i>), the <i>copedon</i> (in intermediary position, where most <a href="/wiki/Weathering" title="Weathering">weathering</a> of minerals takes place) and the <i>lithopedon</i> (in contact with the subsoil).<sup id="cite_ref-37" class="reference"><a href="#cite_note-37"><span class="cite-bracket">&#91;</span>37<span class="cite-bracket">&#93;</span></a></sup> </p><p> The soil texture is determined by the relative proportions of the individual particles of <a href="/wiki/Sand" title="Sand">sand</a>, <a href="/wiki/Silt" title="Silt">silt</a>, and <a href="/wiki/Clay" title="Clay">clay</a> that make up the soil. </p><figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:SoilTextureTriangle.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/3/39/SoilTextureTriangle.svg/220px-SoilTextureTriangle.svg.png" decoding="async" width="220" height="254" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/3/39/SoilTextureTriangle.svg/330px-SoilTextureTriangle.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/3/39/SoilTextureTriangle.svg/440px-SoilTextureTriangle.svg.png 2x" data-file-width="800" data-file-height="924" /></a><figcaption>A <a href="/wiki/Soil_triangle" class="mw-redirect" title="Soil triangle">soil texture triangle</a> plot is a visual representation of the proportions of sand, silt, and clay in a soil sample.</figcaption></figure><p> The interaction of the individual mineral particles with organic matter, water, gases via <a href="/wiki/Biotic_component" class="mw-redirect" title="Biotic component">biotic</a> and <a href="/wiki/Abiotic" class="mw-redirect" title="Abiotic">abiotic</a> processes causes those particles to <a href="/wiki/Flocculate" class="mw-redirect" title="Flocculate">flocculate</a> (stick together) to form <a href="/wiki/Soil_structure" title="Soil structure">aggregates</a> or <a href="/wiki/Ped" title="Ped">peds</a>.<sup id="cite_ref-Bronick2005_38-0" class="reference"><a href="#cite_note-Bronick2005-38"><span class="cite-bracket">&#91;</span>38<span class="cite-bracket">&#93;</span></a></sup> Where these aggregates can be identified, a soil can be said to be developed, and can be described further in terms of color, porosity, consistency, reaction (<a href="/wiki/Acidity" class="mw-redirect" title="Acidity">acidity</a>), etc. </p><p>Water is a critical agent in soil development due to its involvement in the dissolution, precipitation, erosion, transport, and deposition of the materials of which a soil is composed.<sup id="cite_ref-39" class="reference"><a href="#cite_note-39"><span class="cite-bracket">&#91;</span>39<span class="cite-bracket">&#93;</span></a></sup> The mixture of water and dissolved or suspended materials that occupy the soil <a href="/wiki/Pore_space" class="mw-redirect" title="Pore space">pore space</a> is called the soil solution. Since soil water is never pure water, but contains hundreds of dissolved organic and mineral substances, it may be more accurately called the soil solution. Water is central to the <a href="/wiki/Dissolution_(chemistry)" class="mw-redirect" title="Dissolution (chemistry)">dissolution</a>, <a href="/wiki/Precipitation_(chemistry)" title="Precipitation (chemistry)">precipitation</a> and <a href="/wiki/Leaching_(agriculture)" title="Leaching (agriculture)">leaching</a> of minerals from the <a href="/wiki/Soil_profile" class="mw-redirect" title="Soil profile">soil profile</a>. Finally, water affects the type of vegetation that grows in a soil, which in turn affects the development of the soil, a complex feedback which is exemplified in the dynamics of banded vegetation patterns in semi-arid regions.<sup id="cite_ref-40" class="reference"><a href="#cite_note-40"><span class="cite-bracket">&#91;</span>40<span class="cite-bracket">&#93;</span></a></sup> </p><p>Soils supply <a href="/wiki/Plant" title="Plant">plants</a> with <a href="/wiki/Nutrient" title="Nutrient">nutrients</a>, most of which are held in place by particles of <a href="/wiki/Soil_texture#Soil_separates" title="Soil texture">clay</a> and organic matter (<a href="/wiki/Colloid" title="Colloid">colloids</a>)<sup id="cite_ref-41" class="reference"><a href="#cite_note-41"><span class="cite-bracket">&#91;</span>41<span class="cite-bracket">&#93;</span></a></sup> The nutrients may be <a href="/wiki/Adsorption" title="Adsorption">adsorbed</a> on clay mineral surfaces, bound within clay minerals (<a href="/wiki/Absorption_(chemistry)" title="Absorption (chemistry)">absorbed</a>), or bound within organic compounds as part of the living <a href="/wiki/Soil_organism" class="mw-redirect" title="Soil organism">organisms</a> or dead soil organic matter. These bound nutrients interact with soil water to <a href="/wiki/Buffer_solution" title="Buffer solution">buffer</a> the soil solution composition (attenuate changes in the soil solution) as soils wet up or dry out, as plants take up nutrients, as salts are leached, or as acids or alkalis are added.<sup id="cite_ref-42" class="reference"><a href="#cite_note-42"><span class="cite-bracket">&#91;</span>42<span class="cite-bracket">&#93;</span></a></sup> </p><p>Plant nutrient availability is affected by <a href="/wiki/Soil_pH" title="Soil pH">soil pH</a>, which is a measure of the <a href="/wiki/Hydrogen" title="Hydrogen">hydrogen</a> <a href="/wiki/Thermodynamic_activity" title="Thermodynamic activity">ion activity</a> in the soil solution. Soil pH is a function of many soil forming factors, and is generally lower (more acidic) where weathering is more advanced.<sup id="cite_ref-43" class="reference"><a href="#cite_note-43"><span class="cite-bracket">&#91;</span>43<span class="cite-bracket">&#93;</span></a></sup> </p><p>Most plant nutrients, with the exception of <a href="/wiki/Nitrogen" title="Nitrogen">nitrogen</a>, originate from the minerals that make up the soil parent material. Some nitrogen originates from rain as dilute <a href="/wiki/Nitric_acid" title="Nitric acid">nitric acid</a> and <a href="/wiki/Ammonia" title="Ammonia">ammonia</a>,<sup id="cite_ref-44" class="reference"><a href="#cite_note-44"><span class="cite-bracket">&#91;</span>44<span class="cite-bracket">&#93;</span></a></sup> but most of the nitrogen is available in soils as a result of <a href="/wiki/Nitrogen_fixation" title="Nitrogen fixation">nitrogen fixation</a> by <a href="/wiki/Bacteria" title="Bacteria">bacteria</a>. Once in the soil-plant system, most nutrients are recycled through living organisms, plant and microbial residues (soil organic matter), mineral-bound forms, and the soil solution. Both living soil organisms (microbes, animals and plant roots) and soil organic matter are of critical importance to this recycling, and thereby to <a href="/wiki/Soil_formation" title="Soil formation">soil formation</a> and <a href="/wiki/Soil_fertility" title="Soil fertility">soil fertility</a>.<sup id="cite_ref-45" class="reference"><a href="#cite_note-45"><span class="cite-bracket">&#91;</span>45<span class="cite-bracket">&#93;</span></a></sup> Microbial <a href="/wiki/Soil_enzyme" title="Soil enzyme">soil enzymes</a> may release nutrients from minerals or organic matter for use by plants and other microorganisms, sequester (incorporate) them into living cells, or cause their loss from the soil by <a href="/wiki/Volatilisation" class="mw-redirect" title="Volatilisation">volatilisation</a> (loss to the atmosphere as gases) or leaching.<sup id="cite_ref-46" class="reference"><a href="#cite_note-46"><span class="cite-bracket">&#91;</span>46<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Formation">Formation</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=3" title="Edit section: Formation"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Soil_formation" title="Soil formation">Soil formation</a></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Further information: <a href="/wiki/Soil_mechanics#Genesis" title="Soil mechanics">Soil mechanics §&#160;Genesis</a></div> <p>Soil is said to be formed when organic matter has accumulated and colloids are washed downward, leaving deposits of clay, <a href="/wiki/Humus" title="Humus">humus</a>, <a href="/wiki/Iron_oxide" title="Iron oxide">iron oxide</a>, <a href="/wiki/Carbonate" title="Carbonate">carbonate</a>, and <a href="/wiki/Gypsum" title="Gypsum">gypsum</a>, producing a distinct layer called the B horizon. This is a somewhat arbitrary definition as mixtures of sand, silt, clay and humus will support biological and agricultural activity before that time.<sup id="cite_ref-47" class="reference"><a href="#cite_note-47"><span class="cite-bracket">&#91;</span>47<span class="cite-bracket">&#93;</span></a></sup> These constituents are moved from one level to another by water and animal activity. As a result, layers (horizons) form in the soil profile. The alteration and movement of materials within a soil causes the formation of distinctive <a href="/wiki/Soil_horizons" class="mw-redirect" title="Soil horizons">soil horizons</a>. However, more recent definitions of soil embrace soils without any organic matter, such as those <a href="/wiki/Regolith" title="Regolith">regoliths</a> that formed on Mars<sup id="cite_ref-48" class="reference"><a href="#cite_note-48"><span class="cite-bracket">&#91;</span>48<span class="cite-bracket">&#93;</span></a></sup> and analogous conditions in planet Earth deserts.<sup id="cite_ref-49" class="reference"><a href="#cite_note-49"><span class="cite-bracket">&#91;</span>49<span class="cite-bracket">&#93;</span></a></sup> </p><p>An example of the development of a soil would begin with the weathering of lava flow bedrock, which would produce the purely mineral-based parent material from which the soil texture forms. Soil development would proceed most rapidly from bare rock of recent flows in a warm climate, under heavy and frequent rainfall. Under such conditions, plants (in a first stage <a href="/wiki/Nitrogen-fixing" class="mw-redirect" title="Nitrogen-fixing">nitrogen-fixing</a> <a href="/wiki/Lichen" title="Lichen">lichens</a> and <a href="/wiki/Cyanobacteria" title="Cyanobacteria">cyanobacteria</a> then <a href="/wiki/Epilithic" class="mw-redirect" title="Epilithic">epilithic</a> <a href="/wiki/Higher_plants" class="mw-redirect" title="Higher plants">higher plants</a>) become established very quickly on <a href="/wiki/Basalt" title="Basalt">basaltic</a> lava, even though there is very little organic material.<sup id="cite_ref-50" class="reference"><a href="#cite_note-50"><span class="cite-bracket">&#91;</span>50<span class="cite-bracket">&#93;</span></a></sup> Basaltic minerals commonly weather relatively quickly, according to the <a href="/wiki/Goldich_dissolution_series" title="Goldich dissolution series">Goldich dissolution series</a>.<sup id="cite_ref-51" class="reference"><a href="#cite_note-51"><span class="cite-bracket">&#91;</span>51<span class="cite-bracket">&#93;</span></a></sup> The plants are supported by the porous rock as it is filled with nutrient-bearing water that carries minerals dissolved from the rocks. Crevasses and pockets, local topography of the rocks, would hold fine materials and harbour plant roots. The developing plant roots are associated with mineral-weathering <a href="/wiki/Mycorrhiza" title="Mycorrhiza">mycorrhizal fungi</a><sup id="cite_ref-Van_Schöll2006_52-0" class="reference"><a href="#cite_note-Van_Schöll2006-52"><span class="cite-bracket">&#91;</span>52<span class="cite-bracket">&#93;</span></a></sup> that assist in breaking up the porous lava, and by these means organic matter and a finer mineral soil accumulate with time. Such initial stages of soil development have been described on volcanoes,<sup id="cite_ref-53" class="reference"><a href="#cite_note-53"><span class="cite-bracket">&#91;</span>53<span class="cite-bracket">&#93;</span></a></sup> inselbergs,<sup id="cite_ref-54" class="reference"><a href="#cite_note-54"><span class="cite-bracket">&#91;</span>54<span class="cite-bracket">&#93;</span></a></sup> and glacial moraines.<sup id="cite_ref-55" class="reference"><a href="#cite_note-55"><span class="cite-bracket">&#91;</span>55<span class="cite-bracket">&#93;</span></a></sup> </p><p>How soil formation proceeds is influenced by at least five classic factors that are intertwined in the evolution of a soil: parent material, climate, topography (relief), organisms, and time.<sup id="cite_ref-Jenny1941_56-0" class="reference"><a href="#cite_note-Jenny1941-56"><span class="cite-bracket">&#91;</span>56<span class="cite-bracket">&#93;</span></a></sup> When reordered to climate, relief, organisms, parent material, and time, they form the acronym CROPT.<sup id="cite_ref-57" class="reference"><a href="#cite_note-57"><span class="cite-bracket">&#91;</span>57<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Physical_properties">Physical properties</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=4" title="Edit section: Physical properties"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Physical_properties_of_soil" title="Physical properties of soil">Physical properties of soil</a></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">For the academic discipline, see <a href="/wiki/Soil_physics" title="Soil physics">Soil physics</a>.</div> <p>The physical properties of soils, in order of decreasing importance for ecosystem services such as <a href="/wiki/Crop_production" class="mw-redirect" title="Crop production">crop production</a>, are <a href="/wiki/Soil_texture" title="Soil texture">texture</a>, <a href="/wiki/Soil_structure" title="Soil structure">structure</a>, <a href="/wiki/Bulk_density" title="Bulk density">bulk density</a>, <a href="/wiki/Pore_space_in_soil" title="Pore space in soil">porosity</a>, consistency, <a href="/wiki/Temperature" title="Temperature">temperature</a>, <a href="/wiki/Soil_color" title="Soil color">colour</a> and <a href="/w/index.php?title=Soil_resistivity&amp;action=edit&amp;redlink=1" class="new" title="Soil resistivity (page does not exist)">resistivity</a>.<sup id="cite_ref-58" class="reference"><a href="#cite_note-58"><span class="cite-bracket">&#91;</span>58<span class="cite-bracket">&#93;</span></a></sup> Soil texture is determined by the relative proportion of the three kinds of soil mineral particles, called soil separates: <a href="/wiki/Sand" title="Sand">sand</a>, <a href="/wiki/Silt" title="Silt">silt</a>, and <a href="/wiki/Clay" title="Clay">clay</a>. At the next larger scale, soil structures called <a href="/wiki/Ped" title="Ped">peds</a> or more commonly <i>soil aggregates</i> are created from the soil separates when <a href="/wiki/Iron_oxide" title="Iron oxide">iron oxides</a>, <a href="/wiki/Carbonate" title="Carbonate">carbonates</a>, clay, <a href="/wiki/Silica" class="mw-redirect" title="Silica">silica</a> and <a href="/wiki/Humus" title="Humus">humus</a>, coat particles and cause them to adhere into larger, relatively <a href="/wiki/Soil_aggregate_stability" title="Soil aggregate stability">stable</a> secondary structures.<sup id="cite_ref-59" class="reference"><a href="#cite_note-59"><span class="cite-bracket">&#91;</span>59<span class="cite-bracket">&#93;</span></a></sup> Soil <a href="/wiki/Bulk_density" title="Bulk density">bulk density</a>, when determined at standardized moisture conditions, is an estimate of <a href="/wiki/Soil_compaction_(agriculture)" title="Soil compaction (agriculture)">soil compaction</a>.<sup id="cite_ref-60" class="reference"><a href="#cite_note-60"><span class="cite-bracket">&#91;</span>60<span class="cite-bracket">&#93;</span></a></sup> Soil porosity consists of the void part of the soil volume and is occupied by gases or water. Soil consistency is the ability of soil materials to stick together. Soil temperature and colour are self-defining. Resistivity refers to the resistance to conduction of electric currents and affects the rate of corrosion of metal and concrete structures which are buried in soil.<sup id="cite_ref-61" class="reference"><a href="#cite_note-61"><span class="cite-bracket">&#91;</span>61<span class="cite-bracket">&#93;</span></a></sup> These properties vary through the depth of a soil profile, i.e. through <a href="/wiki/Soil_horizon" title="Soil horizon">soil horizons</a>. Most of these properties determine the <a href="/wiki/Permeability_of_soils" title="Permeability of soils">aeration</a> of the soil and the ability of water to <a href="/wiki/Infiltration_(hydrology)" title="Infiltration (hydrology)">infiltrate</a> and to be <a href="/wiki/Soil_water_(retention)" title="Soil water (retention)">held</a> within the soil.<sup id="cite_ref-62" class="reference"><a href="#cite_note-62"><span class="cite-bracket">&#91;</span>62<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Soil_moisture">Soil moisture</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=5" title="Edit section: Soil moisture"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Soil_moisture" title="Soil moisture">Soil moisture</a></div> <p>Soil <a href="/wiki/Water_content" title="Water content">water content</a> can be measured as volume or <a href="/wiki/Specific_weight#Soil_mechanics" title="Specific weight">weight</a>. Soil moisture levels, in order of decreasing water content, are saturation, <a href="/wiki/Field_capacity" title="Field capacity">field capacity</a>, <a href="/wiki/Wilting_point" class="mw-redirect" title="Wilting point">wilting point</a>, air dry, and oven dry. Field capacity describes a drained wet soil at the point water content reaches equilibrium with gravity. Irrigating soil above field capacity risks percolation losses. Wilting point describes the dry limit for growing plants. During growing season, soil moisture is unaffected by functional groups or specie richness.<sup id="cite_ref-auto1_63-0" class="reference"><a href="#cite_note-auto1-63"><span class="cite-bracket">&#91;</span>63<span class="cite-bracket">&#93;</span></a></sup> </p><p><a href="/wiki/Available_water_capacity" title="Available water capacity">Available water capacity</a> is the amount of water held in a soil profile available to plants. As water content drops, plants have to work against increasing forces of <a href="/wiki/Adhesion" title="Adhesion">adhesion</a> and <a href="/wiki/Sorptivity" title="Sorptivity">sorptivity</a> to withdraw water. <a href="/wiki/Irrigation_scheduling" title="Irrigation scheduling">Irrigation scheduling</a> avoids <a href="/wiki/Moisture_stress" title="Moisture stress">moisture stress</a> by replenishing depleted water before stress is induced.<sup id="cite_ref-64" class="reference"><a href="#cite_note-64"><span class="cite-bracket">&#91;</span>64<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-65" class="reference"><a href="#cite_note-65"><span class="cite-bracket">&#91;</span>65<span class="cite-bracket">&#93;</span></a></sup> </p><p><a href="/wiki/Capillary_action" title="Capillary action">Capillary action</a> is responsible for moving <a href="/wiki/Groundwater" title="Groundwater">groundwater</a> from wet regions of the soil to dry areas. <a href="/wiki/Subirrigation" title="Subirrigation">Subirrigation</a> designs (e.g., <a href="/wiki/Wicking_bed" title="Wicking bed">wicking beds</a>, <a href="/wiki/Sub-irrigated_planter" title="Sub-irrigated planter">sub-irrigated planters</a>) rely on <a href="/wiki/Capillary_action" title="Capillary action">capillarity</a> to supply water to plant roots. Capillary action can result in an evaporative concentration of salts, causing land degradation through <a href="/wiki/Soil_salinity#Dry_land_salinity" title="Soil salinity">salination</a>. </p><p><a href="/wiki/Soil_moisture_measurement" class="mw-redirect" title="Soil moisture measurement">Soil moisture measurement</a>—measuring the water content of the soil, as can be expressed in terms of volume or weight—can be based on <i>in situ</i> probes (e.g., <a href="/wiki/Capacitance_probe" title="Capacitance probe">capacitance probes</a>, <a href="/wiki/Neutron_probe" title="Neutron probe">neutron probes</a>), or <a href="/wiki/Remote_sensing" title="Remote sensing">remote sensing</a> methods. Soil moisture measurement is an important factor in determining changes in soil activity.<sup id="cite_ref-auto1_63-1" class="reference"><a href="#cite_note-auto1-63"><span class="cite-bracket">&#91;</span>63<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Soil_gas">Soil gas</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=6" title="Edit section: Soil gas"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Soil_gas" title="Soil gas">Soil gas</a></div> <p>The atmosphere of soil, or <a href="/wiki/Soil_gas" title="Soil gas">soil gas</a>, is very different from the atmosphere above. The consumption of oxygen by microbes and plant roots, and their release of carbon dioxide, decreases oxygen and increases carbon dioxide concentration. Atmospheric CO<sub>2</sub> concentration is 0.04%, but in the soil pore space it may range from 10 to 100 times that level, thus potentially contributing to the inhibition of root respiration.<sup id="cite_ref-66" class="reference"><a href="#cite_note-66"><span class="cite-bracket">&#91;</span>66<span class="cite-bracket">&#93;</span></a></sup> Calcareous soils regulate CO<sub>2</sub> concentration by <a href="/wiki/Carbonate" title="Carbonate">carbonate</a> <a href="/wiki/Buffering_agent" class="mw-redirect" title="Buffering agent">buffering</a>, contrary to acid soils in which all CO<sub>2</sub> respired accumulates in the soil pore system.<sup id="cite_ref-67" class="reference"><a href="#cite_note-67"><span class="cite-bracket">&#91;</span>67<span class="cite-bracket">&#93;</span></a></sup> At extreme levels, CO<sub>2</sub> is toxic.<sup id="cite_ref-68" class="reference"><a href="#cite_note-68"><span class="cite-bracket">&#91;</span>68<span class="cite-bracket">&#93;</span></a></sup> This suggests a possible <a href="/wiki/Negative_feedback" title="Negative feedback">negative feedback</a> control of soil CO<sub>2</sub> concentration through its inhibitory effects on root and microbial respiration (also called <a href="/wiki/Soil_respiration" title="Soil respiration">soil respiration</a>).<sup id="cite_ref-69" class="reference"><a href="#cite_note-69"><span class="cite-bracket">&#91;</span>69<span class="cite-bracket">&#93;</span></a></sup> In addition, the soil voids are saturated with water vapour, at least until the point of maximal <a href="/wiki/Hygroscopic" class="mw-redirect" title="Hygroscopic">hygroscopicity</a>, beyond which a <a href="/wiki/Vapour-pressure_deficit" title="Vapour-pressure deficit">vapour-pressure deficit</a> occurs in the soil pore space.<sup id="cite_ref-Vannier1987_34-1" class="reference"><a href="#cite_note-Vannier1987-34"><span class="cite-bracket">&#91;</span>34<span class="cite-bracket">&#93;</span></a></sup> Adequate porosity is necessary, not just to allow the penetration of water, but also to allow gases to diffuse in and out. Movement of gases is by <a href="/wiki/Diffusion" title="Diffusion">diffusion</a> from high concentrations to lower, the <a href="/wiki/Diffusion_coefficient" class="mw-redirect" title="Diffusion coefficient">diffusion coefficient</a> decreasing with <a href="/wiki/Soil_compaction_(agriculture)" title="Soil compaction (agriculture)">soil compaction</a>.<sup id="cite_ref-70" class="reference"><a href="#cite_note-70"><span class="cite-bracket">&#91;</span>70<span class="cite-bracket">&#93;</span></a></sup> Oxygen from above atmosphere diffuses in the soil where it is consumed and levels of carbon dioxide in excess of above atmosphere diffuse out with other gases (including <a href="/wiki/Greenhouse_gases" class="mw-redirect" title="Greenhouse gases">greenhouse gases</a>) as well as water.<sup id="cite_ref-Smith2003_71-0" class="reference"><a href="#cite_note-Smith2003-71"><span class="cite-bracket">&#91;</span>71<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Soil_texture" title="Soil texture">Soil texture</a> and <a href="/wiki/Soil_structure" title="Soil structure">structure</a> strongly affect soil porosity and gas diffusion. It is the total pore space (<a href="/wiki/Porosity" title="Porosity">porosity</a>) of soil, not the pore size, and the degree of pore interconnection (or conversely pore sealing), together with water content, air <a href="/wiki/Turbulence" title="Turbulence">turbulence</a> and temperature, that determine the rate of diffusion of gases into and out of soil.<sup id="cite_ref-FOOTNOTERussell195735–36_72-0" class="reference"><a href="#cite_note-FOOTNOTERussell195735–36-72"><span class="cite-bracket">&#91;</span>72<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Smith2003_71-1" class="reference"><a href="#cite_note-Smith2003-71"><span class="cite-bracket">&#91;</span>71<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Ped#Platy" title="Ped">Platy</a> soil structure and soil compaction (low porosity) impede gas flow, and a deficiency of oxygen may encourage anaerobic bacteria to reduce (strip oxygen) from nitrate NO<sub>3</sub> to the gases N<sub>2</sub>, N<sub>2</sub>O, and NO, which are then lost to the atmosphere, thereby depleting the soil of nitrogen, a detrimental process called <a href="/wiki/Denitrification" title="Denitrification">denitrification</a>.<sup id="cite_ref-73" class="reference"><a href="#cite_note-73"><span class="cite-bracket">&#91;</span>73<span class="cite-bracket">&#93;</span></a></sup> Aerated soil is also a net sink of methane (CH<sub>4</sub>)<sup id="cite_ref-74" class="reference"><a href="#cite_note-74"><span class="cite-bracket">&#91;</span>74<span class="cite-bracket">&#93;</span></a></sup> but a net producer of methane (a strong heat-absorbing <a href="/wiki/Greenhouse_gas" title="Greenhouse gas">greenhouse gas</a>) when soils are depleted of oxygen and subject to elevated temperatures.<sup id="cite_ref-75" class="reference"><a href="#cite_note-75"><span class="cite-bracket">&#91;</span>75<span class="cite-bracket">&#93;</span></a></sup> </p><p>Soil atmosphere is also the seat of emissions of <a href="/wiki/Volatile_(astrogeology)" title="Volatile (astrogeology)">volatiles</a> other than carbon and nitrogen oxides from various soil organisms, e.g. roots,<sup id="cite_ref-76" class="reference"><a href="#cite_note-76"><span class="cite-bracket">&#91;</span>76<span class="cite-bracket">&#93;</span></a></sup> bacteria,<sup id="cite_ref-77" class="reference"><a href="#cite_note-77"><span class="cite-bracket">&#91;</span>77<span class="cite-bracket">&#93;</span></a></sup> fungi,<sup id="cite_ref-78" class="reference"><a href="#cite_note-78"><span class="cite-bracket">&#91;</span>78<span class="cite-bracket">&#93;</span></a></sup> animals.<sup id="cite_ref-79" class="reference"><a href="#cite_note-79"><span class="cite-bracket">&#91;</span>79<span class="cite-bracket">&#93;</span></a></sup> These volatiles are used as chemical cues, making soil atmosphere the seat of interaction networks<sup id="cite_ref-80" class="reference"><a href="#cite_note-80"><span class="cite-bracket">&#91;</span>80<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-81" class="reference"><a href="#cite_note-81"><span class="cite-bracket">&#91;</span>81<span class="cite-bracket">&#93;</span></a></sup> playing a decisive role in the stability, dynamics and evolution of soil ecosystems.<sup id="cite_ref-82" class="reference"><a href="#cite_note-82"><span class="cite-bracket">&#91;</span>82<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Biogenic_substance" title="Biogenic substance">Biogenic</a> soil <a href="/wiki/Volatile_organic_compound" title="Volatile organic compound">volatile organic compounds</a> are exchanged with the aboveground atmosphere, in which they are just 1–2 orders of magnitude lower than those from aboveground vegetation.<sup id="cite_ref-83" class="reference"><a href="#cite_note-83"><span class="cite-bracket">&#91;</span>83<span class="cite-bracket">&#93;</span></a></sup> </p><p>Humans can get some idea of the soil atmosphere through the well-known 'after-the-rain' scent, when infiltering rainwater flushes out the whole soil atmosphere after a drought period, or when soil is excavated,<sup id="cite_ref-84" class="reference"><a href="#cite_note-84"><span class="cite-bracket">&#91;</span>84<span class="cite-bracket">&#93;</span></a></sup> a bulk property attributed in a <a href="/wiki/Reductionist" class="mw-redirect" title="Reductionist">reductionist</a> manner to particular biochemical compounds such as <a href="/wiki/Petrichor" title="Petrichor">petrichor</a> or <a href="/wiki/Geosmin" title="Geosmin">geosmin</a>. </p> <div class="mw-heading mw-heading2"><h2 id="Solid_phase_(soil_matrix)"><span id="Solid_phase_.28soil_matrix.29"></span>Solid phase (soil matrix)</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=7" title="Edit section: Solid phase (soil matrix)"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Soil_matrix" title="Soil matrix">Soil matrix</a></div> <p>Soil particles can be classified by their chemical composition (<a href="/wiki/Mineralogy" title="Mineralogy">mineralogy</a>) as well as their size. The <a href="/wiki/Particle-size_distribution" title="Particle-size distribution">particle size distribution</a> of a soil, its texture, determines many of the properties of that soil, in particular <a href="/wiki/Hydraulic_conductivity" title="Hydraulic conductivity">hydraulic conductivity</a> and <a href="/wiki/Water_potential" title="Water potential">water potential</a>,<sup id="cite_ref-85" class="reference"><a href="#cite_note-85"><span class="cite-bracket">&#91;</span>85<span class="cite-bracket">&#93;</span></a></sup> but the <a href="/wiki/Mineralogy" title="Mineralogy">mineralogy</a> of those particles can strongly modify those properties. The mineralogy of the finest soil particles, clay, is especially important.<sup id="cite_ref-86" class="reference"><a href="#cite_note-86"><span class="cite-bracket">&#91;</span>86<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Soil_biodiversity">Soil biodiversity</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=8" title="Edit section: Soil biodiversity"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Large numbers of <a href="/wiki/Microorganism" title="Microorganism">microbes</a>, <a href="/wiki/Animal" title="Animal">animals</a>, <a href="/wiki/Plant" title="Plant">plants</a> and <a href="/wiki/Fungus" title="Fungus">fungi</a> are living in soil. However, <a href="/wiki/Biodiversity" title="Biodiversity">biodiversity</a> in soil is much harder to study as most of this life is invisible, hence estimates about soil biodiversity have been unsatisfactory. A recent study suggested that soil is likely home to 59 ± 15% of the species on Earth. <a href="/wiki/Enchytraeidae" title="Enchytraeidae">Enchytraeidae</a> (worms) have the greatest percentage of species in soil (98.6%), followed by fungi (90%), plants (85.5%), and termites (<a href="/wiki/Termite" title="Termite">Isoptera</a>) (84.2%). Many other groups of animals have substantial fractions of species living in soil, e.g. about 30% of <a href="/wiki/Insect" title="Insect">insects</a>, and close to 50% of <a href="/wiki/Arachnid" title="Arachnid">arachnids</a>.<sup id="cite_ref-87" class="reference"><a href="#cite_note-87"><span class="cite-bracket">&#91;</span>87<span class="cite-bracket">&#93;</span></a></sup> While most <a href="/wiki/Vertebrate" title="Vertebrate">vertebrates</a> live above ground (ignoring aquatic species), many species are <a href="/wiki/Fossorial" title="Fossorial">fossorial</a>, that is, they live in soil, such as most <a href="/wiki/Scolecophidia" title="Scolecophidia">blind snakes</a>. </p> <div class="mw-heading mw-heading2"><h2 id="Chemistry">Chemistry</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=9" title="Edit section: Chemistry"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">For the academic discipline, see <a href="/wiki/Soil_chemistry" title="Soil chemistry">Soil chemistry</a>.</div> <p>The chemistry of a soil determines its ability to supply available <a href="/wiki/Plant_nutrition" title="Plant nutrition">plant nutrients</a> and affects its physical properties and the health of its living population. In addition, a soil's chemistry also determines its <a href="/wiki/Corrosivity" class="mw-redirect" title="Corrosivity">corrosivity</a>, stability, and ability to <a href="/wiki/Sorption" title="Sorption">absorb</a> <a href="/wiki/Pollutants" class="mw-redirect" title="Pollutants">pollutants</a> and to filter water. It is the <a href="/wiki/Surface_chemistry" class="mw-redirect" title="Surface chemistry">surface chemistry</a> of mineral and organic <a href="/wiki/Colloids" class="mw-redirect" title="Colloids">colloids</a> that determines soil's chemical properties.<sup id="cite_ref-88" class="reference"><a href="#cite_note-88"><span class="cite-bracket">&#91;</span>88<span class="cite-bracket">&#93;</span></a></sup> A colloid is a small, insoluble particle ranging in size from 1 <a href="/wiki/Nanometer" class="mw-redirect" title="Nanometer">nanometer</a> to 1 <a href="/wiki/Micrometre" title="Micrometre">micrometer</a>, thus small enough to remain suspended by <a href="/wiki/Brownian_motion" title="Brownian motion">Brownian motion</a> in a fluid medium without settling.<sup id="cite_ref-89" class="reference"><a href="#cite_note-89"><span class="cite-bracket">&#91;</span>89<span class="cite-bracket">&#93;</span></a></sup> Most soils contain organic colloidal particles called <a href="/wiki/Humus" title="Humus">humus</a> as well as the inorganic colloidal particles of <a href="/wiki/Clays" class="mw-redirect" title="Clays">clays</a>. The very high <a href="/wiki/Specific_surface_area" title="Specific surface area">specific surface area</a> of colloids and their net <a href="/wiki/Electrical_charge" class="mw-redirect" title="Electrical charge">electrical charges</a> give soil its ability to hold and release <a href="/wiki/Ions" class="mw-redirect" title="Ions">ions</a>. Negatively charged sites on colloids attract and release <a href="/wiki/Cations" class="mw-redirect" title="Cations">cations</a> in what is referred to as <a href="/wiki/Cation_exchange" class="mw-redirect" title="Cation exchange">cation exchange</a>. <a href="/wiki/Cation-exchange_capacity" title="Cation-exchange capacity">Cation-exchange capacity</a> is the amount of exchangeable <a href="/wiki/Cations" class="mw-redirect" title="Cations">cations</a> per unit weight of dry soil and is expressed in terms of <a href="/wiki/Milliequivalents" class="mw-redirect" title="Milliequivalents">milliequivalents</a> of <a href="/wiki/Positively_charged" class="mw-redirect" title="Positively charged">positively charged</a> ions per 100&#160;grams of soil (or centimoles of positive charge per kilogram of soil; <a href="/wiki/Cation-exchange_capacity" title="Cation-exchange capacity">cmol<sub>c</sub>/kg</a>). Similarly, positively charged sites on colloids can attract and release <a href="/wiki/Anions" class="mw-redirect" title="Anions">anions</a> in the soil, giving the soil anion exchange capacity. </p> <div class="mw-heading mw-heading3"><h3 id="Cation_and_anion_exchange">Cation and anion exchange</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=10" title="Edit section: Cation and anion exchange"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Further information: <a href="/wiki/Cation-exchange_capacity" title="Cation-exchange capacity">Cation-exchange capacity</a></div> <p>The cation exchange, that takes place between colloids and soil water, <a href="/wiki/Buffer_solution" title="Buffer solution">buffers</a> (moderates) soil pH, alters soil structure, and purifies <a href="/wiki/Percolation" title="Percolation">percolating</a> water by adsorbing cations of all types, both useful and harmful. </p><p>The negative or positive charges on colloid particles make them able to hold cations or anions, respectively, to their surfaces. The charges result from four sources.<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977103–106_90-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977103–106-90"><span class="cite-bracket">&#91;</span>90<span class="cite-bracket">&#93;</span></a></sup> </p> <ol><li>Isomorphous substitution occurs in clay during its formation, when lower-valence cations substitute for higher-valence cations in the crystal structure.<sup id="cite_ref-&#80;MID10097044_91-0" class="reference"><a href="#cite_note-PMID10097044-91"><span class="cite-bracket">&#91;</span>91<span class="cite-bracket">&#93;</span></a></sup> Substitutions in the outermost layers are more effective than for the innermost layers, as the <a href="/wiki/Electric_charge" title="Electric charge">electric charge</a> strength drops off as the square of the distance. The net result is oxygen atoms with net negative charge and the ability to attract cations.</li> <li>Edge-of-clay oxygen atoms are not in balance ionically as the tetrahedral and octahedral structures are incomplete.<sup id="cite_ref-92" class="reference"><a href="#cite_note-92"><span class="cite-bracket">&#91;</span>92<span class="cite-bracket">&#93;</span></a></sup></li> <li><a href="/wiki/Hydroxyl" class="mw-redirect" title="Hydroxyl">Hydroxyls</a> may substitute for oxygens of the silica layers, a process called <a href="/wiki/Hydroxylation" title="Hydroxylation">hydroxylation</a>. When the hydrogens of the clay hydroxyls are ionised into solution, they leave the oxygen with a negative charge (anionic clays).<sup id="cite_ref-93" class="reference"><a href="#cite_note-93"><span class="cite-bracket">&#91;</span>93<span class="cite-bracket">&#93;</span></a></sup></li> <li>Hydrogens of humus hydroxyl groups may also be ionised into solution, leaving, similarly to clay, an oxygen with a negative charge.<sup id="cite_ref-94" class="reference"><a href="#cite_note-94"><span class="cite-bracket">&#91;</span>94<span class="cite-bracket">&#93;</span></a></sup></li></ol> <p>Cations held to the negatively charged colloids resist being washed downward by water and are out of reach of plant roots, thereby preserving the <a href="/wiki/Soil_fertility" title="Soil fertility">soil fertility</a> in areas of moderate rainfall and low temperatures.<sup id="cite_ref-95" class="reference"><a href="#cite_note-95"><span class="cite-bracket">&#91;</span>95<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-96" class="reference"><a href="#cite_note-96"><span class="cite-bracket">&#91;</span>96<span class="cite-bracket">&#93;</span></a></sup> </p><p>There is a hierarchy in the process of cation exchange on colloids, as cations differ in the strength of adsorption by the colloid and hence their ability to replace one another (<a href="/wiki/Ion_exchange" title="Ion exchange">ion exchange</a>). If present in equal amounts in the soil water solution: </p><p>Al<sup>3+</sup> replaces H<sup>+</sup> replaces Ca<sup>2+</sup> replaces Mg<sup>2+</sup> replaces K<sup>+</sup> same as <span class="chemf nowrap">NH<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">+</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span> replaces Na<sup>+</sup><sup id="cite_ref-97" class="reference"><a href="#cite_note-97"><span class="cite-bracket">&#91;</span>97<span class="cite-bracket">&#93;</span></a></sup> </p><p>If one cation is added in large amounts, it may replace the others by the sheer force of its numbers. This is called <a href="/wiki/Law_of_mass_action" title="Law of mass action">law of mass action</a>. This is largely what occurs with the addition of cationic <a href="/wiki/Fertilizer" title="Fertilizer">fertilisers</a> (<a href="/wiki/Potash" title="Potash">potash</a>, <a href="/wiki/Lime_(material)" title="Lime (material)">lime</a>).<sup id="cite_ref-98" class="reference"><a href="#cite_note-98"><span class="cite-bracket">&#91;</span>98<span class="cite-bracket">&#93;</span></a></sup> </p><p>As the soil solution becomes more acidic (low <a href="/wiki/PH" title="PH">pH</a>, meaning an abundance of H<sup>+</sup>), the other cations more weakly bound to colloids are pushed into solution as hydrogen ions occupy exchange sites (<a href="/wiki/Protonation" title="Protonation">protonation</a>). A low pH may cause the hydrogen of hydroxyl groups to be pulled into solution, leaving charged sites on the colloid available to be occupied by other cations. This <a href="/wiki/Ionization" title="Ionization">ionisation</a> of <a href="/wiki/Hydroxy_group" title="Hydroxy group">hydroxy groups</a> on the surface of soil colloids creates what is described as pH-dependent surface charges.<sup id="cite_ref-99" class="reference"><a href="#cite_note-99"><span class="cite-bracket">&#91;</span>99<span class="cite-bracket">&#93;</span></a></sup> Unlike permanent charges developed by <a href="/wiki/Isomorphous_replacement" title="Isomorphous replacement">isomorphous substitution</a>, pH-dependent charges are variable and increase with increasing pH.<sup id="cite_ref-CEC_100-0" class="reference"><a href="#cite_note-CEC-100"><span class="cite-bracket">&#91;</span>100<span class="cite-bracket">&#93;</span></a></sup> Freed cations can be made available to plants but are also prone to be leached from the soil, possibly making the soil less fertile.<sup id="cite_ref-101" class="reference"><a href="#cite_note-101"><span class="cite-bracket">&#91;</span>101<span class="cite-bracket">&#93;</span></a></sup> Plants are able to excrete H<sup>+</sup> into the soil through the synthesis of <a href="/wiki/Organic_acid" title="Organic acid">organic acids</a> and by that means, change the pH of the soil near the root and push cations off the colloids, thus making those available to the plant.<sup id="cite_ref-102" class="reference"><a href="#cite_note-102"><span class="cite-bracket">&#91;</span>102<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading4"><h4 id="Cation_exchange_capacity_(CEC)"><span id="Cation_exchange_capacity_.28CEC.29"></span>Cation exchange capacity (CEC)</h4><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=11" title="Edit section: Cation exchange capacity (CEC)"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p><a href="/wiki/Cation_exchange_capacity" class="mw-redirect" title="Cation exchange capacity">Cation exchange capacity</a> is the soil's ability to remove cations from the soil water solution and sequester those to be exchanged later as the plant roots release hydrogen ions to the solution.<sup id="cite_ref-103" class="reference"><a href="#cite_note-103"><span class="cite-bracket">&#91;</span>103<span class="cite-bracket">&#93;</span></a></sup> CEC is the amount of exchangeable hydrogen cation (H<sup>+</sup>) that will combine with 100&#160;grams dry weight of soil and whose measure is one milliequivalents per 100&#160;grams of soil (1&#160;meq/100&#160;g). Hydrogen ions have a single charge and one-thousandth of a gram of hydrogen ions per 100&#160;grams dry soil gives a measure of one milliequivalent of hydrogen ion. Calcium, with an atomic weight 40 times that of hydrogen and with a valence of two, converts to <span class="nowrap">(40 ÷ 2) × 1 milliequivalent</span> = 20 milliequivalents of hydrogen ion per 100&#160;grams of dry soil or 20&#160;meq/100&#160;g.<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977114_104-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977114-104"><span class="cite-bracket">&#91;</span>104<span class="cite-bracket">&#93;</span></a></sup> The modern measure of CEC is expressed as centimoles of positive charge per kilogram (cmol/kg) of oven-dry soil. </p><p>Most of the soil's CEC occurs on clay and humus colloids, and the lack of those in hot, humid, wet climates (such as <a href="/wiki/Tropical_rainforest" title="Tropical rainforest">tropical rainforests</a>), due to leaching and decomposition, respectively, explains the apparent sterility of tropical soils.<sup id="cite_ref-105" class="reference"><a href="#cite_note-105"><span class="cite-bracket">&#91;</span>105<span class="cite-bracket">&#93;</span></a></sup> Live plant roots also have some CEC, linked to their specific surface area.<sup id="cite_ref-106" class="reference"><a href="#cite_note-106"><span class="cite-bracket">&#91;</span>106<span class="cite-bracket">&#93;</span></a></sup> </p> <table class="wikitable" style="border-spacing: 5px; margin:auto;"> <caption>Cation exchange capacity for soils; soil textures; soil colloids<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977115–116_107-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977115–116-107"><span class="cite-bracket">&#91;</span>107<span class="cite-bracket">&#93;</span></a></sup> </caption> <tbody><tr> <th scope="col" style="width:200px;">Soil </th> <th scope="col" style="width:100px;">State </th> <th scope="col" style="width:100px;">CEC meq/100&#160;g </th></tr> <tr> <td>Charlotte fine sand</td> <td>Florida</td> <td>1.0 </td></tr> <tr> <td>Ruston fine sandy loam</td> <td>Texas</td> <td>1.9 </td></tr> <tr> <td>Glouchester loam</td> <td>New Jersey</td> <td>11.9 </td></tr> <tr> <td>Grundy silt loam</td> <td>Illinois</td> <td>26.3 </td></tr> <tr> <td>Gleason clay loam</td> <td>California</td> <td>31.6 </td></tr> <tr> <td>Susquehanna clay loam</td> <td>Alabama</td> <td>34.3 </td></tr> <tr> <td>Davie mucky fine sand</td> <td>Florida</td> <td>100.8 </td></tr> <tr> <td>Sands</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>1–5 </td></tr> <tr> <td>Fine sandy loams</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>5–10 </td></tr> <tr> <td>Loams and silt loams</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>5–15 </td></tr> <tr> <td>Clay loams</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>15–30 </td></tr> <tr> <td>Clays</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>over 30 </td></tr> <tr> <td>Sesquioxides</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>0–3 </td></tr> <tr> <td>Kaolinite</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>3–15 </td></tr> <tr> <td>Illite</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>25–40 </td></tr> <tr> <td>Montmorillonite</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>60–100 </td></tr> <tr> <td>Vermiculite (similar to illite)</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>80–150 </td></tr> <tr> <td>Humus</td> <td data-sort-value="" style="background: var(--background-color-interactive, #ececec); color: var(--color-base, inherit); vertical-align: middle; text-align: center;" class="table-na">—</td> <td>100–300 </td></tr></tbody></table> <div class="mw-heading mw-heading4"><h4 id="Anion_exchange_capacity_(AEC)"><span id="Anion_exchange_capacity_.28AEC.29"></span>Anion exchange capacity (AEC)</h4><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=12" title="Edit section: Anion exchange capacity (AEC)"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Anion exchange capacity is the soil's ability to remove anions (such as <a href="/wiki/Nitrate" title="Nitrate">nitrate</a>, <a href="/wiki/Phosphate" title="Phosphate">phosphate</a>) from the soil water solution and sequester those for later exchange as the plant roots release carbonate anions to the soil water solution.<sup id="cite_ref-Hinsinger_2001_173–195_108-0" class="reference"><a href="#cite_note-Hinsinger_2001_173–195-108"><span class="cite-bracket">&#91;</span>108<span class="cite-bracket">&#93;</span></a></sup> Those colloids which have low CEC tend to have some AEC. Amorphous and sesquioxide clays have the highest AEC,<sup id="cite_ref-109" class="reference"><a href="#cite_note-109"><span class="cite-bracket">&#91;</span>109<span class="cite-bracket">&#93;</span></a></sup> followed by the iron oxides.<sup id="cite_ref-110" class="reference"><a href="#cite_note-110"><span class="cite-bracket">&#91;</span>110<span class="cite-bracket">&#93;</span></a></sup> Levels of AEC are much lower than for CEC, because of the generally higher rate of positively (versus negatively) charged surfaces on soil colloids, to the exception of variable-charge soils.<sup id="cite_ref-111" class="reference"><a href="#cite_note-111"><span class="cite-bracket">&#91;</span>111<span class="cite-bracket">&#93;</span></a></sup> Phosphates tend to be held at anion exchange sites.<sup id="cite_ref-112" class="reference"><a href="#cite_note-112"><span class="cite-bracket">&#91;</span>112<span class="cite-bracket">&#93;</span></a></sup> </p><p>Iron and aluminum hydroxide clays are able to exchange their hydroxide anions (OH<sup>−</sup>) for other anions.<sup id="cite_ref-Hinsinger_2001_173–195_108-1" class="reference"><a href="#cite_note-Hinsinger_2001_173–195-108"><span class="cite-bracket">&#91;</span>108<span class="cite-bracket">&#93;</span></a></sup> The order reflecting the strength of anion adhesion is as follows: </p> <dl><dd><span class="chemf nowrap">H<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline"></sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">2</sub></span></span>PO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span> replaces <span class="chemf nowrap">SO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">2−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span> replaces <span class="chemf nowrap">NO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">3</sub></span></span></span> replaces Cl<sup>−</sup></dd></dl> <p>The amount of exchangeable anions is of a magnitude of tenths to a few milliequivalents per 100&#160;g dry soil.<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977115–116_107-1" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977115–116-107"><span class="cite-bracket">&#91;</span>107<span class="cite-bracket">&#93;</span></a></sup> As pH rises, there are relatively more hydroxyls, which will displace anions from the colloids and force them into solution and out of storage; hence AEC decreases with increasing pH (alkalinity).<sup id="cite_ref-113" class="reference"><a href="#cite_note-113"><span class="cite-bracket">&#91;</span>113<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Reactivity_(pH)"><span id="Reactivity_.28pH.29"></span>Reactivity (pH)</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=13" title="Edit section: Reactivity (pH)"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main articles: <a href="/wiki/Soil_pH" title="Soil pH">Soil pH</a> and <a href="/wiki/Soil_pH#Effect_of_soil_pH_on_plant_growth" title="Soil pH">Soil pH §&#160;Effect of soil pH on plant growth</a></div> <p>Soil reactivity is expressed in terms of pH and is a measure of the <a href="/wiki/Acid" title="Acid">acidity</a> or <a href="/wiki/Base_(chemistry)" title="Base (chemistry)">alkalinity</a> of the soil. More precisely, it is a measure of <a href="/wiki/Hydronium" title="Hydronium">hydronium</a> concentration in an aqueous solution and ranges in values from 0 to 14 (acidic to basic) but practically speaking for soils, pH ranges from 3.5 to 9.5, as pH values beyond those extremes are toxic to life forms.<sup id="cite_ref-114" class="reference"><a href="#cite_note-114"><span class="cite-bracket">&#91;</span>114<span class="cite-bracket">&#93;</span></a></sup> </p><p>At 25&#160;°C an aqueous solution that has a pH of 3.5 has 10<sup>−3.5</sup> <a href="/wiki/Mole_(unit)" title="Mole (unit)">moles</a> H<sub>3</sub>O<sup>+</sup> (hydronium ions) per litre of solution (and also 10<sup>−10.5</sup> moles per litre OH<sup>−</sup>). A pH of 7, defined as neutral, has 10<sup>−7</sup> moles of hydronium ions per litre of solution and also 10<sup>−7</sup> moles of OH<sup>−</sup> per litre; since the two concentrations are equal, they are said to neutralise each other. A pH of 9.5 has 10<sup>−9.5</sup> moles hydronium ions per litre of solution (and also 10<sup>−2.5</sup> moles per litre OH<sup>−</sup>). A pH of 3.5 has one million times more hydronium ions per litre than a solution with pH of 9.5 (<span class="nowrap">9.5 − 3.5 = 6</span> or 10<sup>6</sup>) and is more acidic.<sup id="cite_ref-115" class="reference"><a href="#cite_note-115"><span class="cite-bracket">&#91;</span>115<span class="cite-bracket">&#93;</span></a></sup> </p><p>The effect of pH on a soil is to remove from the soil or to make available certain ions. Soils with high acidity tend to have toxic amounts of <a href="/wiki/Aluminium" title="Aluminium">aluminium</a> and <a href="/wiki/Manganese" title="Manganese">manganese</a>.<sup id="cite_ref-116" class="reference"><a href="#cite_note-116"><span class="cite-bracket">&#91;</span>116<span class="cite-bracket">&#93;</span></a></sup> As a result of a trade-off between toxicity and requirement most nutrients are better available to plants at moderate pH,<sup id="cite_ref-117" class="reference"><a href="#cite_note-117"><span class="cite-bracket">&#91;</span>117<span class="cite-bracket">&#93;</span></a></sup> although most minerals are more soluble in acid soils. Soil organisms are hindered by high acidity, and most agricultural crops do best with mineral soils of pH&#160;6.5 and organic soils of pH&#160;5.5.<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977116–117_118-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977116–117-118"><span class="cite-bracket">&#91;</span>118<span class="cite-bracket">&#93;</span></a></sup> Given that at low pH toxic metals (e.g. cadmium, zinc, lead) are positively charged as cations and organic pollutants are in non-ionic form, thus both made more available to organisms,<sup id="cite_ref-119" class="reference"><a href="#cite_note-119"><span class="cite-bracket">&#91;</span>119<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-120" class="reference"><a href="#cite_note-120"><span class="cite-bracket">&#91;</span>120<span class="cite-bracket">&#93;</span></a></sup> it has been suggested that plants, animals and microbes commonly living in acid soils are <a href="/wiki/Pre-adapted" class="mw-redirect" title="Pre-adapted">pre-adapted</a> to every kind of pollution, whether of natural or human origin.<sup id="cite_ref-121" class="reference"><a href="#cite_note-121"><span class="cite-bracket">&#91;</span>121<span class="cite-bracket">&#93;</span></a></sup> </p><p>In high rainfall areas, soils tend to acidify as the basic cations are forced off the soil colloids by the mass action of hydronium ions from usual or unusual <a href="/wiki/Acid_rain" title="Acid rain">rain acidity</a> against those attached to the colloids. High rainfall rates can then wash the nutrients out, leaving the soil inhabited only by those organisms which are particularly efficient to uptake nutrients in very acid conditions, like in <a href="/wiki/Tropical_rainforests" class="mw-redirect" title="Tropical rainforests">tropical rainforests</a>.<sup id="cite_ref-122" class="reference"><a href="#cite_note-122"><span class="cite-bracket">&#91;</span>122<span class="cite-bracket">&#93;</span></a></sup> Once the colloids are saturated with H<sub>3</sub>O<sup>+</sup>, the addition of any more hydronium ions or aluminum hydroxyl cations drives the pH even lower (more acidic) as the soil has been left with no buffering capacity.<sup id="cite_ref-123" class="reference"><a href="#cite_note-123"><span class="cite-bracket">&#91;</span>123<span class="cite-bracket">&#93;</span></a></sup> In areas of extreme rainfall and high temperatures, the clay and humus may be washed out, further reducing the buffering capacity of the soil.<sup id="cite_ref-124" class="reference"><a href="#cite_note-124"><span class="cite-bracket">&#91;</span>124<span class="cite-bracket">&#93;</span></a></sup> In low rainfall areas, unleached calcium pushes pH to 8.5 and with the addition of exchangeable sodium, soils may reach pH&#160;10.<sup id="cite_ref-125" class="reference"><a href="#cite_note-125"><span class="cite-bracket">&#91;</span>125<span class="cite-bracket">&#93;</span></a></sup> Beyond a pH of 9, plant growth is reduced.<sup id="cite_ref-126" class="reference"><a href="#cite_note-126"><span class="cite-bracket">&#91;</span>126<span class="cite-bracket">&#93;</span></a></sup> High pH results in low <a href="/wiki/Micro-nutrient" class="mw-redirect" title="Micro-nutrient">micro-nutrient</a> mobility, but water-soluble <a href="/wiki/Chelates" class="mw-redirect" title="Chelates">chelates</a> of those nutrients can correct the deficit.<sup id="cite_ref-127" class="reference"><a href="#cite_note-127"><span class="cite-bracket">&#91;</span>127<span class="cite-bracket">&#93;</span></a></sup> Sodium can be reduced by the addition of gypsum (calcium sulphate) as calcium adheres to clay more tightly than does sodium causing sodium to be pushed into the soil water solution where it can be washed out by an abundance of water.<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977116–119_128-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977116–119-128"><span class="cite-bracket">&#91;</span>128<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-129" class="reference"><a href="#cite_note-129"><span class="cite-bracket">&#91;</span>129<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading4"><h4 id="Base_saturation_percentage">Base saturation percentage</h4><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=14" title="Edit section: Base saturation percentage"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>There are acid-forming cations (e.g. hydronium, aluminium, iron) and there are base-forming cations (e.g. calcium, magnesium, sodium). The fraction of the negatively-charged soil colloid exchange sites (CEC) that are occupied by base-forming cations is called <a href="/wiki/Base_saturation" class="mw-redirect" title="Base saturation">base saturation</a>. If a soil has a CEC of 20&#160;meq and 5&#160;meq are aluminium and hydronium cations (acid-forming), the remainder of positions on the colloids (<span class="nowrap">20 − 5 = 15 meq</span>) are assumed occupied by base-forming cations, so that the base saturation is <span class="nowrap">15 ÷ 20 × 100% = 75%</span> (the compliment 25% is assumed acid-forming cations). Base saturation is almost in direct proportion to pH (it increases with increasing pH).<sup id="cite_ref-130" class="reference"><a href="#cite_note-130"><span class="cite-bracket">&#91;</span>130<span class="cite-bracket">&#93;</span></a></sup> It is of use in calculating the amount of lime needed to neutralise an acid soil (lime requirement). The amount of lime needed to neutralize a soil must take account of the amount of acid forming ions on the colloids (exchangeable acidity), not just those in the soil water solution (free acidity).<sup id="cite_ref-131" class="reference"><a href="#cite_note-131"><span class="cite-bracket">&#91;</span>131<span class="cite-bracket">&#93;</span></a></sup> The addition of enough lime to neutralize the soil water solution will be insufficient to change the pH, as the acid forming cations stored on the soil colloids will tend to restore the original pH condition as they are pushed off those colloids by the calcium of the added lime.<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977119–120_132-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977119–120-132"><span class="cite-bracket">&#91;</span>132<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading4"><h4 id="Buffering">Buffering</h4><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=15" title="Edit section: Buffering"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Further information: <a href="/wiki/Soil_conditioner" title="Soil conditioner">Soil conditioner</a></div> <p>The resistance of soil to change in pH, as a result of the addition of acid or basic material, is a measure of the buffering capacity of a soil and (for a particular soil type) increases as the CEC increases. Hence, pure sand has almost no buffering ability, though soils high in colloids (whether mineral or organic) have high <a href="/wiki/Buffering_capacity" class="mw-redirect" title="Buffering capacity">buffering capacity</a>.<sup id="cite_ref-133" class="reference"><a href="#cite_note-133"><span class="cite-bracket">&#91;</span>133<span class="cite-bracket">&#93;</span></a></sup> Buffering occurs by cation exchange and <a href="/wiki/Neutralization_(chemistry)" title="Neutralization (chemistry)">neutralisation</a>. However, colloids are not the only regulators of soil pH. The role of <a href="/wiki/Carbonates" class="mw-redirect" title="Carbonates">carbonates</a> should be underlined, too.<sup id="cite_ref-134" class="reference"><a href="#cite_note-134"><span class="cite-bracket">&#91;</span>134<span class="cite-bracket">&#93;</span></a></sup> More generally, according to pH levels, several buffer systems take precedence over each other, from <a href="/wiki/Calcium_carbonate" title="Calcium carbonate">calcium carbonate</a> <a href="/wiki/Buffer_range" class="mw-redirect" title="Buffer range">buffer range</a> to iron buffer range.<sup id="cite_ref-135" class="reference"><a href="#cite_note-135"><span class="cite-bracket">&#91;</span>135<span class="cite-bracket">&#93;</span></a></sup> </p><p>The addition of a small amount of highly basic aqueous ammonia to a soil will cause the <a href="/wiki/Ammonium" title="Ammonium">ammonium</a> to displace hydronium ions from the colloids, and the end product is water and colloidally fixed ammonium, but little permanent change overall in soil pH. </p><p>The addition of a small amount of <a href="/wiki/Liming_(soil)" title="Liming (soil)">lime</a>, Ca(OH)<sub>2</sub>, will displace hydronium ions from the soil colloids, causing the fixation of calcium to colloids and the evolution of CO<sub>2</sub> and water, with little permanent change in soil pH. </p><p>The above are examples of the buffering of soil pH. The general principal is that an increase in a particular cation in the soil water solution will cause that cation to be fixed to colloids (buffered) and a decrease in solution of that cation will cause it to be withdrawn from the colloid and moved into solution (buffered). The degree of buffering is often related to the CEC of the soil; the greater the CEC, the greater the buffering capacity of the soil.<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977120–121_136-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977120–121-136"><span class="cite-bracket">&#91;</span>136<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Redox">Redox</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=16" title="Edit section: Redox"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Redox#Redox_reactions_in_soils" title="Redox">Redox §&#160;Redox_reactions_in_soils</a></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">See also: <a href="/wiki/Table_of_standard_reduction_potentials_for_half-reactions_important_in_biochemistry" title="Table of standard reduction potentials for half-reactions important in biochemistry">Table of standard reduction potentials for half-reactions important in biochemistry</a></div> <p>Soil chemical reactions involve some combination of proton and electron transfer. Oxidation occurs if there is a loss of electrons in the transfer process while reduction occurs if there is a gain of electrons. <a href="/wiki/Reduction_potential" title="Reduction potential">Reduction potential</a> is measured in volts or millivolts. Soil microbial communities develop along <a href="/wiki/Electron_transport_chain" title="Electron transport chain">electron transport chains</a>, forming electrically conductive <a href="/wiki/Geobacter#Biofilm_conductivity" title="Geobacter">biofilms</a>, and developing networks of <a href="/wiki/Bacterial_nanowires" title="Bacterial nanowires">bacterial nanowires</a>. </p><p>Redox factors in soil development, where formation of <a href="/wiki/Redoximorphic_features" title="Redoximorphic features">redoximorphic color features</a> provides critical information for soil interpretation. Understanding the <a href="/wiki/Redox_gradient#Terrestrial_Environments" title="Redox gradient">redox gradient</a> is important to managing carbon sequestration, bioremediation, <a href="/wiki/Pedosphere#Redox_conditions_in_wetland_soils" title="Pedosphere">wetland delineation</a>, and <a href="/wiki/Soil-based_microbial_fuel_cell" class="mw-redirect" title="Soil-based microbial fuel cell">soil-based microbial fuel cells</a>. </p> <div class="mw-heading mw-heading2"><h2 id="Nutrients">Nutrients</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=17" title="Edit section: Nutrients"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <table class="wikitable sortable floatright"> <caption>Plant nutrients, their chemical symbols, and the ionic forms common in soils and available for plant uptake<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977125_137-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977125-137"><span class="cite-bracket">&#91;</span>137<span class="cite-bracket">&#93;</span></a></sup> </caption> <tbody><tr> <th>Element</th> <th>Symbol</th> <th>Ion or molecule </th></tr> <tr> <td>Carbon</td> <td>C</td> <td>CO<sub>2</sub> (mostly through leaves) </td></tr> <tr> <td>Hydrogen</td> <td>H</td> <td>H<sup>+</sup>, H<sub>2</sub>O (water) </td></tr> <tr> <td>Oxygen</td> <td>O</td> <td>O<sup>2−</sup>, OH<sup>−</sup>, <span class="chemf nowrap">CO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">2−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">3</sub></span></span></span>, <span class="chemf nowrap">SO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">2−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span>, CO<sub>2</sub> </td></tr> <tr> <td>Phosphorus</td> <td>P</td> <td><span class="chemf nowrap">H<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline"></sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">2</sub></span></span>PO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span>, <span class="chemf nowrap">HPO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">2−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span> (phosphates) </td></tr> <tr> <td>Potassium</td> <td>K</td> <td>K<sup>+</sup> </td></tr> <tr> <td>Nitrogen</td> <td>N</td> <td><span class="chemf nowrap">NH<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">+</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span>, <span class="chemf nowrap">NO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">3</sub></span></span></span> (ammonium, nitrate) </td></tr> <tr> <td>Sulfur</td> <td>S</td> <td><span class="chemf nowrap">SO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">2−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span> </td></tr> <tr> <td>Calcium</td> <td>Ca</td> <td>Ca<sup>2+</sup> </td></tr> <tr> <td>Iron</td> <td>Fe</td> <td>Fe<sup>2+</sup>, Fe<sup>3+</sup> (ferrous, ferric) </td></tr> <tr> <td>Magnesium</td> <td>Mg</td> <td>Mg<sup>2+</sup> </td></tr> <tr> <td>Boron</td> <td>B</td> <td>H<sub>3</sub>BO<sub>3</sub>, <span class="chemf nowrap">H<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline"></sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">2</sub></span></span>BO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">3</sub></span></span></span>, <span class="chemf nowrap">B(OH)<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span> </td></tr> <tr> <td>Manganese</td> <td>Mn</td> <td>Mn<sup>2+</sup> </td></tr> <tr> <td>Copper</td> <td>Cu</td> <td>Cu<sup>2+</sup> </td></tr> <tr> <td>Zinc</td> <td>Zn</td> <td>Zn<sup>2+</sup> </td></tr> <tr> <td>Molybdenum</td> <td>Mo</td> <td><span class="chemf nowrap">MoO<span class="nowrap"><span style="display:inline-block;margin-bottom:-0.3em;vertical-align:-0.4em;line-height:1em;font-size:80%;text-align:left"><sup style="font-size:inherit;line-height:inherit;vertical-align:baseline">2−</sup><br /><sub style="font-size:inherit;line-height:inherit;vertical-align:baseline">4</sub></span></span></span> (molybdate) </td></tr> <tr> <td>Chlorine</td> <td>Cl</td> <td>Cl<sup>−</sup> (chloride) </td></tr></tbody></table> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main articles: <a href="/wiki/Plant_nutrients_in_soil" title="Plant nutrients in soil">Plant nutrients in soil</a>, <a href="/wiki/Plant_nutrition" title="Plant nutrition">Plant nutrition</a>, and <a href="/wiki/Soil_pH#Effect_of_soil_pH_on_plant_growth" title="Soil pH">Soil pH §&#160;Effect of soil pH on plant growth</a></div> <p>Seventeen elements or nutrients are essential for plant growth and reproduction. They are <a href="/wiki/Carbon" title="Carbon">carbon</a> (C), <a href="/wiki/Hydrogen" title="Hydrogen">hydrogen</a> (H), <a href="/wiki/Oxygen" title="Oxygen">oxygen</a> (O), <a href="/wiki/Nitrogen" title="Nitrogen">nitrogen</a> (N), <a href="/wiki/Phosphorus" title="Phosphorus">phosphorus</a> (P), <a href="/wiki/Potassium" title="Potassium">potassium</a> (K), <a href="/wiki/Sulfur" title="Sulfur">sulfur</a> (S), <a href="/wiki/Calcium" title="Calcium">calcium</a> (Ca), <a href="/wiki/Magnesium" title="Magnesium">magnesium</a> (Mg), <a href="/wiki/Iron" title="Iron">iron</a> (Fe), <a href="/wiki/Boron" title="Boron">boron</a> (B), manganese (Mn), <a href="/wiki/Copper" title="Copper">copper</a> (Cu), <a href="/wiki/Zinc" title="Zinc">zinc</a> (Zn), <a href="/wiki/Molybdenum" title="Molybdenum">molybdenum</a> (Mo), <a href="/wiki/Nickel" title="Nickel">nickel</a> (Ni) and <a href="/wiki/Chlorine" title="Chlorine">chlorine</a> (Cl).<sup id="cite_ref-FOOTNOTEDean195780_138-0" class="reference"><a href="#cite_note-FOOTNOTEDean195780-138"><span class="cite-bracket">&#91;</span>138<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-FOOTNOTERussel1957123–125_139-0" class="reference"><a href="#cite_note-FOOTNOTERussel1957123–125-139"><span class="cite-bracket">&#91;</span>139<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-BradyWeil_140-0" class="reference"><a href="#cite_note-BradyWeil-140"><span class="cite-bracket">&#91;</span>140<span class="cite-bracket">&#93;</span></a></sup> Nutrients required for plants to complete their life cycle are considered <a href="/wiki/Essential_nutrients" class="mw-redirect" title="Essential nutrients">essential nutrients</a>. Nutrients that enhance the growth of plants but are not necessary to complete the plant's life cycle are considered non-essential. With the exception of carbon, hydrogen and oxygen, which are supplied by carbon dioxide and water, and nitrogen, provided through nitrogen fixation,<sup id="cite_ref-BradyWeil_140-1" class="reference"><a href="#cite_note-BradyWeil-140"><span class="cite-bracket">&#91;</span>140<span class="cite-bracket">&#93;</span></a></sup> the nutrients derive originally from the mineral component of the soil. The <a href="/wiki/Law_of_the_Minimum" class="mw-redirect" title="Law of the Minimum">Law of the Minimum</a> expresses that when the available form of a nutrient is not in enough proportion in the soil solution, then other nutrients cannot be taken up at an optimum rate by a plant.<sup id="cite_ref-141" class="reference"><a href="#cite_note-141"><span class="cite-bracket">&#91;</span>141<span class="cite-bracket">&#93;</span></a></sup> A particular nutrient ratio of the soil solution is thus mandatory for optimizing plant growth, a value which might differ from nutrient ratios calculated from plant composition.<sup id="cite_ref-142" class="reference"><a href="#cite_note-142"><span class="cite-bracket">&#91;</span>142<span class="cite-bracket">&#93;</span></a></sup> </p><p>Plant uptake of nutrients can only proceed when they are present in a plant-available form. In most situations, nutrients are absorbed in an <a href="/wiki/Ionic_compound" class="mw-redirect" title="Ionic compound">ionic</a> form from (or together with) soil water. Although minerals are the origin of most nutrients, and the bulk of most nutrient elements in the soil is held in crystalline form within <a href="/wiki/Primary_mineral" title="Primary mineral">primary</a> and <a href="/wiki/Secondary_mineral" class="mw-redirect" title="Secondary mineral">secondary minerals</a>, they weather too slowly to support rapid plant growth. For example, the application of finely ground minerals, <a href="/wiki/Feldspar" title="Feldspar">feldspar</a> and <a href="/wiki/Apatite" title="Apatite">apatite</a>, to soil seldom provides the necessary amounts of potassium and phosphorus at a rate sufficient for good plant growth, as most of the nutrients remain bound in the crystals of those minerals.<sup id="cite_ref-FOOTNOTEDean195780–81_143-0" class="reference"><a href="#cite_note-FOOTNOTEDean195780–81-143"><span class="cite-bracket">&#91;</span>143<span class="cite-bracket">&#93;</span></a></sup> </p><p>The nutrients adsorbed onto the surfaces of clay colloids and soil organic matter provide a more accessible reservoir of many plant nutrients (e.g. K, Ca, Mg, P, Zn). As plants absorb the nutrients from the soil water, the soluble pool is replenished from the surface-bound pool. The decomposition of soil organic matter by microorganisms is another mechanism whereby the soluble pool of nutrients is replenished – this is important for the supply of plant-available N, S, P, and B from soil.<sup id="cite_ref-Roy2006Chapter4_144-0" class="reference"><a href="#cite_note-Roy2006Chapter4-144"><span class="cite-bracket">&#91;</span>144<span class="cite-bracket">&#93;</span></a></sup> </p><p>Gram for gram, the capacity of <a href="/wiki/Humus" title="Humus">humus</a> to hold nutrients and water is far greater than that of clay minerals, most of the soil <a href="/wiki/Cation-exchange_capacity" title="Cation-exchange capacity">cation exchange capacity</a> arising from charged <a href="/wiki/Carboxylic" class="mw-redirect" title="Carboxylic">carboxylic</a> groups on organic matter.<sup id="cite_ref-145" class="reference"><a href="#cite_note-145"><span class="cite-bracket">&#91;</span>145<span class="cite-bracket">&#93;</span></a></sup> However, despite the great capacity of humus to retain water once water-soaked, its high <a href="/wiki/Hydrophobicity" class="mw-redirect" title="Hydrophobicity">hydrophobicity</a> decreases its <a href="/wiki/Wettability" class="mw-redirect" title="Wettability">wettability</a> once dry.<sup id="cite_ref-146" class="reference"><a href="#cite_note-146"><span class="cite-bracket">&#91;</span>146<span class="cite-bracket">&#93;</span></a></sup> All in all, small amounts of humus may remarkably increase the soil's capacity to promote plant growth.<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna1977123–131_147-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna1977123–131-147"><span class="cite-bracket">&#91;</span>147<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Roy2006Chapter4_144-1" class="reference"><a href="#cite_note-Roy2006Chapter4-144"><span class="cite-bracket">&#91;</span>144<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Soil_organic_matter">Soil organic matter</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=18" title="Edit section: Soil organic matter"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Soil_organic_matter" title="Soil organic matter">Soil organic matter</a></div><style data-mw-deduplicate="TemplateStyles:r1251242444">.mw-parser-output .ambox{border:1px solid #a2a9b1;border-left:10px solid #36c;background-color:#fbfbfb;box-sizing:border-box}.mw-parser-output .ambox+link+.ambox,.mw-parser-output .ambox+link+style+.ambox,.mw-parser-output .ambox+link+link+.ambox,.mw-parser-output .ambox+.mw-empty-elt+link+.ambox,.mw-parser-output .ambox+.mw-empty-elt+link+style+.ambox,.mw-parser-output .ambox+.mw-empty-elt+link+link+.ambox{margin-top:-1px}html body.mediawiki .mw-parser-output .ambox.mbox-small-left{margin:4px 1em 4px 0;overflow:hidden;width:238px;border-collapse:collapse;font-size:88%;line-height:1.25em}.mw-parser-output .ambox-speedy{border-left:10px solid #b32424;background-color:#fee7e6}.mw-parser-output .ambox-delete{border-left:10px solid #b32424}.mw-parser-output .ambox-content{border-left:10px solid #f28500}.mw-parser-output .ambox-style{border-left:10px solid #fc3}.mw-parser-output .ambox-move{border-left:10px solid #9932cc}.mw-parser-output .ambox-protection{border-left:10px solid #a2a9b1}.mw-parser-output .ambox .mbox-text{border:none;padding:0.25em 0.5em;width:100%}.mw-parser-output .ambox .mbox-image{border:none;padding:2px 0 2px 0.5em;text-align:center}.mw-parser-output .ambox .mbox-imageright{border:none;padding:2px 0.5em 2px 0;text-align:center}.mw-parser-output .ambox .mbox-empty-cell{border:none;padding:0;width:1px}.mw-parser-output .ambox .mbox-image-div{width:52px}@media(min-width:720px){.mw-parser-output .ambox{margin:0 10%}}@media print{body.ns-0 .mw-parser-output .ambox{display:none!important}}</style><table class="box-Overly_detailed plainlinks metadata ambox ambox-style ambox-overly_detailed" role="presentation"><tbody><tr><td class="mbox-image"><div class="mbox-image-div"><span typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/f/f2/Edit-clear.svg/40px-Edit-clear.svg.png" decoding="async" width="40" height="40" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/en/thumb/f/f2/Edit-clear.svg/60px-Edit-clear.svg.png 1.5x, //upload.wikimedia.org/wikipedia/en/thumb/f/f2/Edit-clear.svg/80px-Edit-clear.svg.png 2x" data-file-width="48" data-file-height="48" /></span></span></div></td><td class="mbox-text"><div class="mbox-text-span">This section <b>may contain an excessive amount of intricate detail that may interest only a particular audience</b>. <b>Specifically, details could be moved into main article</b>.<span class="hide-when-compact"> Please help by <a href="/wiki/Wikipedia:Content_forking#Article_spinoffs:_.22Summary_style.22_meta-articles_and_summary_sections" class="mw-redirect" title="Wikipedia:Content forking">spinning off</a> or <a href="/wiki/Wikipedia:Handling_trivia#Recommendations_for_handling_trivia" title="Wikipedia:Handling trivia">relocating</a> any relevant information, and removing excessive detail that may be against <a href="/wiki/Wikipedia:What_Wikipedia_is_not" title="Wikipedia:What Wikipedia is not">Wikipedia's inclusion policy</a>.</span> <span class="date-container"><i>(<span class="date">April 2021</span>)</i></span><span class="hide-when-compact"><i> (<small><a href="/wiki/Help:Maintenance_template_removal" title="Help:Maintenance template removal">Learn how and when to remove this message</a></small>)</i></span></div></td></tr></tbody></table> <p>The organic material in soil is made up of <a href="/wiki/Organic_compounds" class="mw-redirect" title="Organic compounds">organic compounds</a> and includes plant, animal and microbial material, both living and dead. A typical soil has a biomass composition of 70% microorganisms, 22% macrofauna, and 8% roots. The living component of an acre of soil may include 900&#160;lb of earthworms, 2400&#160;lb of fungi, 1500&#160;lb of bacteria, 133&#160;lb of protozoa and 890&#160;lb of arthropods and algae.<sup id="cite_ref-148" class="reference"><a href="#cite_note-148"><span class="cite-bracket">&#91;</span>148<span class="cite-bracket">&#93;</span></a></sup> </p><p>A few percent of the soil organic matter, with small <a href="/wiki/Residence_time" title="Residence time">residence time</a>, consists of the microbial <a href="/wiki/Biomass" title="Biomass">biomass</a> and <a href="/wiki/Metabolites" class="mw-redirect" title="Metabolites">metabolites</a> of bacteria, molds, and actinomycetes that work to break down the dead organic matter.<sup id="cite_ref-149" class="reference"><a href="#cite_note-149"><span class="cite-bracket">&#91;</span>149<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-150" class="reference"><a href="#cite_note-150"><span class="cite-bracket">&#91;</span>150<span class="cite-bracket">&#93;</span></a></sup> Were it not for the action of these micro-organisms, the entire carbon dioxide part of the atmosphere would be sequestered as organic matter in the soil. However, in the same time soil microbes contribute to <a href="/wiki/Carbon_sequestration" title="Carbon sequestration">carbon sequestration</a> in the topsoil through the formation of stable humus.<sup id="cite_ref-151" class="reference"><a href="#cite_note-151"><span class="cite-bracket">&#91;</span>151<span class="cite-bracket">&#93;</span></a></sup> In the aim to sequester more carbon in the soil for alleviating the <a href="/wiki/Greenhouse_effect" title="Greenhouse effect">greenhouse effect</a> it would be more efficient in the long-term to stimulate <a href="/wiki/Humification" class="mw-redirect" title="Humification">humification</a> than to decrease litter <a href="/wiki/Decomposition" title="Decomposition">decomposition</a>.<sup id="cite_ref-152" class="reference"><a href="#cite_note-152"><span class="cite-bracket">&#91;</span>152<span class="cite-bracket">&#93;</span></a></sup> </p><p>The main part of soil organic matter is a complex assemblage of small organic molecules, collectively called humus or <a href="/wiki/Humic" class="mw-redirect" title="Humic">humic</a> substances. The use of these terms, which do not rely on a clear chemical classification, has been considered as obsolete.<sup id="cite_ref-153" class="reference"><a href="#cite_note-153"><span class="cite-bracket">&#91;</span>153<span class="cite-bracket">&#93;</span></a></sup> Other studies showed that the classical notion of molecule is not convenient for humus, which escaped most attempts done over two centuries to resolve it in unit components, but still is chemically distinct from polysaccharides, lignins and proteins.<sup id="cite_ref-Piccolo2002_154-0" class="reference"><a href="#cite_note-Piccolo2002-154"><span class="cite-bracket">&#91;</span>154<span class="cite-bracket">&#93;</span></a></sup> </p><p>Most living things in soils, including plants, animals, bacteria, and fungi, are dependent on organic matter for nutrients and/or energy. Soils have organic compounds in varying degrees of decomposition, the rate of which is dependent on the temperature, soil moisture, and aeration. Bacteria and fungi feed on the raw organic matter, which are fed upon by <a href="/wiki/Protozoa" title="Protozoa">protozoa</a>, which in turn are fed upon by <a href="/wiki/Nematodes" class="mw-redirect" title="Nematodes">nematodes</a>, <a href="/wiki/Annelids" class="mw-redirect" title="Annelids">annelids</a> and <a href="/wiki/Arthropod" title="Arthropod">arthropods</a>, themselves able to consume and transform raw or humified organic matter. This has been called the <a href="/wiki/Soil_food_web" title="Soil food web">soil food web</a>, through which all organic matter is processed as in a <a href="/wiki/Digestive_system" class="mw-redirect" title="Digestive system">digestive system</a>.<sup id="cite_ref-155" class="reference"><a href="#cite_note-155"><span class="cite-bracket">&#91;</span>155<span class="cite-bracket">&#93;</span></a></sup> Organic matter holds soils open, allowing the infiltration of air and water, and may hold as much as twice its weight in water. Many soils, including desert and rocky-gravel soils, have little or no organic matter. Soils that are all organic matter, such as <a href="/wiki/Peat" title="Peat">peat</a> (<a href="/wiki/Histosols" class="mw-redirect" title="Histosols">histosols</a>), are infertile.<sup id="cite_ref-Foth1984_156-0" class="reference"><a href="#cite_note-Foth1984-156"><span class="cite-bracket">&#91;</span>156<span class="cite-bracket">&#93;</span></a></sup> In its earliest stage of decomposition, the original organic material is often called raw organic matter. The final stage of decomposition is called humus. </p><p>In <a href="/wiki/Grassland" title="Grassland">grassland</a>, much of the organic matter added to the soil is from the deep, fibrous, grass root systems. By contrast, tree leaves falling on the forest floor are the principal source of soil organic matter in the forest. Another difference is the frequent occurrence in the grasslands of fires that destroy large amounts of aboveground material but stimulate even greater contributions from roots. Also, the much greater acidity under any forests inhibits the action of certain soil organisms that otherwise would mix much of the surface litter into the mineral soil. As a result, the soils under grasslands generally develop a thicker <a href="/wiki/A_horizon" class="mw-redirect" title="A horizon">A horizon</a> with a deeper distribution of organic matter than in comparable soils under forests, which characteristically store most of their organic matter in the forest floor (<a href="/wiki/O_horizon" class="mw-redirect" title="O horizon">O horizon</a>) and thin A horizon.<sup id="cite_ref-Ponge2003_157-0" class="reference"><a href="#cite_note-Ponge2003-157"><span class="cite-bracket">&#91;</span>157<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Humus">Humus</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=19" title="Edit section: Humus"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Humus refers to organic matter that has been decomposed by soil microflora and fauna to the point where it is resistant to further breakdown. Humus usually constitutes only five percent of the soil or less by volume, but it is an essential source of nutrients and adds important textural qualities crucial to <a href="/wiki/Soil_health" title="Soil health">soil health</a> and plant growth.<sup id="cite_ref-158" class="reference"><a href="#cite_note-158"><span class="cite-bracket">&#91;</span>158<span class="cite-bracket">&#93;</span></a></sup> Humus also feeds arthropods, <a href="/wiki/Termite" title="Termite">termites</a> and <a href="/wiki/Earthworm" title="Earthworm">earthworms</a> which further improve the soil.<sup id="cite_ref-159" class="reference"><a href="#cite_note-159"><span class="cite-bracket">&#91;</span>159<span class="cite-bracket">&#93;</span></a></sup> The end product, humus, is suspended in <a href="/wiki/Colloidal" class="mw-redirect" title="Colloidal">colloidal</a> form in the soil solution and forms a <a href="/wiki/Weak_acid" class="mw-redirect" title="Weak acid">weak acid</a> that can attack silicate minerals by <a href="/wiki/Chelation" title="Chelation">chelating</a> their iron and aluminum atoms.<sup id="cite_ref-160" class="reference"><a href="#cite_note-160"><span class="cite-bracket">&#91;</span>160<span class="cite-bracket">&#93;</span></a></sup> Humus has a high cation and anion exchange capacity that on a dry weight basis is many times greater than that of clay colloids. It also acts as a buffer, like clay, against changes in pH and soil moisture.<sup id="cite_ref-Piccolo1996_161-0" class="reference"><a href="#cite_note-Piccolo1996-161"><span class="cite-bracket">&#91;</span>161<span class="cite-bracket">&#93;</span></a></sup> </p><p><a href="/wiki/Humic_acid" class="mw-redirect" title="Humic acid">Humic acids</a> and <a href="/wiki/Fulvic_acid" class="mw-redirect" title="Fulvic acid">fulvic acids</a>, which begin as raw organic matter, are important constituents of humus. After the death of plants, animals, and microbes, microbes begin to feed on the residues through their production of extra-cellular soil enzymes, resulting finally in the formation of humus.<sup id="cite_ref-162" class="reference"><a href="#cite_note-162"><span class="cite-bracket">&#91;</span>162<span class="cite-bracket">&#93;</span></a></sup> As the residues break down, only molecules made of <a href="/wiki/Aliphatic_compound" title="Aliphatic compound">aliphatic</a> and <a href="/wiki/Aromatic_hydrocarbon" class="mw-redirect" title="Aromatic hydrocarbon">aromatic</a> hydrocarbons, assembled and stabilized by oxygen and hydrogen bonds, remain in the form of complex molecular assemblages collectively called humus.<sup id="cite_ref-Piccolo2002_154-1" class="reference"><a href="#cite_note-Piccolo2002-154"><span class="cite-bracket">&#91;</span>154<span class="cite-bracket">&#93;</span></a></sup> Humus is never pure in the soil, because it reacts with metals and clays to form complexes which further contribute to its stability and to soil structure.<sup id="cite_ref-Piccolo1996_161-1" class="reference"><a href="#cite_note-Piccolo1996-161"><span class="cite-bracket">&#91;</span>161<span class="cite-bracket">&#93;</span></a></sup> Although the structure of humus has in itself few nutrients (with the exception of constitutive metals such as calcium, iron and aluminum) it is able to attract and link, by weak bonds, cation and anion nutrients that can further be released into the soil solution in response to selective root uptake and changes in soil pH, a process of paramount importance for the maintenance of fertility in tropical soils.<sup id="cite_ref-163" class="reference"><a href="#cite_note-163"><span class="cite-bracket">&#91;</span>163<span class="cite-bracket">&#93;</span></a></sup> </p><p><a href="/wiki/Lignin" title="Lignin">Lignin</a> is resistant to breakdown and accumulates within the soil. It also reacts with <a href="/wiki/Proteins" class="mw-redirect" title="Proteins">proteins</a>,<sup id="cite_ref-164" class="reference"><a href="#cite_note-164"><span class="cite-bracket">&#91;</span>164<span class="cite-bracket">&#93;</span></a></sup> which further increases its resistance to decomposition, including enzymatic decomposition by microbes.<sup id="cite_ref-165" class="reference"><a href="#cite_note-165"><span class="cite-bracket">&#91;</span>165<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Fat" title="Fat">Fats</a> and <a href="/wiki/Wax" title="Wax">waxes</a> from plant matter have still more resistance to decomposition and persist in soils for thousand years, hence their use as tracers of past vegetation in buried soil layers.<sup id="cite_ref-166" class="reference"><a href="#cite_note-166"><span class="cite-bracket">&#91;</span>166<span class="cite-bracket">&#93;</span></a></sup> Clay soils often have higher organic contents that persist longer than soils without clay as the organic molecules adhere to and are stabilised by the clay.<sup id="cite_ref-167" class="reference"><a href="#cite_note-167"><span class="cite-bracket">&#91;</span>167<span class="cite-bracket">&#93;</span></a></sup> Proteins normally decompose readily, to the exception of <a href="/wiki/Scleroproteins" class="mw-redirect" title="Scleroproteins">scleroproteins</a>, but when bound to clay particles they become more resistant to decomposition.<sup id="cite_ref-168" class="reference"><a href="#cite_note-168"><span class="cite-bracket">&#91;</span>168<span class="cite-bracket">&#93;</span></a></sup> As for other proteins clay particles absorb the enzymes exuded by microbes, decreasing <a href="/wiki/Enzyme_activity" class="mw-redirect" title="Enzyme activity">enzyme activity</a> while protecting <a href="/wiki/Extracellular_enzymes" class="mw-redirect" title="Extracellular enzymes">extracellular enzymes</a> from degradation.<sup id="cite_ref-169" class="reference"><a href="#cite_note-169"><span class="cite-bracket">&#91;</span>169<span class="cite-bracket">&#93;</span></a></sup> The addition of organic matter to clay soils can render that organic matter and any added nutrients inaccessible to plants and microbes for many years.<sup id="cite_ref-170" class="reference"><a href="#cite_note-170"><span class="cite-bracket">&#91;</span>170<span class="cite-bracket">&#93;</span></a></sup> A study showed increased soil fertility following the addition of mature compost to a clay soil.<sup id="cite_ref-171" class="reference"><a href="#cite_note-171"><span class="cite-bracket">&#91;</span>171<span class="cite-bracket">&#93;</span></a></sup> High soil <a href="/wiki/Tannin" title="Tannin">tannin</a> content can cause nitrogen to be sequestered as resistant tannin-protein complexes.<sup id="cite_ref-172" class="reference"><a href="#cite_note-172"><span class="cite-bracket">&#91;</span>172<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Fierer2001_173-0" class="reference"><a href="#cite_note-Fierer2001-173"><span class="cite-bracket">&#91;</span>173<span class="cite-bracket">&#93;</span></a></sup> </p><p>Humus formation is a process dependent on the amount of plant material added each year and the type of base soil. Both are affected by climate and the type of organisms present.<sup id="cite_ref-Ponge2003_157-1" class="reference"><a href="#cite_note-Ponge2003-157"><span class="cite-bracket">&#91;</span>157<span class="cite-bracket">&#93;</span></a></sup> Soils with humus can vary in nitrogen content but typically have 3 to 6&#160;percent nitrogen. Raw organic matter, as a reserve of nitrogen and phosphorus, is a vital component affecting <a href="/wiki/Fertile_soil" class="mw-redirect" title="Fertile soil">soil fertility</a>.<sup id="cite_ref-Foth1984_156-1" class="reference"><a href="#cite_note-Foth1984-156"><span class="cite-bracket">&#91;</span>156<span class="cite-bracket">&#93;</span></a></sup> Humus also absorbs water, and expands and shrinks between dry and wet states to a higher extent than clay, increasing soil porosity.<sup id="cite_ref-174" class="reference"><a href="#cite_note-174"><span class="cite-bracket">&#91;</span>174<span class="cite-bracket">&#93;</span></a></sup> Humus is less stable than the soil's mineral constituents, as it is reduced by microbial decomposition, and over time its concentration diminishes without the addition of new organic matter. However, humus in its most stable forms may persist over centuries if not millennia.<sup id="cite_ref-175" class="reference"><a href="#cite_note-175"><span class="cite-bracket">&#91;</span>175<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Charcoal" title="Charcoal">Charcoal</a> is a source of highly stable humus, called <a href="/wiki/Black_carbon" title="Black carbon">black carbon</a>,<sup id="cite_ref-176" class="reference"><a href="#cite_note-176"><span class="cite-bracket">&#91;</span>176<span class="cite-bracket">&#93;</span></a></sup> which had been used traditionally to improve the fertility of nutrient-poor tropical soils. This very ancient practice, as ascertained in the genesis of <a href="/wiki/Amazonian_dark_earths" class="mw-redirect" title="Amazonian dark earths">Amazonian dark earths</a>, has been renewed and became popular under the name of <a href="/wiki/Biochar" title="Biochar">biochar</a>. It has been suggested that biochar could be used to sequester more carbon in the fight against the greenhouse effect.<sup id="cite_ref-177" class="reference"><a href="#cite_note-177"><span class="cite-bracket">&#91;</span>177<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Climatological_influence">Climatological influence</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=20" title="Edit section: Climatological influence"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>The production, accumulation and degradation of organic matter are greatly dependent on climate. For example, when a <a href="/wiki/Thaw_(weather)" title="Thaw (weather)">thawing</a> event occurs, the flux of <a href="/wiki/Soil_gas" title="Soil gas">soil gases</a> with atmospheric gases is significantly influenced.<sup id="cite_ref-178" class="reference"><a href="#cite_note-178"><span class="cite-bracket">&#91;</span>178<span class="cite-bracket">&#93;</span></a></sup> Temperature, soil moisture and <a href="/wiki/Topography" title="Topography">topography</a> are the major factors affecting the accumulation of organic matter in soils. Organic matter tends to accumulate under wet or cold conditions where <a href="/wiki/Decomposer" title="Decomposer">decomposer</a> activity is impeded by low temperature<sup id="cite_ref-Wagai2008_179-0" class="reference"><a href="#cite_note-Wagai2008-179"><span class="cite-bracket">&#91;</span>179<span class="cite-bracket">&#93;</span></a></sup> or excess moisture which results in anaerobic conditions.<sup id="cite_ref-Minayeva2008_180-0" class="reference"><a href="#cite_note-Minayeva2008-180"><span class="cite-bracket">&#91;</span>180<span class="cite-bracket">&#93;</span></a></sup> Conversely, excessive rain and high temperatures of tropical climates enables rapid decomposition of organic matter and leaching of plant nutrients. Forest ecosystems on these soils rely on efficient recycling of nutrients and plant matter by the living plant and microbial biomass to maintain their productivity, a process which is disturbed by human activities.<sup id="cite_ref-181" class="reference"><a href="#cite_note-181"><span class="cite-bracket">&#91;</span>181<span class="cite-bracket">&#93;</span></a></sup> Excessive slope, in particular in the presence of cultivation for the sake of agriculture, may encourage the erosion of the top layer of soil which holds most of the raw organic material that would otherwise eventually become humus.<sup id="cite_ref-182" class="reference"><a href="#cite_note-182"><span class="cite-bracket">&#91;</span>182<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Plant_residue">Plant residue</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=21" title="Edit section: Plant residue"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <div class="PieChartTemplate thumb tright"><div class="thumbinner" style="width:202px"> <div class="mw-no-invert" style="background-color:white;margin:auto;position:relative;width:200px;height:200px;overflow:hidden;border-radius:100px;border:1px solid black;transform:scaleX(-1)rotate(-90deg)"> <div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;left:100px; top:100px; border-width:100px 0 0 791.58150883059px; border-left-color:#B15928"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 200px 100px 0;border-color:#B15928"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 100px 200px 0;border-color:#B15928"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;left:100px; top:100px; border-width:100px 0 0 389.47428549299px; border-left-color:#6A3D9A"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 200px 100px 0;border-color:#6A3D9A"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 100px 200px 0;border-color:#6A3D9A"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;left:100px; top:100px; border-width:100px 0 0 157.57478599687px; border-left-color:#FF7F00"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 200px 100px 0;border-color:#FF7F00"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 100px 200px 0;border-color:#FF7F00"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;left:100px; top:100px; border-width:100px 0 0 54.975465219277px; border-left-color:#E31A1C"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 200px 100px 0;border-color:#E31A1C"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 100px 200px 0;border-color:#E31A1C"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;right:100px; top:100px; border-width:80.901699437495px 58.778525229247px 0 0; border-top-color:#33A02C"></div> <div style="position:absolute;line-height:0;border-style:solid;left:0;top:0;border-width:0 200px 100px 0;border-color:#33A02C"></div><div style="border:solid transparent;background-color:initial;position:absolute;width:100px;line-height:0;right:100px; top:0; border-width:0 307.76835371753px 100px 0; border-right-color:#1F78B4"></div> <div style="position:absolute;line-height:0;border-style:solid;right:0;top:0;border-width:0 100px 100px 0;border-color:#1F78B4"></div> </div> <div class="thumbcaption"> <p>Typical types and percentages of plant residue components </p> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:#1F78B4; color:;">&#160;</span>&#160;Cellulose (45%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:#33A02C; color:;">&#160;</span>&#160;Lignin (20%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:#E31A1C; color:;">&#160;</span>&#160;Hemicellulose (18%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:#FF7F00; color:;">&#160;</span>&#160;Protein (8%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:#6A3D9A; color:;">&#160;</span>&#160;Sugars and starches (5%)</div><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r981673959"><div class="legend"><span class="legend-color mw-no-invert" style="background-color:#B15928; color:;">&#160;</span>&#160;Fats and waxes (2%)</div> </div> </div></div> <p><a href="/wiki/Cellulose" title="Cellulose">Cellulose</a> and <a href="/wiki/Hemicellulose" title="Hemicellulose">hemicellulose</a> undergo fast decomposition by fungi and bacteria, with a half-life of 12–18&#160;days in a temperate climate.<sup id="cite_ref-Paul1997_183-0" class="reference"><a href="#cite_note-Paul1997-183"><span class="cite-bracket">&#91;</span>183<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Wood-decay_fungus" title="Wood-decay fungus">Brown rot fungi</a> can decompose the cellulose and hemicellulose, leaving the lignin and <a href="/wiki/Phenols" title="Phenols">phenolic compounds</a> behind. <a href="/wiki/Starch" title="Starch">Starch</a>, which is an <a href="/wiki/Energy_storage" title="Energy storage">energy storage</a> system for plants, undergoes fast decomposition by bacteria and fungi. Lignin consists of <a href="/wiki/Polymers" class="mw-redirect" title="Polymers">polymers</a> composed of 500 to 600 units with a highly branched, amorphous structure, linked to cellulose, hemicellulose and <a href="/wiki/Pectin" title="Pectin">pectin</a> in <a href="/wiki/Plant_cell_walls" class="mw-redirect" title="Plant cell walls">plant cell walls</a>. Lignin undergoes very slow decomposition, mainly by <a href="/wiki/White_rot" class="mw-redirect" title="White rot">white rot</a> fungi and <a href="/wiki/Actinomycetes" class="mw-redirect" title="Actinomycetes">actinomycetes</a>; its half-life under temperate conditions is about six months.<sup id="cite_ref-Paul1997_183-1" class="reference"><a href="#cite_note-Paul1997-183"><span class="cite-bracket">&#91;</span>183<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Horizons">Horizons</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=22" title="Edit section: Horizons"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Soil_horizon" title="Soil horizon">Soil horizon</a></div> <p>A horizontal layer of the soil, whose physical features, composition and age are distinct from those above and beneath, is referred to as a soil horizon. The naming of a horizon is based on the type of material of which it is composed. Those materials reflect the duration of specific processes of soil formation. They are labelled using a shorthand notation of letters and numbers which describe the horizon in terms of its colour, size, texture, structure, consistency, root quantity, pH, voids, boundary characteristics and presence of nodules or concretions.<sup id="cite_ref-184" class="reference"><a href="#cite_note-184"><span class="cite-bracket">&#91;</span>184<span class="cite-bracket">&#93;</span></a></sup> No soil profile has all the major horizons. Some, called <a href="/wiki/Entisols" class="mw-redirect" title="Entisols">entisols</a>, may have only one horizon or are currently considered as having no horizon, in particular incipient soils from unreclaimed <a href="/wiki/Mining_waste" class="mw-redirect" title="Mining waste">mining waste</a> deposits,<sup id="cite_ref-185" class="reference"><a href="#cite_note-185"><span class="cite-bracket">&#91;</span>185<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Moraines" class="mw-redirect" title="Moraines">moraines</a>,<sup id="cite_ref-186" class="reference"><a href="#cite_note-186"><span class="cite-bracket">&#91;</span>186<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Volcanic_cones" class="mw-redirect" title="Volcanic cones">volcanic cones</a><sup id="cite_ref-187" class="reference"><a href="#cite_note-187"><span class="cite-bracket">&#91;</span>187<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Sand_dunes" class="mw-redirect" title="Sand dunes">sand dunes</a> or <a href="/wiki/Alluvial_terrace" class="mw-redirect" title="Alluvial terrace">alluvial terraces</a>.<sup id="cite_ref-188" class="reference"><a href="#cite_note-188"><span class="cite-bracket">&#91;</span>188<span class="cite-bracket">&#93;</span></a></sup> Upper soil horizons may be lacking in truncated soils following wind or water ablation, with concomitant downslope burying of soil horizons, a natural process aggravated by agricultural practices such as tillage.<sup id="cite_ref-189" class="reference"><a href="#cite_note-189"><span class="cite-bracket">&#91;</span>189<span class="cite-bracket">&#93;</span></a></sup> The growth of trees is another source of disturbance, creating a micro-scale heterogeneity which is still visible in soil horizons once trees have died.<sup id="cite_ref-190" class="reference"><a href="#cite_note-190"><span class="cite-bracket">&#91;</span>190<span class="cite-bracket">&#93;</span></a></sup> By passing from a horizon to another, from the top to the bottom of the soil profile, one goes back in time, with past events registered in soil horizons like in <a href="/wiki/Sediment" title="Sediment">sediment</a> layers. Sampling <a href="/wiki/Pollen" title="Pollen">pollen</a>, <a href="/wiki/Testate_amoebae" title="Testate amoebae">testate amoebae</a> and plant remains in soil horizons may help to reveal environmental changes (e.g. climate change, <a href="/wiki/Land_use" title="Land use">land use</a> change) which occurred in the course of soil formation.<sup id="cite_ref-191" class="reference"><a href="#cite_note-191"><span class="cite-bracket">&#91;</span>191<span class="cite-bracket">&#93;</span></a></sup> Soil horizons can be dated by several methods such as <a href="/wiki/Radiocarbon" class="mw-redirect" title="Radiocarbon">radiocarbon</a>, using pieces of charcoal provided they are of enough size to escape <a href="/wiki/Pedoturbation" class="mw-redirect" title="Pedoturbation">pedoturbation</a> by earthworm activity and other mechanical disturbances.<sup id="cite_ref-192" class="reference"><a href="#cite_note-192"><span class="cite-bracket">&#91;</span>192<span class="cite-bracket">&#93;</span></a></sup> Fossil soil horizons from <a href="/wiki/Paleosols" class="mw-redirect" title="Paleosols">paleosols</a> can be found within <a href="/wiki/Sedimentary_rock" title="Sedimentary rock">sedimentary rock</a> sequences, allowing the study of past environments.<sup id="cite_ref-193" class="reference"><a href="#cite_note-193"><span class="cite-bracket">&#91;</span>193<span class="cite-bracket">&#93;</span></a></sup> </p><p>The exposure of parent material to favourable conditions produces mineral soils that are marginally suitable for plant growth, as is the case in eroded soils.<sup id="cite_ref-194" class="reference"><a href="#cite_note-194"><span class="cite-bracket">&#91;</span>194<span class="cite-bracket">&#93;</span></a></sup> The growth of vegetation results in the production of organic residues which fall on the ground as litter for plant aerial parts (<a href="/wiki/Leaf_litter" class="mw-redirect" title="Leaf litter">leaf litter</a>) or are directly produced belowground for subterranean plant organs (root litter), and then release <a href="/wiki/Dissolved_organic_matter" class="mw-redirect" title="Dissolved organic matter">dissolved organic matter</a>.<sup id="cite_ref-195" class="reference"><a href="#cite_note-195"><span class="cite-bracket">&#91;</span>195<span class="cite-bracket">&#93;</span></a></sup> The remaining surficial organic layer, called the <a href="/wiki/Forest_floor" title="Forest floor">O horizon</a>, produces a more active soil due to the effect of the organisms that live within it. Organisms colonise and break down organic materials, making available nutrients upon which other plants and animals can live.<sup id="cite_ref-196" class="reference"><a href="#cite_note-196"><span class="cite-bracket">&#91;</span>196<span class="cite-bracket">&#93;</span></a></sup> After sufficient time, humus moves downward and is deposited in a distinctive organic-mineral surface layer called the A horizon, in which organic matter is mixed with mineral matter through the activity of burrowing animals, a process called pedoturbation. This natural process does not go to completion in the presence of conditions detrimental to soil life such as strong acidity, cold climate or pollution, stemming in the accumulation of undecomposed organic matter within a single organic horizon overlying the mineral soil<sup id="cite_ref-197" class="reference"><a href="#cite_note-197"><span class="cite-bracket">&#91;</span>197<span class="cite-bracket">&#93;</span></a></sup> and in the juxtaposition of humified organic matter and mineral particles, without intimate mixing, in the underlying mineral horizons.<sup id="cite_ref-198" class="reference"><a href="#cite_note-198"><span class="cite-bracket">&#91;</span>198<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Classification">Classification</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=23" title="Edit section: Classification"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Soil_classification" title="Soil classification">Soil classification</a></div> <p>One of the first soil classification systems was developed by Russian scientist <a href="/wiki/Vasily_Dokuchaev" title="Vasily Dokuchaev">Vasily Dokuchaev</a> around 1880.<sup id="cite_ref-199" class="reference"><a href="#cite_note-199"><span class="cite-bracket">&#91;</span>199<span class="cite-bracket">&#93;</span></a></sup> It was modified a number of times by American and European researchers and was developed into the system commonly used until the 1960s. It was based on the idea that soils have a particular morphology based on the materials and factors that form them. In the 1960s, a different classification system began to emerge which focused on <a href="/wiki/Soil_morphology" title="Soil morphology">soil morphology</a> instead of parental materials and soil-forming factors. Since then, it has undergone further modifications. The <a href="/wiki/World_Reference_Base_for_Soil_Resources" title="World Reference Base for Soil Resources">World Reference Base for Soil Resources</a><sup id="cite_ref-WRB_200-0" class="reference"><a href="#cite_note-WRB-200"><span class="cite-bracket">&#91;</span>200<span class="cite-bracket">&#93;</span></a></sup> aims to establish an international reference base for soil classification. </p> <div class="mw-heading mw-heading2"><h2 id="Uses">Uses</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=24" title="Edit section: Uses"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Soil is used in agriculture, where it serves as the anchor and primary nutrient base for plants. The types of soil and available moisture determine the species of plants that can be cultivated. <a href="/wiki/Agricultural_soil_science" title="Agricultural soil science">Agricultural soil science</a> was the primeval domain of soil knowledge, long time before the advent of <a href="/wiki/Pedology" title="Pedology">pedology</a> in the 19th century. However, as demonstrated by <a href="/wiki/Aeroponics" title="Aeroponics">aeroponics</a>, <a href="/wiki/Aquaponics" title="Aquaponics">aquaponics</a> and <a href="/wiki/Hydroponics" title="Hydroponics">hydroponics</a>, soil material is not an absolute essential for agriculture, and soilless cropping systems have been claimed as the future of agriculture for an endless growing mankind.<sup id="cite_ref-201" class="reference"><a href="#cite_note-201"><span class="cite-bracket">&#91;</span>201<span class="cite-bracket">&#93;</span></a></sup> </p><p>Soil material is also a critical component in mining, construction and landscape development industries.<sup id="cite_ref-202" class="reference"><a href="#cite_note-202"><span class="cite-bracket">&#91;</span>202<span class="cite-bracket">&#93;</span></a></sup> Soil serves as a foundation for most construction projects. The movement of massive volumes of soil can be involved in <a href="/wiki/Surface_mining" title="Surface mining">surface mining</a>, <a href="/wiki/Road_building" class="mw-redirect" title="Road building">road building</a> and <a href="/wiki/Dam" title="Dam">dam</a> construction. <a href="/wiki/Earth_sheltering" class="mw-redirect" title="Earth sheltering">Earth sheltering</a> is the architectural practice of using soil for external <a href="/wiki/Thermal_mass" title="Thermal mass">thermal mass</a> against building walls. Many <a href="/wiki/Building_material" title="Building material">building materials</a> are soil based. Loss of soil through urbanization is growing at a high rate in many areas and can be critical for the maintenance of <a href="/wiki/Subsistence_agriculture" title="Subsistence agriculture">subsistence agriculture</a>.<sup id="cite_ref-203" class="reference"><a href="#cite_note-203"><span class="cite-bracket">&#91;</span>203<span class="cite-bracket">&#93;</span></a></sup> </p><p>Soil resources are critical to the environment, as well as to food and fibre production, producing 98.8% of food consumed by humans.<sup id="cite_ref-204" class="reference"><a href="#cite_note-204"><span class="cite-bracket">&#91;</span>204<span class="cite-bracket">&#93;</span></a></sup> Soil provides minerals and water to plants according to several processes involved in plant nutrition. Soil absorbs rainwater and releases it later, thus preventing floods and drought, flood regulation being one of the major ecosystem services provided by soil.<sup id="cite_ref-205" class="reference"><a href="#cite_note-205"><span class="cite-bracket">&#91;</span>205<span class="cite-bracket">&#93;</span></a></sup> Soil cleans water as it percolates through it.<sup id="cite_ref-206" class="reference"><a href="#cite_note-206"><span class="cite-bracket">&#91;</span>206<span class="cite-bracket">&#93;</span></a></sup> Soil is the habitat for many organisms: the major part of known and unknown <a href="/wiki/Biodiversity" title="Biodiversity">biodiversity</a> is in the soil, in the form of earthworms, <a href="/wiki/Woodlice" class="mw-redirect" title="Woodlice">woodlice</a>, <a href="/wiki/Millipede" title="Millipede">millipedes</a>, <a href="/wiki/Centipede" title="Centipede">centipedes</a>, <a href="/wiki/Snail" title="Snail">snails</a>, <a href="/wiki/Slug" title="Slug">slugs</a>, <a href="/wiki/Mite" title="Mite">mites</a>, <a href="/wiki/Springtail" title="Springtail">springtails</a>, <a href="/wiki/Enchytraeidae" title="Enchytraeidae">enchytraeids</a>, <a href="/wiki/Nematode" title="Nematode">nematodes</a>, <a href="/wiki/Protist" title="Protist">protists</a>), bacteria, <a href="/wiki/Archaea" title="Archaea">archaea</a>, fungi and <a href="/wiki/Algae" title="Algae">algae</a>; and most organisms living above ground have part of them (<a href="/wiki/Plants" class="mw-redirect" title="Plants">plants</a>) or spend part of their <a href="/wiki/Biological_life_cycle" title="Biological life cycle">life cycle</a> (<a href="/wiki/Insects" class="mw-redirect" title="Insects">insects</a>) below-ground.<sup id="cite_ref-207" class="reference"><a href="#cite_note-207"><span class="cite-bracket">&#91;</span>207<span class="cite-bracket">&#93;</span></a></sup> Above-ground and below-ground biodiversities are tightly interconnected,<sup id="cite_ref-Ponge2003_157-2" class="reference"><a href="#cite_note-Ponge2003-157"><span class="cite-bracket">&#91;</span>157<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-De_Deyn2005_208-0" class="reference"><a href="#cite_note-De_Deyn2005-208"><span class="cite-bracket">&#91;</span>208<span class="cite-bracket">&#93;</span></a></sup> making <a href="/wiki/Soil_protection" class="mw-redirect" title="Soil protection">soil protection</a> of paramount importance for any <a href="/wiki/Environmental_restoration" class="mw-redirect" title="Environmental restoration">restoration</a> or <a href="/wiki/Nature_conservation" title="Nature conservation">conservation</a> plan. </p><p>The biological component of soil is an extremely important carbon sink since about 57% of the biotic content is carbon. Even in deserts, cyanobacteria, <a href="/wiki/Lichen" title="Lichen">lichens</a> and <a href="/wiki/Moss" title="Moss">mosses</a> form <a href="/wiki/Biological_soil_crust" title="Biological soil crust">biological soil crusts</a> which capture and sequester a significant amount of carbon by <a href="/wiki/Photosynthesis" title="Photosynthesis">photosynthesis</a>. Poor farming and grazing methods have degraded soils and released much of this sequestered carbon to the atmosphere. Restoring the world's soils could offset the effect of increases in <a href="/wiki/Greenhouse_gas_emissions" title="Greenhouse gas emissions">greenhouse gas emissions</a> and slow global warming, while improving crop yields and reducing water needs.<sup id="cite_ref-209" class="reference"><a href="#cite_note-209"><span class="cite-bracket">&#91;</span>209<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-210" class="reference"><a href="#cite_note-210"><span class="cite-bracket">&#91;</span>210<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-211" class="reference"><a href="#cite_note-211"><span class="cite-bracket">&#91;</span>211<span class="cite-bracket">&#93;</span></a></sup> </p><p><a href="/wiki/Waste_management" title="Waste management">Waste management</a> often has a soil component. <a href="/wiki/Septic_drain_field" title="Septic drain field">Septic drain fields</a> treat <a href="/wiki/Septic_tank" title="Septic tank">septic tank</a> effluent using <a href="/wiki/Aerobic_organism" title="Aerobic organism">aerobic</a> soil processes. Land application of <a href="/wiki/Waste_water" class="mw-redirect" title="Waste water">waste water</a> relies on <a href="/wiki/Soil_biology" title="Soil biology">soil biology</a> to aerobically treat <a href="/wiki/Biochemical_oxygen_demand" title="Biochemical oxygen demand">BOD</a>. Alternatively, <a href="/wiki/Landfill" title="Landfill">landfills</a> use soil for <a href="/wiki/Daily_cover" title="Daily cover">daily cover</a>, isolating waste deposits from the atmosphere and preventing unpleasant smells. <a href="/wiki/Composting" class="mw-redirect" title="Composting">Composting</a> is now widely used to treat aerobically solid domestic waste and dried effluents of <a href="/wiki/Settling_basin" title="Settling basin">settling basins</a>. Although compost is not soil, biological processes taking place during composting are similar to those occurring during decomposition and humification of soil organic matter.<sup id="cite_ref-212" class="reference"><a href="#cite_note-212"><span class="cite-bracket">&#91;</span>212<span class="cite-bracket">&#93;</span></a></sup> </p><p>Organic soils, especially peat, serve as a significant fuel and <a href="/wiki/Horticulture" title="Horticulture">horticultural</a> resource. Peat soils are also commonly used for the sake of agriculture in Nordic countries, because peatland sites, when drained, provide fertile soils for food production.<sup id="cite_ref-213" class="reference"><a href="#cite_note-213"><span class="cite-bracket">&#91;</span>213<span class="cite-bracket">&#93;</span></a></sup> However, wide areas of peat production, such as rain-fed <a href="/wiki/Sphagnum" title="Sphagnum">sphagnum</a> <a href="/wiki/Bog" title="Bog">bogs</a>, also called <a href="/wiki/Blanket_bog" title="Blanket bog">blanket bogs</a> or <a href="/wiki/Raised_bog" title="Raised bog">raised bogs</a>, are now protected because of their patrimonial interest. As an example, <a href="/wiki/Flow_Country" title="Flow Country">Flow Country</a>, covering 4,000 square kilometres of rolling expanse of blanket bogs in Scotland, is now candidate for being included in the <a href="/wiki/World_Heritage_List" class="mw-redirect" title="World Heritage List">World Heritage List</a>. Under present-day global warming peat soils are thought to be involved in a self-reinforcing (positive feedback) process of increased emission of greenhouse gases (methane and carbon dioxide) and increased temperature,<sup id="cite_ref-214" class="reference"><a href="#cite_note-214"><span class="cite-bracket">&#91;</span>214<span class="cite-bracket">&#93;</span></a></sup> a contention which is still under debate when replaced at field scale and including stimulated plant growth.<sup id="cite_ref-215" class="reference"><a href="#cite_note-215"><span class="cite-bracket">&#91;</span>215<span class="cite-bracket">&#93;</span></a></sup> </p><p><a href="/wiki/Geophagy" class="mw-redirect" title="Geophagy">Geophagy</a> is the practice of eating soil-like substances. Both animals and humans occasionally consume soil for medicinal, recreational, or religious purposes.<sup id="cite_ref-216" class="reference"><a href="#cite_note-216"><span class="cite-bracket">&#91;</span>216<span class="cite-bracket">&#93;</span></a></sup> It has been shown that some <a href="/wiki/Monkeys" class="mw-redirect" title="Monkeys">monkeys</a> consume soil, together with their preferred food (tree <a href="/wiki/Foliage" class="mw-redirect" title="Foliage">foliage</a> and <a href="/wiki/Fruits" class="mw-redirect" title="Fruits">fruits</a>), in order to alleviate tannin toxicity.<sup id="cite_ref-Setz1999_217-0" class="reference"><a href="#cite_note-Setz1999-217"><span class="cite-bracket">&#91;</span>217<span class="cite-bracket">&#93;</span></a></sup> </p><p>Soils filter and purify water and affect its chemistry. Rain water and pooled water from ponds, lakes and rivers percolate through the soil horizons and the upper <a href="/wiki/Stratum" title="Stratum">rock strata</a>, thus becoming <a href="/wiki/Groundwater" title="Groundwater">groundwater</a>. <a href="/wiki/Pest_(organism)" title="Pest (organism)">Pests</a> (<a href="/wiki/Virus" title="Virus">viruses</a>) and <a href="/wiki/Pollutant" title="Pollutant">pollutants</a>, such as <a href="/wiki/Persistent_organic_pollutant" title="Persistent organic pollutant">persistent organic pollutants</a> (<a href="/wiki/Chlorinated" class="mw-redirect" title="Chlorinated">chlorinated</a> <a href="/wiki/Pesticide" title="Pesticide">pesticides</a>, <a href="/wiki/Polychlorinated_biphenyl" title="Polychlorinated biphenyl">polychlorinated biphenyls</a>), oils (<a href="/wiki/Hydrocarbon" title="Hydrocarbon">hydrocarbons</a>), heavy metals (<a href="/wiki/Lead" title="Lead">lead</a>, zinc, <a href="/wiki/Cadmium" title="Cadmium">cadmium</a>), and excess nutrients (nitrates, <a href="/wiki/Sulfate" title="Sulfate">sulfates</a>, phosphates) are filtered out by the soil.<sup id="cite_ref-Kohne2009_218-0" class="reference"><a href="#cite_note-Kohne2009-218"><span class="cite-bracket">&#91;</span>218<span class="cite-bracket">&#93;</span></a></sup> Soil organisms <a href="/wiki/Metabolise" class="mw-redirect" title="Metabolise">metabolise</a> them or immobilise them in their biomass and necromass,<sup id="cite_ref-Diplock2009_219-0" class="reference"><a href="#cite_note-Diplock2009-219"><span class="cite-bracket">&#91;</span>219<span class="cite-bracket">&#93;</span></a></sup> thereby incorporating them into stable humus.<sup id="cite_ref-Moeckel2008_220-0" class="reference"><a href="#cite_note-Moeckel2008-220"><span class="cite-bracket">&#91;</span>220<span class="cite-bracket">&#93;</span></a></sup> The physical integrity of soil is also a prerequisite for avoiding landslides in rugged landscapes.<sup id="cite_ref-Rezaei2009_221-0" class="reference"><a href="#cite_note-Rezaei2009-221"><span class="cite-bracket">&#91;</span>221<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Degradation">Degradation</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=25" title="Edit section: Degradation"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main articles: <a href="/wiki/Soil_retrogression_and_degradation" title="Soil retrogression and degradation">Soil retrogression and degradation</a> and <a href="/wiki/Soil_conservation" title="Soil conservation">Soil conservation</a></div> <p><a href="/wiki/Land_degradation" title="Land degradation">Land degradation</a> is a human-induced or natural process which impairs the capacity of <a href="/wiki/Land_(economics)" title="Land (economics)">land</a> to function.<sup id="cite_ref-222" class="reference"><a href="#cite_note-222"><span class="cite-bracket">&#91;</span>222<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Soil_degradation" class="mw-redirect" title="Soil degradation">Soil degradation</a> involves <a href="/wiki/Soil_acidification" title="Soil acidification">acidification</a>, <a href="/wiki/Soil_contamination" title="Soil contamination">contamination</a>, <a href="/wiki/Desertification" title="Desertification">desertification</a>, <a href="/wiki/Erosion" title="Erosion">erosion</a> or <a href="/wiki/Soil_salinity" title="Soil salinity">salination</a>.<sup id="cite_ref-223" class="reference"><a href="#cite_note-223"><span class="cite-bracket">&#91;</span>223<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Acidification">Acidification</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=26" title="Edit section: Acidification"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Soil acidification is beneficial in the case of <a href="/wiki/Alkaline_soil" class="mw-redirect" title="Alkaline soil">alkaline soils</a>, but it degrades land when it lowers <a href="/wiki/Crop_productivity" class="mw-redirect" title="Crop productivity">crop productivity</a>, soil biological activity and increases soil vulnerability to <a href="/wiki/Contamination" title="Contamination">contamination</a> and erosion. Soils are initially acid and remain such when their parent materials are low in basic <a href="/wiki/Cation" class="mw-redirect" title="Cation">cations</a> (calcium, magnesium, potassium and <a href="/wiki/Sodium" title="Sodium">sodium</a>). On parent materials richer in <a href="/wiki/Mineral_weathering" class="mw-redirect" title="Mineral weathering">weatherable minerals</a> acidification occurs when basic cations are <a href="/wiki/Leaching_(pedology)" title="Leaching (pedology)">leached</a> from the soil profile by rainfall or exported by the harvesting of forest or agricultural crops. Soil acidification is accelerated by the use of acid-forming <a href="/wiki/Nitrogenous_fertilizer" class="mw-redirect" title="Nitrogenous fertilizer">nitrogenous fertilizers</a> and by the effects of <a href="/wiki/Acid_precipitation" class="mw-redirect" title="Acid precipitation">acid precipitation</a>. <a href="/wiki/Deforestation" title="Deforestation">Deforestation</a> is another cause of soil acidification, mediated by increased leaching of soil nutrients in the absence of <a href="/wiki/Tree_canopies" class="mw-redirect" title="Tree canopies">tree canopies</a>.<sup id="cite_ref-224" class="reference"><a href="#cite_note-224"><span class="cite-bracket">&#91;</span>224<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Contamination">Contamination</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=27" title="Edit section: Contamination"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Soil <a href="/wiki/Contamination" title="Contamination">contamination</a> at low levels is often within a soil's capacity to treat and assimilate <a href="/wiki/Waste" title="Waste">waste</a> material. <a href="/wiki/Soil_biota" class="mw-redirect" title="Soil biota">Soil biota</a> can treat waste by transforming it, mainly through microbial <a href="/wiki/Enzyme" title="Enzyme">enzymatic</a> activity.<sup id="cite_ref-225" class="reference"><a href="#cite_note-225"><span class="cite-bracket">&#91;</span>225<span class="cite-bracket">&#93;</span></a></sup> Soil organic matter and soil minerals can adsorb the waste material and decrease its <a href="/wiki/Toxicity" title="Toxicity">toxicity</a>,<sup id="cite_ref-226" class="reference"><a href="#cite_note-226"><span class="cite-bracket">&#91;</span>226<span class="cite-bracket">&#93;</span></a></sup> although when in colloidal form they may transport the adsorbed contaminants to subsurface environments.<sup id="cite_ref-227" class="reference"><a href="#cite_note-227"><span class="cite-bracket">&#91;</span>227<span class="cite-bracket">&#93;</span></a></sup> Many waste treatment processes rely on this natural <a href="/wiki/Bioremediation" title="Bioremediation">bioremediation</a> capacity. Exceeding treatment capacity can damage soil biota and limit soil function. Derelict soils occur where industrial contamination or other development activity damages the soil to such a degree that the land cannot be used safely or productively. <a href="/wiki/Environmental_remediation" title="Environmental remediation">Remediation</a> of derelict soil uses principles of geology, physics, chemistry and biology to degrade, attenuate, isolate or remove soil contaminants to restore <a href="/wiki/Soil_functions" title="Soil functions">soil functions</a> and values. Techniques include <a href="/wiki/Leaching_(chemistry)" title="Leaching (chemistry)">leaching</a>, <a href="/wiki/Air_sparging" title="Air sparging">air sparging</a>, <a href="/wiki/Soil_conditioner" title="Soil conditioner">soil conditioners</a>, <a href="/wiki/Phytoremediation" title="Phytoremediation">phytoremediation</a>, bioremediation and <a href="/wiki/In_situ_bioremediation" title="In situ bioremediation">Monitored Natural Attenuation</a>. An example of diffuse pollution with contaminants is copper accumulation in <a href="/wiki/Vineyard" title="Vineyard">vineyards</a> and <a href="/wiki/Orchard" title="Orchard">orchards</a> to which fungicides are repeatedly applied, even in <a href="/wiki/Organic_farming" title="Organic farming">organic farming</a>.<sup id="cite_ref-228" class="reference"><a href="#cite_note-228"><span class="cite-bracket">&#91;</span>228<span class="cite-bracket">&#93;</span></a></sup> </p><p><a href="/wiki/Microfiber" title="Microfiber">Microfibres</a> from synthetic textiles are another type of plastic soil contamination, 100% of agricultural soil samples from southwestern China contained plastic particles, 92% of which were microfibres. Sources of microfibres likely included string or twine, as well as irrigation water in which clothes had been washed.<sup id="cite_ref-auto_229-0" class="reference"><a href="#cite_note-auto-229"><span class="cite-bracket">&#91;</span>229<span class="cite-bracket">&#93;</span></a></sup> </p><p>The application of biosolids from sewage sludge and compost can introduce <a href="/wiki/Microplastics" title="Microplastics">microplastics</a> to soils. This adds to the burden of microplastics from other sources (e.g. the atmosphere). Approximately half the sewage sludge in Europe and North America is applied to agricultural land. In Europe it has been estimated that for every million inhabitants 113 to 770 tonnes of microplastics are added to agricultural soils each year.<sup id="cite_ref-auto_229-1" class="reference"><a href="#cite_note-auto-229"><span class="cite-bracket">&#91;</span>229<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Desertification">Desertification</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=28" title="Edit section: Desertification"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Soil_erosion,_Southfield_-_geograph.org.uk_-_367917.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/9/95/Soil_erosion%2C_Southfield_-_geograph.org.uk_-_367917.jpg/220px-Soil_erosion%2C_Southfield_-_geograph.org.uk_-_367917.jpg" decoding="async" width="220" height="174" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/9/95/Soil_erosion%2C_Southfield_-_geograph.org.uk_-_367917.jpg/330px-Soil_erosion%2C_Southfield_-_geograph.org.uk_-_367917.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/9/95/Soil_erosion%2C_Southfield_-_geograph.org.uk_-_367917.jpg/440px-Soil_erosion%2C_Southfield_-_geograph.org.uk_-_367917.jpg 2x" data-file-width="640" data-file-height="506" /></a><figcaption>Desertification</figcaption></figure> <p><a href="/wiki/Desertification" title="Desertification">Desertification</a>, an environmental process of ecosystem degradation in arid and semi-arid regions, is often caused by badly adapted human activities such as <a href="/wiki/Overgrazing" title="Overgrazing">overgrazing</a> or excess harvesting of <a href="/wiki/Firewood" title="Firewood">firewood</a>. It is a common misconception that <a href="/wiki/Drought" title="Drought">drought</a> causes desertification.<sup id="cite_ref-230" class="reference"><a href="#cite_note-230"><span class="cite-bracket">&#91;</span>230<span class="cite-bracket">&#93;</span></a></sup> Droughts are common in arid and semiarid lands. Well-managed lands can recover from drought when the rains return. <a href="/wiki/Soil_management" title="Soil management">Soil management</a> tools include maintaining soil nutrient and organic matter levels, reduced tillage and increased cover.<sup id="cite_ref-231" class="reference"><a href="#cite_note-231"><span class="cite-bracket">&#91;</span>231<span class="cite-bracket">&#93;</span></a></sup> These practices help to control erosion and maintain productivity during periods when moisture is available. Continued land abuse during droughts, however, increases <a href="/wiki/Land_degradation" title="Land degradation">land degradation</a>. Increased population and livestock pressure on marginal lands accelerates desertification.<sup id="cite_ref-232" class="reference"><a href="#cite_note-232"><span class="cite-bracket">&#91;</span>232<span class="cite-bracket">&#93;</span></a></sup> It is now questioned whether present-day climate warming will favour or disfavour desertification, with contradictory reports about predicted rainfall trends associated with increased temperature, and strong discrepancies among regions, even in the same country.<sup id="cite_ref-233" class="reference"><a href="#cite_note-233"><span class="cite-bracket">&#91;</span>233<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Erosion">Erosion</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=29" title="Edit section: Erosion"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:Riparian_buffer_on_Bear_Creek_in_Story_County,_Iowa.JPG" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/b/b6/Riparian_buffer_on_Bear_Creek_in_Story_County%2C_Iowa.JPG/170px-Riparian_buffer_on_Bear_Creek_in_Story_County%2C_Iowa.JPG" decoding="async" width="170" height="238" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/b/b6/Riparian_buffer_on_Bear_Creek_in_Story_County%2C_Iowa.JPG/255px-Riparian_buffer_on_Bear_Creek_in_Story_County%2C_Iowa.JPG 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/b/b6/Riparian_buffer_on_Bear_Creek_in_Story_County%2C_Iowa.JPG/340px-Riparian_buffer_on_Bear_Creek_in_Story_County%2C_Iowa.JPG 2x" data-file-width="1500" data-file-height="2100" /></a><figcaption>Erosion control</figcaption></figure> <p><a href="/wiki/Erosion" title="Erosion">Erosion</a> of soil is caused by <a href="/wiki/Water_erosion#Rainfall" class="mw-redirect" title="Water erosion">water</a>, <a href="/wiki/Water_erosion#Wind_erosion" class="mw-redirect" title="Water erosion">wind</a>, <a href="/wiki/Water_erosion#Glaciers" class="mw-redirect" title="Water erosion">ice</a>, and <a href="/wiki/Water_erosion#Mass_movement" class="mw-redirect" title="Water erosion">movement in response to gravity</a>. More than one kind of erosion can occur simultaneously. Erosion is distinguished from <a href="/wiki/Weathering" title="Weathering">weathering</a>, since erosion also transports eroded soil away from its place of origin (soil in transit may be described as <a href="/wiki/Sediment" title="Sediment">sediment</a>). Erosion is an intrinsic natural process, but in many places it is greatly increased by human activity, especially unsuitable land use practices.<sup id="cite_ref-234" class="reference"><a href="#cite_note-234"><span class="cite-bracket">&#91;</span>234<span class="cite-bracket">&#93;</span></a></sup> These include <a href="/wiki/Agriculture" title="Agriculture">agricultural</a> activities which leave the soil bare during times of heavy rain or strong winds, <a href="/wiki/Overgrazing" title="Overgrazing">overgrazing</a>, <a href="/wiki/Deforestation" title="Deforestation">deforestation</a>, and improper <a href="/wiki/Construction" title="Construction">construction</a> activity. Improved management can limit erosion. <a href="/wiki/Soil_conservation#Erosion_prevention" title="Soil conservation">Soil conservation techniques</a> which are employed include changes of land use (such as replacing erosion-prone <a href="/wiki/Crop" title="Crop">crops</a> with <a href="/wiki/Grass" class="mw-redirect" title="Grass">grass</a> or other soil-binding plants), changes to the timing or type of agricultural operations, <a href="/wiki/Terrace_(agriculture)" class="mw-redirect" title="Terrace (agriculture)">terrace</a> building, use of erosion-suppressing cover materials (including <a href="/wiki/Cover_crop#Water_management" title="Cover crop">cover crops</a> and other plants), limiting disturbance during construction, and avoiding construction during erosion-prone periods and in erosion-prone places such as steep slopes.<sup id="cite_ref-235" class="reference"><a href="#cite_note-235"><span class="cite-bracket">&#91;</span>235<span class="cite-bracket">&#93;</span></a></sup> Historically, one of the best examples of large-scale soil erosion due to unsuitable land-use practices is wind erosion (the so-called <a href="/wiki/Dust_Bowl" title="Dust Bowl">dust bowl</a>) which ruined American and Canadian prairies during the 1930s, when immigrant farmers, encouraged by the federal government of both countries, settled and converted the original <a href="/wiki/Shortgrass_prairie" title="Shortgrass prairie">shortgrass prairie</a> to <a href="/wiki/Agricultural_crops" class="mw-redirect" title="Agricultural crops">agricultural crops</a> and <a href="/wiki/Cattle_ranching" class="mw-redirect" title="Cattle ranching">cattle ranching</a>. </p><p>A serious and long-running water erosion problem occurs in <a href="/wiki/China" title="China">China</a>, on the middle reaches of the <a href="/wiki/Yellow_River" title="Yellow River">Yellow River</a> and the upper reaches of the <a href="/wiki/Yangtze_River" class="mw-redirect" title="Yangtze River">Yangtze River</a>. From the Yellow River, over 1.6&#160;billion tons of sediment flow each year into the ocean. The sediment originates primarily from water erosion (gully erosion) in the <a href="/wiki/Loess_Plateau" title="Loess Plateau">Loess Plateau</a> region of northwest China.<sup id="cite_ref-236" class="reference"><a href="#cite_note-236"><span class="cite-bracket">&#91;</span>236<span class="cite-bracket">&#93;</span></a></sup> </p><p>Soil piping is a particular form of soil erosion that occurs below the soil surface.<sup id="cite_ref-237" class="reference"><a href="#cite_note-237"><span class="cite-bracket">&#91;</span>237<span class="cite-bracket">&#93;</span></a></sup> It causes <a href="/wiki/Levee" title="Levee">levee</a> and dam failure, as well as <a href="/wiki/Sinkhole" title="Sinkhole">sink hole</a> formation. Turbulent flow removes soil starting at the mouth of the <a href="/wiki/Seep_(hydrology)" title="Seep (hydrology)">seep</a> flow and the <a href="/wiki/Subsoil" title="Subsoil">subsoil</a> erosion advances up-gradient.<sup id="cite_ref-238" class="reference"><a href="#cite_note-238"><span class="cite-bracket">&#91;</span>238<span class="cite-bracket">&#93;</span></a></sup> The term <a href="/wiki/Sand_boil" title="Sand boil">sand boil</a> is used to describe the appearance of the discharging end of an active soil pipe.<sup id="cite_ref-239" class="reference"><a href="#cite_note-239"><span class="cite-bracket">&#91;</span>239<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Salination">Salination</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=30" title="Edit section: Salination"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p><a href="/wiki/Soil_salination" class="mw-redirect" title="Soil salination">Soil salination</a> is the accumulation of free <a href="/wiki/Salt" title="Salt">salts</a> to such an extent that it leads to degradation of the agricultural value of soils and vegetation. Consequences include <a href="/wiki/Corrosion" title="Corrosion">corrosion</a> damage, reduced plant growth, erosion due to loss of plant cover and soil structure, and <a href="/wiki/Water_quality" title="Water quality">water quality</a> problems due to <a href="/wiki/Sedimentation" title="Sedimentation">sedimentation</a>. Salination occurs due to a combination of natural and human-caused processes. Arid conditions favour salt accumulation. This is especially apparent when soil parent material is saline. <a href="/wiki/Surface_irrigation" title="Surface irrigation">Irrigation</a> of arid lands is especially problematic.<sup id="cite_ref-240" class="reference"><a href="#cite_note-240"><span class="cite-bracket">&#91;</span>240<span class="cite-bracket">&#93;</span></a></sup> All irrigation water has some level of salinity. Irrigation, especially when it involves leakage from canals and overirrigation in the field, often raises the underlying <a href="/wiki/Water_table" title="Water table">water table</a>. Rapid salination occurs when the land surface is within the <a href="/wiki/Capillary_fringe" title="Capillary fringe">capillary fringe</a> of saline groundwater. <a href="/wiki/Soil_salinity_control" title="Soil salinity control">Soil salinity control</a> involves <a href="/wiki/Watertable_control" title="Watertable control">watertable control</a> and <a href="/wiki/Leaching_model" class="mw-redirect" title="Leaching model">flushing</a> with higher levels of applied water in combination with <a href="/wiki/Tile_drainage" title="Tile drainage">tile drainage</a> or another form of <a href="/wiki/Drainage_system_(agriculture)" title="Drainage system (agriculture)">subsurface drainage</a>.<sup id="cite_ref-241" class="reference"><a href="#cite_note-241"><span class="cite-bracket">&#91;</span>241<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Waterlog_242-0" class="reference"><a href="#cite_note-Waterlog-242"><span class="cite-bracket">&#91;</span>242<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Reclamation">Reclamation</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=31" title="Edit section: Reclamation"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Soil_regeneration" title="Soil regeneration">Soil regeneration</a></div> <p>Soils which contain high levels of particular clays with high swelling properties, such as <a href="/wiki/Smectite" title="Smectite">smectites</a>, are often very fertile. For example, the smectite-rich <a href="/wiki/Paddy_field" title="Paddy field">paddy</a> soils of Thailand's <a href="/wiki/Central_Thailand" title="Central Thailand">Central Plains</a> are among the most productive in the world. However, the overuse of mineral nitrogen <a href="/wiki/Fertilizer" title="Fertilizer">fertilizers</a> and pesticides in <a href="/wiki/Irrigation" title="Irrigation">irrigated</a> intensive <a href="/wiki/Rice_production_in_Thailand" title="Rice production in Thailand">rice production</a> has endangered these soils, forcing farmers to implement <a href="/wiki/Integrated_farming" title="Integrated farming">integrated practices</a> based on Cost Reduction Operating Principles.<sup id="cite_ref-243" class="reference"><a href="#cite_note-243"><span class="cite-bracket">&#91;</span>243<span class="cite-bracket">&#93;</span></a></sup> </p><p>Many farmers in tropical areas, however, struggle to retain organic matter and clay in the soils they work. In recent years, for example, productivity has declined and soil erosion has increased in the low-clay soils of northern Thailand, following the abandonment of <a href="/wiki/Shifting_cultivation" title="Shifting cultivation">shifting cultivation</a> for a more permanent land use.<sup id="cite_ref-244" class="reference"><a href="#cite_note-244"><span class="cite-bracket">&#91;</span>244<span class="cite-bracket">&#93;</span></a></sup> Farmers initially responded by adding organic matter and clay from <a href="/wiki/Mound-building_termites" title="Mound-building termites">termite mound</a> material, but this was <a href="/wiki/Sustainability" title="Sustainability">unsustainable</a> in the long-term because of rarefaction of termite mounds. Scientists experimented with adding <a href="/wiki/Bentonite" title="Bentonite">bentonite</a>, one of the smectite family of clays, to the soil. In field trials, conducted by scientists from the <a href="/wiki/International_Water_Management_Institute" title="International Water Management Institute">International Water Management Institute</a> (IWMI) in cooperation with <a href="/wiki/Khon_Kaen_University" title="Khon Kaen University">Khon Kaen University</a> and local farmers, this had the effect of helping retain water and nutrients. Supplementing the farmer's usual practice with a single application of 200 <a href="/wiki/Kilogram" title="Kilogram">kilograms</a> per <a href="/wiki/Rai_(unit)" class="mw-redirect" title="Rai (unit)">rai</a> (1,300&#160;kg/ha; 1,100&#160;lb/acre) of bentonite resulted in an average yield increase of 73%.<sup id="cite_ref-245" class="reference"><a href="#cite_note-245"><span class="cite-bracket">&#91;</span>245<span class="cite-bracket">&#93;</span></a></sup> Other studies showed that applying bentonite to degraded sandy soils reduced the risk of crop failure during drought years.<sup id="cite_ref-246" class="reference"><a href="#cite_note-246"><span class="cite-bracket">&#91;</span>246<span class="cite-bracket">&#93;</span></a></sup> </p><p>In 2008, three years after the initial trials, IWMI scientists conducted a survey among 250 farmers in northeast Thailand, half of whom had applied bentonite to their fields. The average improvement for those using the clay addition was 18% higher than for non-clay users. Using the clay had enabled some farmers to switch to growing vegetables, which need more fertile soil. This helped to increase their income. The researchers estimated that 200 farmers in northeast Thailand and 400 in Cambodia had adopted the use of clays, and that a further 20,000 farmers were introduced to the new technique.<sup id="cite_ref-Water_Management_Institute2010_247-0" class="reference"><a href="#cite_note-Water_Management_Institute2010-247"><span class="cite-bracket">&#91;</span>247<span class="cite-bracket">&#93;</span></a></sup> </p><p>If the soil is too high in clay or salts (e.g. <a href="/wiki/Saline_sodic_soil" class="mw-redirect" title="Saline sodic soil">saline sodic soil</a>), adding gypsum, washed river sand and organic matter (e.g.<a href="/wiki/Municipal_solid_waste" title="Municipal solid waste">municipal solid waste</a>) will balance the composition.<sup id="cite_ref-248" class="reference"><a href="#cite_note-248"><span class="cite-bracket">&#91;</span>248<span class="cite-bracket">&#93;</span></a></sup> </p><p>Adding organic matter, like <a href="/wiki/Ramial_chipped_wood" title="Ramial chipped wood">ramial chipped wood</a> or <a href="/wiki/Compost" title="Compost">compost</a>, to soil which is depleted in nutrients and too high in sand will boost its quality and improve production.<sup id="cite_ref-249" class="reference"><a href="#cite_note-249"><span class="cite-bracket">&#91;</span>249<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-250" class="reference"><a href="#cite_note-250"><span class="cite-bracket">&#91;</span>250<span class="cite-bracket">&#93;</span></a></sup> </p><p>Special mention must be made of the use of <a href="/wiki/Charcoal" title="Charcoal">charcoal</a>, and more generally <a href="/wiki/Biochar" title="Biochar">biochar</a> to improve nutrient-poor tropical soils, a process based on the higher fertility of anthropogenic <a href="/wiki/Pre-Columbian_era" title="Pre-Columbian era">pre-Columbian</a> Amazonian <a href="/wiki/Dark_earth" title="Dark earth">Dark Earths</a>, also called <a href="/wiki/Terra_Preta" class="mw-redirect" title="Terra Preta">Terra Preta</a> de Índio, due to interesting physical and chemical properties of soil black carbon as a source of stable humus.<sup id="cite_ref-251" class="reference"><a href="#cite_note-251"><span class="cite-bracket">&#91;</span>251<span class="cite-bracket">&#93;</span></a></sup> However, the uncontrolled application of <a href="/wiki/Charring" title="Charring">charred</a> waste products of all kinds may endanger soil life and human health.<sup id="cite_ref-252" class="reference"><a href="#cite_note-252"><span class="cite-bracket">&#91;</span>252<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="History_of_studies_and_research">History of studies and research</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=32" title="Edit section: History of studies and research"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>The history of the study of soil is intimately tied to humans' urgent need to provide food for themselves and forage for their animals. Throughout history, civilizations have prospered or declined as a function of the availability and productivity of their soils.<sup id="cite_ref-253" class="reference"><a href="#cite_note-253"><span class="cite-bracket">&#91;</span>253<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Studies_of_soil_fertility">Studies of soil fertility</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=33" title="Edit section: Studies of soil fertility"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">Main article: <a href="/wiki/Soil_fertility" title="Soil fertility">Soil fertility</a></div> <p>The Greek historian <a href="/wiki/Xenophon" title="Xenophon">Xenophon</a> (450–355&#160;<a href="/wiki/Before_the_Common_Era" class="mw-redirect" title="Before the Common Era">BCE</a>) was the first to expound upon the merits of green-manuring crops: 'But then whatever weeds are upon the ground, being turned into earth, enrich the soil as much as dung.'<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna19774_254-0" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna19774-254"><span class="cite-bracket">&#91;</span>254<span class="cite-bracket">&#93;</span></a></sup> </p><p><a href="/wiki/Columella" title="Columella">Columella</a>'s <i>Of husbandry</i>, circa 60&#160;<a href="/wiki/Common_Era" title="Common Era">CE</a>, advocated the use of lime and that <a href="/wiki/Clover" title="Clover">clover</a> and <a href="/wiki/Alfalfa" title="Alfalfa">alfalfa</a> (<a href="/wiki/Green_manure" title="Green manure">green manure</a>) should be turned under,<sup id="cite_ref-255" class="reference"><a href="#cite_note-255"><span class="cite-bracket">&#91;</span>255<span class="cite-bracket">&#93;</span></a></sup> and was used by 15 generations (450&#160;years) under the <a href="/wiki/Roman_Empire" title="Roman Empire">Roman Empire</a> until its collapse.<sup id="cite_ref-FOOTNOTEDonahueMillerShickluna19774_254-1" class="reference"><a href="#cite_note-FOOTNOTEDonahueMillerShickluna19774-254"><span class="cite-bracket">&#91;</span>254<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-FOOTNOTEKellogg19571_256-0" class="reference"><a href="#cite_note-FOOTNOTEKellogg19571-256"><span class="cite-bracket">&#91;</span>256<span class="cite-bracket">&#93;</span></a></sup> From the <a href="/wiki/Fall_of_Rome" class="mw-redirect" title="Fall of Rome">fall of Rome</a> to the <a href="/wiki/French_Revolution" title="French Revolution">French Revolution</a>, knowledge of soil and agriculture was passed on from parent to child and as a result, crop yields were low. During the European <a href="/wiki/Middle_Ages" title="Middle Ages">Middle Ages</a>, <a href="/wiki/Ibn_al-%27Awwam" title="Ibn al-&#39;Awwam">Yahya Ibn al-'Awwam</a>'s handbook,<sup id="cite_ref-257" class="reference"><a href="#cite_note-257"><span class="cite-bracket">&#91;</span>257<span class="cite-bracket">&#93;</span></a></sup> with its emphasis on irrigation, guided the people of North Africa, Spain and the <a href="/wiki/Middle_East" title="Middle East">Middle East</a>; a translation of this work was finally carried to the southwest of the United States when under Spanish influence.<sup id="cite_ref-258" class="reference"><a href="#cite_note-258"><span class="cite-bracket">&#91;</span>258<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Olivier_de_Serres" title="Olivier de Serres">Olivier de Serres</a>, considered the father of French <a href="/wiki/Agronomy" title="Agronomy">agronomy</a>, was the first to suggest the abandonment of <a href="/wiki/Fallowing" class="mw-redirect" title="Fallowing">fallowing</a> and its replacement by hay <a href="/wiki/Meadows" class="mw-redirect" title="Meadows">meadows</a> within <a href="/wiki/Crop_rotation" title="Crop rotation">crop rotations</a>. He also highlighted the importance of soil (the French <a href="/wiki/Terroir" title="Terroir">terroir</a>) in the management of vineyards. His famous book <span title="French-language text"><i lang="fr">Le Théâtre d'Agriculture et mesnage des champs</i></span><sup id="cite_ref-259" class="reference"><a href="#cite_note-259"><span class="cite-bracket">&#91;</span>259<span class="cite-bracket">&#93;</span></a></sup> contributed to the rise of modern, <a href="/wiki/Sustainable_agriculture" title="Sustainable agriculture">sustainable agriculture</a> and to the collapse of old <a href="/wiki/Agricultural_practices" class="mw-redirect" title="Agricultural practices">agricultural practices</a> such as <a href="/wiki/Soil_amendment" class="mw-redirect" title="Soil amendment">soil amendment</a> for crops by the lifting of <a href="/wiki/Forest_litter" class="mw-redirect" title="Forest litter">forest litter</a> and <a href="/wiki/Assarting" title="Assarting">assarting</a>, which ruined the soils of western Europe during the Middle Ages and even later on according to regions.<sup id="cite_ref-260" class="reference"><a href="#cite_note-260"><span class="cite-bracket">&#91;</span>260<span class="cite-bracket">&#93;</span></a></sup> </p><p>Experiments into what made plants grow first led to the idea that the ash left behind when plant matter was burned was the essential element but overlooked the role of nitrogen, which is not left on the ground after combustion, a belief which prevailed until the 19th century.<sup id="cite_ref-261" class="reference"><a href="#cite_note-261"><span class="cite-bracket">&#91;</span>261<span class="cite-bracket">&#93;</span></a></sup> In about 1635, the Flemish chemist <a href="/wiki/Jan_Baptist_van_Helmont" title="Jan Baptist van Helmont">Jan Baptist van Helmont</a> thought he had proved water to be the essential element from his famous five years' experiment with a willow tree grown with only the addition of rainwater. His conclusion came from the fact that the increase in the plant's weight had apparently been produced only by the addition of water, with no reduction in the soil's weight.<sup id="cite_ref-262" class="reference"><a href="#cite_note-262"><span class="cite-bracket">&#91;</span>262<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Brady_263-0" class="reference"><a href="#cite_note-Brady-263"><span class="cite-bracket">&#91;</span>263<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-FOOTNOTEKellogg19573_264-0" class="reference"><a href="#cite_note-FOOTNOTEKellogg19573-264"><span class="cite-bracket">&#91;</span>264<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/John_Woodward_(naturalist)" title="John Woodward (naturalist)">John Woodward</a> (<abbr title="died">d.</abbr>&#160;1728) experimented with various types of water ranging from clean to muddy and found muddy water the best, and so he concluded that earthy matter was the essential element. Others concluded it was humus in the soil that passed some essence to the growing plant. Still others held that the vital growth principal was something passed from dead plants or animals to the new plants. At the start of the 18th century, <a href="/wiki/Jethro_Tull_(agriculturist)" title="Jethro Tull (agriculturist)">Jethro Tull</a> demonstrated that it was beneficial to cultivate (stir) the soil, but his opinion that the stirring made the fine parts of soil available for plant absorption was erroneous.<sup id="cite_ref-Brady_263-1" class="reference"><a href="#cite_note-Brady-263"><span class="cite-bracket">&#91;</span>263<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-FOOTNOTEKellogg19572_265-0" class="reference"><a href="#cite_note-FOOTNOTEKellogg19572-265"><span class="cite-bracket">&#91;</span>265<span class="cite-bracket">&#93;</span></a></sup> </p><p>As chemistry developed, it was applied to the investigation of soil fertility. The French chemist <a href="/wiki/Antoine_Lavoisier" title="Antoine Lavoisier">Antoine Lavoisier</a> showed in about 1778 that plants and animals must <a href="/wiki/Combustion" title="Combustion">combust</a> oxygen internally to live. He was able to deduce that most of the 165-pound (75&#160;kg) weight of van Helmont's willow tree derived from air.<sup id="cite_ref-266" class="reference"><a href="#cite_note-266"><span class="cite-bracket">&#91;</span>266<span class="cite-bracket">&#93;</span></a></sup> It was the French agriculturalist <a href="/wiki/Jean-Baptiste_Boussingault" title="Jean-Baptiste Boussingault">Jean-Baptiste Boussingault</a> who by means of experimentation obtained evidence showing that the main sources of carbon, hydrogen and oxygen for plants were air and water, while nitrogen was taken from soil.<sup id="cite_ref-267" class="reference"><a href="#cite_note-267"><span class="cite-bracket">&#91;</span>267<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Justus_von_Liebig" title="Justus von Liebig">Justus von Liebig</a> in his book <i>Organic chemistry in its applications to agriculture and physiology</i> (published 1840), asserted that the chemicals in plants must have come from the soil and air and that to maintain soil fertility, the used minerals must be replaced.<sup id="cite_ref-268" class="reference"><a href="#cite_note-268"><span class="cite-bracket">&#91;</span>268<span class="cite-bracket">&#93;</span></a></sup> Liebig nevertheless believed the nitrogen was supplied from the air. The enrichment of soil with guano by the Incas was rediscovered in 1802, by <a href="/wiki/Alexander_von_Humboldt" title="Alexander von Humboldt">Alexander von Humboldt</a>. This led to its mining and that of Chilean nitrate and to its application to soil in the United States and Europe after 1840.<sup id="cite_ref-269" class="reference"><a href="#cite_note-269"><span class="cite-bracket">&#91;</span>269<span class="cite-bracket">&#93;</span></a></sup> </p><p>The work of Liebig was a revolution for agriculture, and so other investigators started experimentation based on it. In England <a href="/wiki/John_Bennet_Lawes" title="John Bennet Lawes">John Bennet Lawes</a> and <a href="/wiki/Joseph_Henry_Gilbert" title="Joseph Henry Gilbert">Joseph Henry Gilbert</a> worked in the <a href="/wiki/Rothamsted_Research" title="Rothamsted Research">Rothamsted Experimental Station</a>, founded by the former, and (re)discovered that plants took nitrogen from the soil, and that salts needed to be in an available state to be absorbed by plants. Their investigations also produced the <a href="/wiki/Superphosphate" title="Superphosphate">superphosphate</a>, consisting in the acid treatment of phosphate rock.<sup id="cite_ref-FOOTNOTEKellogg19574_270-0" class="reference"><a href="#cite_note-FOOTNOTEKellogg19574-270"><span class="cite-bracket">&#91;</span>270<span class="cite-bracket">&#93;</span></a></sup> This led to the invention and use of salts of potassium (K) and nitrogen (N) as fertilizers. Ammonia generated by the production of <a href="/wiki/Coke_(fuel)" title="Coke (fuel)">coke</a> was recovered and used as fertiliser.<sup id="cite_ref-271" class="reference"><a href="#cite_note-271"><span class="cite-bracket">&#91;</span>271<span class="cite-bracket">&#93;</span></a></sup> Finally, the chemical basis of nutrients delivered to the soil in manure was understood and in the mid-19th century chemical fertilisers were applied. However, the dynamic interaction of soil and its life forms was still not understood. </p><p>In 1856, J. Thomas Way discovered that ammonia contained in fertilisers was transformed into nitrates,<sup id="cite_ref-272" class="reference"><a href="#cite_note-272"><span class="cite-bracket">&#91;</span>272<span class="cite-bracket">&#93;</span></a></sup> and twenty years later <a href="/wiki/Robert_Warington" title="Robert Warington">Robert Warington</a> proved that this transformation was done by living organisms.<sup id="cite_ref-273" class="reference"><a href="#cite_note-273"><span class="cite-bracket">&#91;</span>273<span class="cite-bracket">&#93;</span></a></sup> In 1890 <a href="/wiki/Sergei_Winogradsky" title="Sergei Winogradsky">Sergei Winogradsky</a> announced he had found the bacteria responsible for this transformation.<sup id="cite_ref-274" class="reference"><a href="#cite_note-274"><span class="cite-bracket">&#91;</span>274<span class="cite-bracket">&#93;</span></a></sup> </p><p>It was known that certain <a href="/wiki/Legume" title="Legume">legumes</a> could take up nitrogen from the air and fix it to the soil but it took the development of bacteriology towards the end of the 19th century to lead to an understanding of the role played in nitrogen fixation by bacteria. The symbiosis of bacteria and leguminous roots, and the fixation of nitrogen by the bacteria, were simultaneously discovered by the German agronomist <a href="/wiki/Hermann_Hellriegel" title="Hermann Hellriegel">Hermann Hellriegel</a> and the Dutch microbiologist <a href="/wiki/Martinus_Beijerinck" title="Martinus Beijerinck">Martinus Beijerinck</a>.<sup id="cite_ref-FOOTNOTEKellogg19574_270-1" class="reference"><a href="#cite_note-FOOTNOTEKellogg19574-270"><span class="cite-bracket">&#91;</span>270<span class="cite-bracket">&#93;</span></a></sup> </p><p>Crop rotation, mechanisation, chemical and natural fertilisers led to a doubling of wheat yields in western Europe between 1800 and 1900.<sup id="cite_ref-FOOTNOTEKellogg19571–4_275-0" class="reference"><a href="#cite_note-FOOTNOTEKellogg19571–4-275"><span class="cite-bracket">&#91;</span>275<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Studies_of_soil_formation">Studies of soil formation</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=34" title="Edit section: Studies of soil formation"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951"><div role="note" class="hatnote navigation-not-searchable">See also: <a href="/wiki/Soil_formation" title="Soil formation">Soil formation</a></div> <p>Scientists who studied soil in connection with agricultural practices considered it mainly a static substrate. However, the soil is the result of evolution from more ancient geological materials under the action of biotic and abiotic processes. After studies of soil improvement commenced, other researchers began to study soil genesis and, as a result, soil types and classifications. </p><p>In 1860, while in Mississippi, <a href="/wiki/Eugene_W._Hilgard" title="Eugene W. Hilgard">Eugene W. Hilgard</a> (1833–1916) studied the relationship between rock material, climate, vegetation, and the type of soils that were developed. He realised that the soils were dynamic and considered the classification of soil types.<sup id="cite_ref-276" class="reference"><a href="#cite_note-276"><span class="cite-bracket">&#91;</span>276<span class="cite-bracket">&#93;</span></a></sup> (See also at <a rel="nofollow" class="external text" href="https://www.gutenberg.org/ebooks/73975">Project Gutenberg</a>). His work was not continued. At about the same time, <a href="/wiki/Friedrich_Albert_Fallou" title="Friedrich Albert Fallou">Friedrich Albert Fallou</a> described soil profiles and related soil characteristics to their formation as part of his professional work evaluating forest and farmland for the principality of <a href="/wiki/Saxony" title="Saxony">Saxony</a>. His 1857 book, <span title="German-language text"><i lang="de">Anfangsgründe der Bodenkunde</i></span> (First Principles of soil science), established modern soil science.<sup id="cite_ref-277" class="reference"><a href="#cite_note-277"><span class="cite-bracket">&#91;</span>277<span class="cite-bracket">&#93;</span></a></sup> Contemporary with Fallou's work, and driven by the same need to accurately assess land for equitable taxation, Vasily Dokuchaev led a team of soil scientists in Russia who conducted an extensive survey of soils, observing that similar basic rocks, climate and vegetation types lead to similar soil layering and types, and established the concepts for soil classifications. Due to language barriers, the work of this team was not communicated to Western Europe until 1914 through a publication in German by <a href="/wiki/Konstantin_Glinka" title="Konstantin Glinka">Konstantin Glinka</a>, a member of the Russian team.<sup id="cite_ref-278" class="reference"><a href="#cite_note-278"><span class="cite-bracket">&#91;</span>278<span class="cite-bracket">&#93;</span></a></sup> </p><p><a href="/wiki/Curtis_F._Marbut" title="Curtis F. Marbut">Curtis F. Marbut</a>, influenced by the work of the Russian team, translated Glinka's publication into English,<sup id="cite_ref-279" class="reference"><a href="#cite_note-279"><span class="cite-bracket">&#91;</span>279<span class="cite-bracket">&#93;</span></a></sup> and, as he was placed in charge of the U.S. <a href="/wiki/National_Cooperative_Soil_Survey" title="National Cooperative Soil Survey">National Cooperative Soil Survey</a>, applied it to a national soil classification system.<sup id="cite_ref-Brady_263-2" class="reference"><a href="#cite_note-Brady-263"><span class="cite-bracket">&#91;</span>263<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="See_also">See also</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=35" title="Edit section: See also"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style 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class="portalbox-image"><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Aegopodium_podagraria1_ies.jpg" class="mw-file-description"><img alt="icon" src="//upload.wikimedia.org/wikipedia/commons/thumb/b/bf/Aegopodium_podagraria1_ies.jpg/32px-Aegopodium_podagraria1_ies.jpg" decoding="async" width="32" height="28" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/b/bf/Aegopodium_podagraria1_ies.jpg/48px-Aegopodium_podagraria1_ies.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/b/bf/Aegopodium_podagraria1_ies.jpg/64px-Aegopodium_podagraria1_ies.jpg 2x" data-file-width="800" data-file-height="700" /></a></span></span><span class="portalbox-link"><a href="/wiki/Portal:Environment" title="Portal:Environment">Environment portal</a></span></li><li class="portalbox-entry"><span class="portalbox-image"><span class="noviewer" typeof="mw:File"><a href="/wiki/File:WikiProject_Geology.svg" class="mw-file-description"><img alt="icon" src="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/WikiProject_Geology.svg/28px-WikiProject_Geology.svg.png" decoding="async" width="28" height="28" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/WikiProject_Geology.svg/42px-WikiProject_Geology.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/e/e7/WikiProject_Geology.svg/56px-WikiProject_Geology.svg.png 2x" data-file-width="327" data-file-height="328" /></a></span></span><span class="portalbox-link"><a href="/wiki/Portal:Geology" title="Portal:Geology">Geology portal</a></span></li></ul> <style data-mw-deduplicate="TemplateStyles:r1184024115">.mw-parser-output .div-col{margin-top:0.3em;column-width:30em}.mw-parser-output .div-col-small{font-size:90%}.mw-parser-output .div-col-rules{column-rule:1px solid #aaa}.mw-parser-output .div-col dl,.mw-parser-output .div-col ol,.mw-parser-output .div-col ul{margin-top:0}.mw-parser-output .div-col li,.mw-parser-output .div-col dd{page-break-inside:avoid;break-inside:avoid-column}</style><div class="div-col"> <ul><li><a href="/wiki/Acid_sulfate_soil" title="Acid sulfate soil">Acid sulfate soil</a></li> <li><a href="/wiki/Agricultural_science" title="Agricultural science">Agricultural science</a></li> <li><a href="/wiki/Agrophysics" title="Agrophysics">Agrophysics</a></li> <li><a href="/wiki/Crust_(geology)" title="Crust (geology)">Crust</a></li> <li><a href="/wiki/Factors_affecting_permeability_of_soils" class="mw-redirect" title="Factors affecting permeability of soils">Factors affecting permeability of soils</a></li> <li><a href="/wiki/Index_of_soil-related_articles" title="Index of soil-related articles">Index of soil-related articles</a></li> <li><a href="/wiki/Lunar_soil" class="mw-redirect" title="Lunar soil">Lunar soil</a> and <a href="/wiki/Martian_soil" class="mw-redirect" title="Martian soil">martian soil</a></li> <li><a href="/wiki/Mycorrhizal_fungi_and_soil_carbon_storage" title="Mycorrhizal fungi and soil carbon storage">Mycorrhizal fungi and soil carbon storage</a></li> <li><a href="/wiki/Red_soil" title="Red soil">Red soil</a></li> <li><a href="/wiki/Shrink%E2%80%93swell_capacity" title="Shrink–swell capacity">Shrink–swell capacity</a></li> <li><a href="/wiki/Soil_biodiversity" title="Soil biodiversity">Soil biodiversity</a></li> <li><a href="/wiki/Soil_liquefaction" title="Soil liquefaction">Soil liquefaction</a></li> <li><a href="/wiki/Soil_moisture_velocity_equation" title="Soil moisture velocity equation">Soil moisture velocity equation</a></li> <li><a href="/wiki/Soil_zoology" title="Soil zoology">Soil zoology</a></li> <li><a href="/wiki/Tillage_erosion" title="Tillage erosion">Tillage erosion</a></li> <li><a href="/wiki/World_Soil_Museum" title="World Soil Museum">World Soil Museum</a></li></ul></div> <div class="mw-heading mw-heading2"><h2 id="References">References</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=36" title="Edit section: References"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1239543626">.mw-parser-output .reflist{margin-bottom:0.5em;list-style-type:decimal}@media screen{.mw-parser-output .reflist{font-size:90%}}.mw-parser-output .reflist .references{font-size:100%;margin-bottom:0;list-style-type:inherit}.mw-parser-output .reflist-columns-2{column-width:30em}.mw-parser-output .reflist-columns-3{column-width:25em}.mw-parser-output .reflist-columns{margin-top:0.3em}.mw-parser-output .reflist-columns ol{margin-top:0}.mw-parser-output .reflist-columns li{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .reflist-upper-alpha{list-style-type:upper-alpha}.mw-parser-output .reflist-upper-roman{list-style-type:upper-roman}.mw-parser-output .reflist-lower-alpha{list-style-type:lower-alpha}.mw-parser-output .reflist-lower-greek{list-style-type:lower-greek}.mw-parser-output .reflist-lower-roman{list-style-type:lower-roman}</style><div class="reflist"> <div class="mw-references-wrap mw-references-columns"><ol class="references"> <li id="cite_note-1"><span class="mw-cite-backlink"><b><a href="#cite_ref-1">^</a></b></span> <span class="reference-text"><style data-mw-deduplicate="TemplateStyles:r1238218222">.mw-parser-output cite.citation{font-style:inherit;word-wrap:break-word}.mw-parser-output .citation q{quotes:"\"""\"""'""'"}.mw-parser-output .citation:target{background-color:rgba(0,127,255,0.133)}.mw-parser-output .id-lock-free.id-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/6/65/Lock-green.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-limited.id-lock-limited a,.mw-parser-output .id-lock-registration.id-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/d/d6/Lock-gray-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-subscription.id-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/a/aa/Lock-red-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .cs1-ws-icon a{background:url("//upload.wikimedia.org/wikipedia/commons/4/4c/Wikisource-logo.svg")right 0.1em center/12px no-repeat}body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-free a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-limited a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-registration a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-subscription a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .cs1-ws-icon a{background-size:contain;padding:0 1em 0 0}.mw-parser-output .cs1-code{color:inherit;background:inherit;border:none;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;color:var(--color-error,#d33)}.mw-parser-output .cs1-visible-error{color:var(--color-error,#d33)}.mw-parser-output .cs1-maint{display:none;color:#085;margin-left:0.3em}.mw-parser-output .cs1-kern-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right{padding-right:0.2em}.mw-parser-output .citation .mw-selflink{font-weight:inherit}@media screen{.mw-parser-output .cs1-format{font-size:95%}html.skin-theme-clientpref-night .mw-parser-output .cs1-maint{color:#18911f}}@media screen and (prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output .cs1-maint{color:#18911f}}</style><cite id="CITEREFVoroneyHeck2007" class="citation book cs1">Voroney, R. Paul; Heck, Richard J. (2007). <a rel="nofollow" class="external text" href="https://fr.art1lib.org/book/34240339/73458e">"The soil habitat"</a>. In Paul, Eldor A. (ed.). <i>Soil microbiology, ecology and biochemistry</i> (3rd&#160;ed.). Amsterdam, the Netherlands: <a href="/wiki/Elsevier" title="Elsevier">Elsevier</a>. pp.&#160;25–49. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1016%2FB978-0-08-047514-1.50006-8">10.1016/B978-0-08-047514-1.50006-8</a>. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/978-0-12-546807-7" title="Special:BookSources/978-0-12-546807-7"><bdi>978-0-12-546807-7</bdi></a>. <a rel="nofollow" class="external text" href="https://web.archive.org/web/20180710102532/http://csmi.issas.ac.cn/uploadfiles/Soil%20Microbiology%2C%20Ecology%20%26%20Biochemistry.pdf">Archived</a> <span class="cs1-format">(PDF)</span> from the original on 10 July 2018<span class="reference-accessdate">. Retrieved <span class="nowrap">27 March</span> 2022</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=bookitem&amp;rft.atitle=The+soil+habitat&amp;rft.btitle=Soil+microbiology%2C+ecology+and+biochemistry&amp;rft.place=Amsterdam%2C+the+Netherlands&amp;rft.pages=25-49&amp;rft.edition=3rd&amp;rft.pub=Elsevier&amp;rft.date=2007&amp;rft_id=info%3Adoi%2F10.1016%2FB978-0-08-047514-1.50006-8&amp;rft.isbn=978-0-12-546807-7&amp;rft.aulast=Voroney&amp;rft.aufirst=R.+Paul&amp;rft.au=Heck%2C+Richard+J.&amp;rft_id=https%3A%2F%2Ffr.art1lib.org%2Fbook%2F34240339%2F73458e&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-2"><span class="mw-cite-backlink"><b><a href="#cite_ref-2">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFTaylorAshcroft1972" class="citation book cs1">Taylor, Sterling A.; Ashcroft, Gaylen L. (1972). <span class="id-lock-registration" title="Free registration required"><a rel="nofollow" class="external text" href="https://archive.org/details/physicaledapholo0000tayl"><i>Physical edaphology: the physics of irrigated and nonirrigated soils</i></a></span>. San Francisco, California: <a href="/wiki/W._H._Freeman_and_Company" title="W. H. Freeman and Company">W.H. Freeman</a>. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/978-0-7167-0818-6" title="Special:BookSources/978-0-7167-0818-6"><bdi>978-0-7167-0818-6</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Physical+edaphology%3A+the+physics+of+irrigated+and+nonirrigated+soils&amp;rft.place=San+Francisco%2C+California&amp;rft.pub=W.H.+Freeman&amp;rft.date=1972&amp;rft.isbn=978-0-7167-0818-6&amp;rft.aulast=Taylor&amp;rft.aufirst=Sterling+A.&amp;rft.au=Ashcroft%2C+Gaylen+L.&amp;rft_id=https%3A%2F%2Farchive.org%2Fdetails%2Fphysicaledapholo0000tayl&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-3"><span class="mw-cite-backlink"><b><a href="#cite_ref-3">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFMcCarthy2014" class="citation book cs1">McCarthy, David F. (2014). <a rel="nofollow" class="external text" href="https://web.archive.org/web/20221016144604/https://fr.b-ok.cc/book/3555343/0f8f97"><i>Essentials of soil mechanics and foundations: basic geotechnics</i></a> (7th&#160;ed.). London, United Kingdom: <a href="/wiki/Pearson_Education" title="Pearson Education">Pearson</a>. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/9781292039398" title="Special:BookSources/9781292039398"><bdi>9781292039398</bdi></a>. Archived from <a rel="nofollow" class="external text" href="https://fr.book4you.org/book/3555343/0f8f97">the original</a> on 16 October 2022<span class="reference-accessdate">. Retrieved <span class="nowrap">27 March</span> 2022</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Essentials+of+soil+mechanics+and+foundations%3A+basic+geotechnics&amp;rft.place=London%2C+United+Kingdom&amp;rft.edition=7th&amp;rft.pub=Pearson&amp;rft.date=2014&amp;rft.isbn=9781292039398&amp;rft.aulast=McCarthy&amp;rft.aufirst=David+F.&amp;rft_id=https%3A%2F%2Ffr.book4you.org%2Fbook%2F3555343%2F0f8f97&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-Gilluly1975-4"><span class="mw-cite-backlink"><b><a href="#cite_ref-Gilluly1975_4-0">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFGillulyWatersWoodford1975" class="citation book cs1"><a href="/wiki/James_Gilluly" title="James Gilluly">Gilluly, James</a>; Waters, Aaron Clement; Woodford, Alfred Oswald (1975). <span class="id-lock-registration" title="Free registration required"><a rel="nofollow" class="external text" href="https://archive.org/details/principlesofgeol0000gill"><i>Principles of geology</i></a></span> (4th&#160;ed.). San Francisco, California: <a href="/wiki/W._H._Freeman_and_Company" title="W. H. Freeman and Company">W.H. Freeman</a>. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/978-0-7167-0269-6" title="Special:BookSources/978-0-7167-0269-6"><bdi>978-0-7167-0269-6</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Principles+of+geology&amp;rft.place=San+Francisco%2C+California&amp;rft.edition=4th&amp;rft.pub=W.H.+Freeman&amp;rft.date=1975&amp;rft.isbn=978-0-7167-0269-6&amp;rft.aulast=Gilluly&amp;rft.aufirst=James&amp;rft.au=Waters%2C+Aaron+Clement&amp;rft.au=Woodford%2C+Alfred+Oswald&amp;rft_id=https%3A%2F%2Farchive.org%2Fdetails%2Fprinciplesofgeol0000gill&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-5"><span class="mw-cite-backlink"><b><a href="#cite_ref-5">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFHuggett2011" class="citation book cs1">Huggett, Richard John (2011). "What is geomorphology?". <a rel="nofollow" class="external text" href="https://cc1lib.vip/book/1220195/5e924c"><i>Fundamentals of geomorphology</i></a>. Routledge Fundamentals of Physical Geography Series (3rd&#160;ed.). London, United Kingdom: <a href="/wiki/Routledge" title="Routledge">Routledge</a>. pp.&#160;148–150. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/978-0-203-86008-3" title="Special:BookSources/978-0-203-86008-3"><bdi>978-0-203-86008-3</bdi></a><span class="reference-accessdate">. Retrieved <span class="nowrap">16 October</span> 2022</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=bookitem&amp;rft.atitle=What+is+geomorphology%3F&amp;rft.btitle=Fundamentals+of+geomorphology&amp;rft.place=London%2C+United+Kingdom&amp;rft.series=Routledge+Fundamentals+of+Physical+Geography+Series&amp;rft.pages=148-150&amp;rft.edition=3rd&amp;rft.pub=Routledge&amp;rft.date=2011&amp;rft.isbn=978-0-203-86008-3&amp;rft.aulast=Huggett&amp;rft.aufirst=Richard+John&amp;rft_id=https%3A%2F%2Fcc1lib.vip%2Fbook%2F1220195%2F5e924c&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span><sup class="noprint Inline-Template"><span style="white-space: nowrap;">&#91;<i><a href="/wiki/Wikipedia:Link_rot" title="Wikipedia:Link rot"><span title="&#160;Dead link tagged August 2023">permanent dead link</span></a></i><span style="visibility:hidden; color:transparent; padding-left:2px">&#8205;</span>&#93;</span></sup></span> </li> <li id="cite_note-6"><span class="mw-cite-backlink"><b><a href="#cite_ref-6">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFPonge2015" class="citation journal cs1">Ponge, Jean-François (2015). <a rel="nofollow" class="external text" href="https://www.researchgate.net/publication/276090499">"The soil as an ecosystem"</a>. <i>Biology and Fertility of Soils</i>. <b>51</b> (6): 645–648. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2015BioFS..51..645P">2015BioFS..51..645P</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1007%2Fs00374-015-1016-1">10.1007/s00374-015-1016-1</a>. <a href="/wiki/S2CID_(identifier)" class="mw-redirect" title="S2CID (identifier)">S2CID</a>&#160;<a rel="nofollow" class="external text" href="https://api.semanticscholar.org/CorpusID:18251180">18251180</a><span class="reference-accessdate">. Retrieved <span class="nowrap">3 April</span> 2022</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=article&amp;rft.jtitle=Biology+and+Fertility+of+Soils&amp;rft.atitle=The+soil+as+an+ecosystem&amp;rft.volume=51&amp;rft.issue=6&amp;rft.pages=645-648&amp;rft.date=2015&amp;rft_id=https%3A%2F%2Fapi.semanticscholar.org%2FCorpusID%3A18251180%23id-name%3DS2CID&amp;rft_id=info%3Adoi%2F10.1007%2Fs00374-015-1016-1&amp;rft_id=info%3Abibcode%2F2015BioFS..51..645P&amp;rft.aulast=Ponge&amp;rft.aufirst=Jean-Fran%C3%A7ois&amp;rft_id=https%3A%2F%2Fwww.researchgate.net%2Fpublication%2F276090499&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-Yu2015-7"><span class="mw-cite-backlink"><b><a href="#cite_ref-Yu2015_7-0">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFYuKambojWangCheng2015" class="citation web cs1">Yu, Charley; Kamboj, Sunita; Wang, Cheng; Cheng, Jing-Jy (2015). <a rel="nofollow" class="external text" href="https://resrad.evs.anl.gov/docs/data_collection.pdf">"Data collection handbook to support modeling impacts of radioactive material in soil and building structures"</a> <span class="cs1-format">(PDF)</span>. <i><a href="/wiki/Argonne_National_Laboratory" title="Argonne National Laboratory">Argonne National Laboratory</a></i>. pp.&#160;13–21. <a rel="nofollow" class="external text" href="https://web.archive.org/web/20180804105951/http://resrad.evs.anl.gov/docs/data_collection.pdf">Archived</a> <span class="cs1-format">(PDF)</span> from the original on 4 August 2018<span class="reference-accessdate">. Retrieved <span class="nowrap">3 April</span> 2022</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=unknown&amp;rft.jtitle=Argonne+National+Laboratory&amp;rft.atitle=Data+collection+handbook+to+support+modeling+impacts+of+radioactive+material+in+soil+and+building+structures&amp;rft.pages=13-21&amp;rft.date=2015&amp;rft.aulast=Yu&amp;rft.aufirst=Charley&amp;rft.au=Kamboj%2C+Sunita&amp;rft.au=Wang%2C+Cheng&amp;rft.au=Cheng%2C+Jing-Jy&amp;rft_id=https%3A%2F%2Fresrad.evs.anl.gov%2Fdocs%2Fdata_collection.pdf&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-Buol-8"><span class="mw-cite-backlink">^ <a href="#cite_ref-Buol_8-0"><sup><i><b>a</b></i></sup></a> <a href="#cite_ref-Buol_8-1"><sup><i><b>b</b></i></sup></a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFBuolSouthardGrahamMcDaniel2011" class="citation book cs1">Buol, Stanley W.; Southard, Randal J.; Graham, Robert C.; McDaniel, Paul A. (2011). <a rel="nofollow" class="external text" href="https://web.archive.org/web/20230422182641/https://fr1lib.org/book/2156097/707d35"><i>Soil genesis and classification</i></a> (6th&#160;ed.). Ames, Iowa: <a href="/wiki/Wiley-Blackwell" title="Wiley-Blackwell">Wiley-Blackwell</a>. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/978-0-470-96060-8" title="Special:BookSources/978-0-470-96060-8"><bdi>978-0-470-96060-8</bdi></a>. Archived from <a rel="nofollow" class="external text" href="https://fr1lib.org/book/2156097/707d35">the original</a> on 22 April 2023<span class="reference-accessdate">. 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(2016). <a rel="nofollow" class="external text" href="https://cpb-us-e1.wpmucdn.com/blogs.uoregon.edu/dist/d/3735/files/2013/07/Retallack-et-al.-2016-Farrel-1gt7uft.pdf">"Archean coastal-plain paleosols and life on land"</a> <span class="cs1-format">(PDF)</span>. <i><a href="/wiki/Gondwana_Research" title="Gondwana Research">Gondwana Research</a></i>. <b>40</b>: 1–20. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2016GondR..40....1R">2016GondR..40....1R</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<span class="id-lock-free" title="Freely accessible"><a rel="nofollow" class="external text" href="https://doi.org/10.1016%2Fj.gr.2016.08.003">10.1016/j.gr.2016.08.003</a></span>. <a rel="nofollow" class="external text" href="https://web.archive.org/web/20181113075710/https://cpb-us-e1.wpmucdn.com/blogs.uoregon.edu/dist/d/3735/files/2013/07/Retallack-et-al.-2016-Farrel-1gt7uft.pdf">Archived</a> <span class="cs1-format">(PDF)</span> from the original on 13 November 2018<span class="reference-accessdate">. Retrieved <span class="nowrap">3 April</span> 2022</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=article&amp;rft.jtitle=Gondwana+Research&amp;rft.atitle=Archean+coastal-plain+paleosols+and+life+on+land&amp;rft.volume=40&amp;rft.pages=1-20&amp;rft.date=2016&amp;rft_id=info%3Adoi%2F10.1016%2Fj.gr.2016.08.003&amp;rft_id=info%3Abibcode%2F2016GondR..40....1R&amp;rft.aulast=Retallack&amp;rft.aufirst=Gregory+J.&amp;rft.au=Krinsley%2C+David+H.&amp;rft.au=Fischer%2C+Robert&amp;rft.au=Razink%2C+Joshua+J.&amp;rft.au=Langworthy%2C+Kurt+A.&amp;rft_id=https%3A%2F%2Fcpb-us-e1.wpmucdn.com%2Fblogs.uoregon.edu%2Fdist%2Fd%2F3735%2Ffiles%2F2013%2F07%2FRetallack-et-al.-2016-Farrel-1gt7uft.pdf&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-ches-10"><span class="mw-cite-backlink"><b><a href="#cite_ref-ches_10-0">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFChesworth2008" class="citation book cs1">Chesworth, Ward, ed. (2008). <a rel="nofollow" class="external text" href="https://fr1lib.org/book/563235/8e916e"><i>Encyclopedia of soil science</i></a> (1st&#160;ed.). Dordrecht, The Netherlands: <a href="/wiki/Springer_Science%2BBusiness_Media" title="Springer Science+Business Media">Springer</a>. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/978-1-4020-3994-2" title="Special:BookSources/978-1-4020-3994-2"><bdi>978-1-4020-3994-2</bdi></a>. <a rel="nofollow" class="external text" href="https://web.archive.org/web/20180905002957/http://www.encyclopedias.biz/dw/Encyclopedia%20of%20Soil%20Science.pdf">Archived</a> <span class="cs1-format">(PDF)</span> from the original on 5 September 2018<span class="reference-accessdate">. Retrieved <span class="nowrap">27 March</span> 2022</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Encyclopedia+of+soil+science&amp;rft.place=Dordrecht%2C+The+Netherlands&amp;rft.edition=1st&amp;rft.pub=Springer&amp;rft.date=2008&amp;rft.isbn=978-1-4020-3994-2&amp;rft_id=https%3A%2F%2Ffr1lib.org%2Fbook%2F563235%2F8e916e&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-11"><span class="mw-cite-backlink"><b><a href="#cite_ref-11">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite class="citation web cs1"><a rel="nofollow" class="external text" href="https://sis.agr.gc.ca/cansis/glossary/e/index.html">"Glossary of terms in soil science"</a>. <i><a href="/wiki/Agriculture_and_Agri-Food_Canada" title="Agriculture and Agri-Food Canada">Agriculture and Agri-Food Canada</a></i>. 13 December 2013. <a rel="nofollow" class="external text" href="https://web.archive.org/web/20181027045042/http://sis.agr.gc.ca/cansis/glossary/e/index.html">Archived</a> from the original on 27 October 2018<span class="reference-accessdate">. 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Hoboken, New Jersey: <a href="/wiki/Wiley-Blackwell" title="Wiley-Blackwell">Wiley-Blackwell</a>. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/9781405197700" title="Special:BookSources/9781405197700"><bdi>9781405197700</bdi></a>. Archived from <a rel="nofollow" class="external text" href="https://fr.book4you.org/book/2156095/fd863f">the original</a> on 22 April 2023<span class="reference-accessdate">. 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Archived from <a rel="nofollow" class="external text" href="https://www.waterboards.ca.gov/centralvalley/water_issues/basin_plans/ph_turbidity/ph_turbidity_04phreq.pdf">the original</a> <span class="cs1-format">(PDF)</span> on 8 May 2021<span class="reference-accessdate">. Retrieved <span class="nowrap">6 June</span> 2021</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=unknown&amp;rft.btitle=pH+requirements+of+freshwater+aquatic+life&amp;rft.aulast=Robertson&amp;rft.aufirst=Bryan&amp;rft_id=https%3A%2F%2Fwww.waterboards.ca.gov%2Fcentralvalley%2Fwater_issues%2Fbasin_plans%2Fph_turbidity%2Fph_turbidity_04phreq.pdf&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-115"><span class="mw-cite-backlink"><b><a href="#cite_ref-115">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFChang2010" class="citation book cs1">Chang, Raymond, ed. (2010). <a rel="nofollow" class="external text" href="https://www.academia.edu/44394574"><i>Chemistry</i></a> (12th&#160;ed.). 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Retrieved <span class="nowrap">21 June</span> 2021</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=bookitem&amp;rft.atitle=Soil+Acidity+and+its+Relations+to+Acid+Deposition&amp;rft.btitle=Effects+of+Accumulation+of+Air+Pollutants+in+Forest+Ecosystems&amp;rft.place=Dordrecht%2C+The+Netherlands&amp;rft.pages=127-146&amp;rft.edition=1st&amp;rft.pub=D.+Reidel+Publishing+Company&amp;rft.date=1983&amp;rft_id=info%3Adoi%2F10.1007%2F978-94-009-6983-4_10&amp;rft.isbn=978-94-009-6985-8&amp;rft.aulast=Ulrich&amp;rft.aufirst=Bernhard&amp;rft_id=https%3A%2F%2Frd.springer.com%2Fcontent%2Fpdf%2F10.1007%252F978-94-009-6983-4_10.pdf&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-FOOTNOTEDonahueMillerShickluna1977120–121-136"><span class="mw-cite-backlink"><b><a href="#cite_ref-FOOTNOTEDonahueMillerShickluna1977120–121_136-0">^</a></b></span> <span class="reference-text"><a href="#CITEREFDonahueMillerShickluna1977">Donahue, Miller &amp; Shickluna 1977</a>, pp.&#160;120–121.</span> </li> <li id="cite_note-FOOTNOTEDonahueMillerShickluna1977125-137"><span class="mw-cite-backlink"><b><a href="#cite_ref-FOOTNOTEDonahueMillerShickluna1977125_137-0">^</a></b></span> <span class="reference-text"><a href="#CITEREFDonahueMillerShickluna1977">Donahue, Miller &amp; Shickluna 1977</a>, p.&#160;125.</span> </li> <li id="cite_note-FOOTNOTEDean195780-138"><span class="mw-cite-backlink"><b><a href="#cite_ref-FOOTNOTEDean195780_138-0">^</a></b></span> <span class="reference-text"><a href="#CITEREFDean1957">Dean 1957</a>, p.&#160;80.</span> </li> <li id="cite_note-FOOTNOTERussel1957123–125-139"><span class="mw-cite-backlink"><b><a href="#cite_ref-FOOTNOTERussel1957123–125_139-0">^</a></b></span> <span class="reference-text"><a href="#CITEREFRussel1957">Russel 1957</a>, pp.&#160;123–125.</span> </li> <li id="cite_note-BradyWeil-140"><span class="mw-cite-backlink">^ <a href="#cite_ref-BradyWeil_140-0"><sup><i><b>a</b></i></sup></a> <a href="#cite_ref-BradyWeil_140-1"><sup><i><b>b</b></i></sup></a></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFWeilBrady2016" class="citation book cs1">Weil, Ray R.; Brady, Nyle C. 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Retrieved <span class="nowrap">19 September</span> 2021</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=article&amp;rft.jtitle=Comptes+Rendus+Hebdomadaires+des+S%C3%A9ances+de+l%27Acad%C3%A9mie+des+Sciences&amp;rft.atitle=Sur+les+organismes+de+la+nitrification&amp;rft.volume=110&amp;rft.issue=1&amp;rft.pages=1013-1016&amp;rft.date=1890&amp;rft.aulast=Winogradsky&amp;rft.aufirst=Sergei&amp;rft_id=https%3A%2F%2Fgallica.bnf.fr%2Fark%3A%2F12148%2Fbpt6k30663%2Ff1087%3Flang%3DEN&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-FOOTNOTEKellogg19571–4-275"><span class="mw-cite-backlink"><b><a href="#cite_ref-FOOTNOTEKellogg19571–4_275-0">^</a></b></span> <span class="reference-text"><a href="#CITEREFKellogg1957">Kellogg 1957</a>, pp.&#160;1–4.</span> </li> <li id="cite_note-276"><span class="mw-cite-backlink"><b><a href="#cite_ref-276">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFHilgard1907" class="citation book cs1">Hilgard, Eugene W. (1907). <a rel="nofollow" class="external text" href="https://www.biodiversitylibrary.org/bibliography/24461"><i>Soils: their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions</i></a>. London, United Kingdom: <a href="/wiki/The_Macmillan_Company" class="mw-redirect" title="The Macmillan Company">The Macmillan Company</a><span class="reference-accessdate">. Retrieved <span class="nowrap">19 September</span> 2021</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Soils%3A+their+formation%2C+properties%2C+composition%2C+and+relations+to+climate+and+plant+growth+in+the+humid+and+arid+regions&amp;rft.place=London%2C+United+Kingdom&amp;rft.pub=The+Macmillan+Company&amp;rft.date=1907&amp;rft.aulast=Hilgard&amp;rft.aufirst=Eugene+W.&amp;rft_id=https%3A%2F%2Fwww.biodiversitylibrary.org%2Fbibliography%2F24461&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-277"><span class="mw-cite-backlink"><b><a href="#cite_ref-277">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFFallou1857" class="citation book cs1 cs1-prop-foreign-lang-source">Fallou, Friedrich Albert (1857). <a rel="nofollow" class="external text" href="https://web.archive.org/web/20181215223343/http://digital.slub-dresden.de/fileadmin/data/321768043/321768043_tif/jpegs/321768043.pdf"><i>Anfangsgründe der Bodenkunde</i></a> <span class="cs1-format">(PDF)</span> (in German). Dresden, Germany: G. Schönfeld's Buchhandlung. Archived from <a rel="nofollow" class="external text" href="http://digital.slub-dresden.de/fileadmin/data/321768043/321768043_tif/jpegs/321768043.pdf">the original</a> <span class="cs1-format">(PDF)</span> on 15 December 2018<span class="reference-accessdate">. Retrieved <span class="nowrap">15 December</span> 2018</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Anfangsgr%C3%BCnde+der+Bodenkunde&amp;rft.place=Dresden%2C+Germany&amp;rft.pub=G.+Sch%C3%B6nfeld%27s+Buchhandlung&amp;rft.date=1857&amp;rft.aulast=Fallou&amp;rft.aufirst=Friedrich+Albert&amp;rft_id=http%3A%2F%2Fdigital.slub-dresden.de%2Ffileadmin%2Fdata%2F321768043%2F321768043_tif%2Fjpegs%2F321768043.pdf&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-278"><span class="mw-cite-backlink"><b><a href="#cite_ref-278">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFGlinka1914" class="citation book cs1 cs1-prop-foreign-lang-source">Glinka, Konstantin Dmitrievich (1914). <i>Die Typen der Bodenbildung: ihre Klassifikation und geographische Verbreitung</i> (in German). Berlin, Germany: <a href="/wiki/Borntraeger" class="mw-redirect" title="Borntraeger">Borntraeger</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Die+Typen+der+Bodenbildung%3A+ihre+Klassifikation+und+geographische+Verbreitung&amp;rft.place=Berlin%2C+Germany&amp;rft.pub=Borntraeger&amp;rft.date=1914&amp;rft.aulast=Glinka&amp;rft.aufirst=Konstantin+Dmitrievich&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> <li id="cite_note-279"><span class="mw-cite-backlink"><b><a href="#cite_ref-279">^</a></b></span> <span class="reference-text"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFGlinka1927" class="citation book cs1">Glinka, Konstantin Dmitrievich (1927). <a rel="nofollow" class="external text" href="http://reader.library.cornell.edu/docviewer/digital?id=chla3055800#mode/1up"><i>The great soil groups of the world and their development</i></a>. Ann Arbor, Michigan: Edwards Brothers<span class="reference-accessdate">. Retrieved <span class="nowrap">19 September</span> 2021</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=The+great+soil+groups+of+the+world+and+their+development&amp;rft.place=Ann+Arbor%2C+Michigan&amp;rft.pub=Edwards+Brothers&amp;rft.date=1927&amp;rft.aulast=Glinka&amp;rft.aufirst=Konstantin+Dmitrievich&amp;rft_id=http%3A%2F%2Freader.library.cornell.edu%2Fdocviewer%2Fdigital%3Fid%3Dchla3055800%23mode%2F1up&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></span> </li> </ol></div></div> <div class="mw-heading mw-heading2"><h2 id="Sources">Sources</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=37" title="Edit section: Sources"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Definition_of_Free_Cultural_Works_logo_notext.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/78/Definition_of_Free_Cultural_Works_logo_notext.svg/12px-Definition_of_Free_Cultural_Works_logo_notext.svg.png" decoding="async" width="12" height="12" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/78/Definition_of_Free_Cultural_Works_logo_notext.svg/18px-Definition_of_Free_Cultural_Works_logo_notext.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/78/Definition_of_Free_Cultural_Works_logo_notext.svg/24px-Definition_of_Free_Cultural_Works_logo_notext.svg.png 2x" data-file-width="219" data-file-height="218" /></a></span>&#160;This article incorporates text from a <a href="/wiki/Free_content" title="Free content">free content</a> work.&#32;Licensed under Cc BY-SA 3.0 IGO&#32;(<a class="external text" href="https://commons.wikimedia.org/wiki/File:United_Nations_Environment_Programme_Drowning_in_Plastics_%E2%80%93_Marine_Litter_and_Plastic_Waste_Vital_Graphics.pdf">license statement/permission</a>).&#32;Text taken from <a rel="nofollow" class="external text" href="https://www.unep.org/resources/report/drowning-plastics-marine-litter-and-plastic-waste-vital-graphics"><i>Drowning in Plastics – Marine Litter and Plastic Waste Vital Graphics&#8203;</i></a>,&#32;United Nations Environment Programme. </p> <div class="mw-heading mw-heading2"><h2 id="Bibliography">Bibliography</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=38" title="Edit section: Bibliography"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1239549316">.mw-parser-output .refbegin{margin-bottom:0.5em}.mw-parser-output .refbegin-hanging-indents>ul{margin-left:0}.mw-parser-output .refbegin-hanging-indents>ul>li{margin-left:0;padding-left:3.2em;text-indent:-3.2em}.mw-parser-output .refbegin-hanging-indents ul,.mw-parser-output .refbegin-hanging-indents ul li{list-style:none}@media(max-width:720px){.mw-parser-output .refbegin-hanging-indents>ul>li{padding-left:1.6em;text-indent:-1.6em}}.mw-parser-output .refbegin-columns{margin-top:0.3em}.mw-parser-output .refbegin-columns ul{margin-top:0}.mw-parser-output .refbegin-columns li{page-break-inside:avoid;break-inside:avoid-column}@media screen{.mw-parser-output .refbegin{font-size:90%}}</style><div class="refbegin" style=""> <ul><li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFDonahueMillerShickluna1977" class="citation book cs1">Donahue, Roy Luther; Miller, Raymond W.; Shickluna, John C. (1977). <a rel="nofollow" class="external text" href="https://archive.org/details/soilsintroductio00dona"><i>Soils: An Introduction to Soils and Plant Growth</i></a>. <a href="/wiki/Prentice-Hall" class="mw-redirect" title="Prentice-Hall">Prentice-Hall</a>. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/978-0-13-821918-5" title="Special:BookSources/978-0-13-821918-5"><bdi>978-0-13-821918-5</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Soils%3A+An+Introduction+to+Soils+and+Plant+Growth&amp;rft.pub=Prentice-Hall&amp;rft.date=1977&amp;rft.isbn=978-0-13-821918-5&amp;rft.aulast=Donahue&amp;rft.aufirst=Roy+Luther&amp;rft.au=Miller%2C+Raymond+W.&amp;rft.au=Shickluna%2C+John+C.&amp;rft_id=https%3A%2F%2Farchive.org%2Fdetails%2Fsoilsintroductio00dona&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite class="citation web cs1"><a rel="nofollow" class="external text" href="http://ag.arizona.edu/pubs/garden/mg/soils/soils.html">"Arizona Master Gardener"</a>. Cooperative Extension, College of Agriculture, <a href="/wiki/University_of_Arizona" title="University of Arizona">University of Arizona</a><span class="reference-accessdate">. Retrieved <span class="nowrap">27 May</span> 2013</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=unknown&amp;rft.btitle=Arizona+Master+Gardener&amp;rft.pub=Cooperative+Extension%2C+College+of+Agriculture%2C+University+of+Arizona&amp;rft_id=http%3A%2F%2Fag.arizona.edu%2Fpubs%2Fgarden%2Fmg%2Fsoils%2Fsoils.html&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFStefferud1957" class="citation book cs1">Stefferud, Alfred, ed. (1957). <a rel="nofollow" class="external text" href="https://archive.org/stream/yoa1957#page/n18/mode/1up"><i>Soil: The Yearbook of Agriculture 1957</i></a>. United States Department of Agriculture. <a href="/wiki/OCLC_(identifier)" class="mw-redirect" title="OCLC (identifier)">OCLC</a>&#160;<a rel="nofollow" class="external text" href="https://search.worldcat.org/oclc/704186906">704186906</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=book&amp;rft.btitle=Soil%3A+The+Yearbook+of+Agriculture+1957&amp;rft.pub=United+States+Department+of+Agriculture&amp;rft.date=1957&amp;rft_id=info%3Aoclcnum%2F704186906&amp;rft_id=https%3A%2F%2Farchive.org%2Fstream%2Fyoa1957%23page%2Fn18%2Fmode%2F1up&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span> <ul><li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><span id="CITEREFKellogg1957" class="citation">Kellogg. "<a rel="nofollow" class="external text" href="//archive.org/stream/yoa1957#page/n17/mode/1up">We Seek; We Learn</a>". In <a href="#CITEREFStefferud1957">Stefferud (1957)</a>.</span></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><span id="CITEREFSimonson1957" class="citation">Simonson. "<a rel="nofollow" class="external text" href="//archive.org/stream/yoa1957#page/n34/mode/1up">What Soils Are</a>". In <a href="#CITEREFStefferud1957">Stefferud (1957)</a>.</span></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><span id="CITEREFRussell1957" class="citation">Russell. "<a rel="nofollow" class="external text" href="//archive.org/stream/yoa1957#page/n49/mode/1up">Physical Properties</a>". In <a href="#CITEREFStefferud1957">Stefferud (1957)</a>.</span></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><span id="CITEREFDean1957" class="citation">Dean. "<a rel="nofollow" class="external text" href="//archive.org/stream/yoa1957#page/n100/mode/1up">Plant Nutrition and Soil Fertility</a>". In <a href="#CITEREFStefferud1957">Stefferud (1957)</a>.</span></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><span id="CITEREFRussel1957" class="citation">Russel. "<a rel="nofollow" class="external text" href="//archive.org/stream/yoa1957#page/n145/mode/1up">Boron and Soil Fertility</a>". In <a href="#CITEREFStefferud1957">Stefferud (1957)</a>.</span></li></ul></li></ul> </div> <div class="mw-heading mw-heading2"><h2 id="Further_reading">Further reading</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=39" title="Edit section: Further reading"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1239549316"><div class="refbegin refbegin-columns references-column-width" style="column-width: 33em"> <ul><li><a rel="nofollow" class="external text" href="http://www.soil-net.com/">Soil-Net.com</a> <a rel="nofollow" class="external text" href="https://web.archive.org/web/20080710061716/http://www.soil-net.com/">Archived</a> 10 July 2008 at the <a href="/wiki/Wayback_Machine" title="Wayback Machine">Wayback Machine</a> A free schools-age educational site teaching about soil and its importance.</li> <li>Adams, J.A. 1986. <i>Dirt</i>. College Station, Texas: Texas A&amp;M University Press <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/0-89096-301-0" title="Special:BookSources/0-89096-301-0">0-89096-301-0</a></li> <li>Certini, G., Scalenghe, R. 2006. Soils: Basic concepts and future challenges. Cambridge Univ Press, Cambridge.</li> <li><a href="/wiki/David_R._Montgomery" title="David R. Montgomery">Montgomery, David R.</a>, <i>Dirt: The Erosion of Civilizations</i> (U of California Press, 2007), <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/978-0-520-25806-8" title="Special:BookSources/978-0-520-25806-8">978-0-520-25806-8</a></li> <li>Faulkner, Edward H. <i>Plowman's Folly</i> (New York, Grosset &amp; Dunlap, 1943). <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/0-933280-51-3" title="Special:BookSources/0-933280-51-3">0-933280-51-3</a></li> <li><a rel="nofollow" class="external text" href="https://web.archive.org/web/20080705133103/http://www.landis.org.uk/soilscapes">LandIS Free Soilscapes Viewer</a> Free interactive viewer for the Soils of England and Wales</li> <li>Jenny, Hans. 1941. <a rel="nofollow" class="external text" href="https://web.archive.org/web/20130225050838/http://soilandhealth.org/01aglibrary/010159.Jenny.pdf">Factors of Soil Formation: A System of Quantitative Pedology</a></li> <li>Logan, W.B. <i>Dirt: The ecstatic skin of the earth</i> (1995). <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a>&#160;<a href="/wiki/Special:BookSources/1-57322-004-3" title="Special:BookSources/1-57322-004-3">1-57322-004-3</a></li> <li>Mann, Charles C. September 2008. " Our good earth" <i>National Geographic Magazine</i></li></ul> <div class="mw-heading mw-heading2"><h2 id="External_links">External links</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Soil&amp;action=edit&amp;section=40" title="Edit section: External links"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <ul><li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite class="citation web cs1"><a rel="nofollow" class="external text" href="https://web.archive.org/web/20080624040143/http://www.mvm.usace.army.mil/Readiness/97flood/flood.htm">"97 Flood"</a>. USGS. Archived from <a rel="nofollow" class="external text" href="http://www.mvm.usace.army.mil/Readiness/97flood/flood.htm">the original</a> on 24 June 2008<span class="reference-accessdate">. Retrieved <span class="nowrap">8 July</span> 2008</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&amp;rft.genre=unknown&amp;rft.btitle=97+Flood&amp;rft.pub=USGS&amp;rft_id=http%3A%2F%2Fwww.mvm.usace.army.mil%2FReadiness%2F97flood%2Fflood.htm&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span> Photographs of sand boils.</li> <li>Soil Survey Division Staff. 1999. <i>Soil survey manual</i>. Soil Conservation Service. U.S. Department of Agriculture Handbook 18.</li> <li>Soil Survey Staff. 1975. <i>Soil Taxonomy: A basic system of soil classification for making and interpreting soil surveys.</i> USDA-SCS Agric. Handb. 436. United States Government Printing Office, Washington, DC.</li> <li><a rel="nofollow" class="external text" href="https://web.archive.org/web/20060828063956/http://forages.oregonstate.edu/is/ssis/main.cfm?PageID=3">Soils (Matching suitable forage species to soil type)</a>, Oregon State University</li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222"><cite id="CITEREFGardiner" class="citation web cs1">Gardiner, Duane T. <a rel="nofollow" class="external text" href="https://web.archive.org/web/20180209052922/http://jan.ucc.nau.edu/~doetqp-p/courses/env320/lec1/Lec1.html">"Lecture 1 Chapter 1 Why Study Soils?"</a>. <i>ENV320: Soil Science Lecture Notes</i>. Texas A&amp;M University-Kingsville. Archived from <a rel="nofollow" class="external text" href="http://jan.ucc.nau.edu/~doetqp-p/courses/env320/lec1/Lec1.html">the original</a> on 9 February 2018<span class="reference-accessdate">. Retrieved <span class="nowrap">7 January</span> 2019</span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=unknown&amp;rft.jtitle=ENV320%3A+Soil+Science+Lecture+Notes&amp;rft.atitle=Lecture+1+Chapter+1+Why+Study+Soils%3F&amp;rft.aulast=Gardiner&amp;rft.aufirst=Duane+T&amp;rft_id=http%3A%2F%2Fjan.ucc.nau.edu%2F~doetqp-p%2Fcourses%2Fenv320%2Flec1%2FLec1.html&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ASoil" class="Z3988"></span></li> <li>Janick, Jules. 2002. <a rel="nofollow" class="external text" href="https://web.archive.org/web/20050317030248/http://www.hort.purdue.edu/newcrop/tropical/lecture_06/chapter_12l_R.html">Soil notes</a>, Purdue University</li> <li><a rel="nofollow" class="external text" href="http://www.landis.org.uk/">LandIS Soils Data for England and Wales</a> <a rel="nofollow" class="external text" href="https://web.archive.org/web/20070716033248/http://www.landis.org.uk/">Archived</a> 16 July 2007 at the <a href="/wiki/Wayback_Machine" title="Wayback Machine">Wayback Machine</a> a pay source for GIS data on the soils of England and Wales and soils data source; they charge a handling fee to researchers.</li></ul> </div> <style data-mw-deduplicate="TemplateStyles:r1235681985">.mw-parser-output .side-box{margin:4px 0;box-sizing:border-box;border:1px solid #aaa;font-size:88%;line-height:1.25em;background-color:var(--background-color-interactive-subtle,#f8f9fa);display:flow-root}.mw-parser-output .side-box-abovebelow,.mw-parser-output .side-box-text{padding:0.25em 0.9em}.mw-parser-output .side-box-image{padding:2px 0 2px 0.9em;text-align:center}.mw-parser-output .side-box-imageright{padding:2px 0.9em 2px 0;text-align:center}@media(min-width:500px){.mw-parser-output .side-box-flex{display:flex;align-items:center}.mw-parser-output .side-box-text{flex:1;min-width:0}}@media(min-width:720px){.mw-parser-output .side-box{width:238px}.mw-parser-output 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href="mw-data:TemplateStyles:r1235681985"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1237033735"><div class="side-box side-box-right plainlinks sistersitebox"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1126788409"> <div class="side-box-flex"> <div class="side-box-image"><span class="noviewer" typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/commons/thumb/d/df/Wikibooks-logo-en-noslogan.svg/40px-Wikibooks-logo-en-noslogan.svg.png" decoding="async" width="40" height="40" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/d/df/Wikibooks-logo-en-noslogan.svg/60px-Wikibooks-logo-en-noslogan.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/d/df/Wikibooks-logo-en-noslogan.svg/80px-Wikibooks-logo-en-noslogan.svg.png 2x" data-file-width="400" data-file-height="400" /></span></span></div> <div class="side-box-text plainlist">The Wikibook <i><a href="https://en.wikibooks.org/wiki/Historical_Geology" class="extiw" title="wikibooks:Historical Geology">Historical Geology</a></i> has a page on the topic of: <i><b><a href="https://en.wikibooks.org/wiki/Historical_Geology/Soils_and_paleosols" class="extiw" title="wikibooks:Historical Geology/Soils and paleosols">Soils and paleosols</a></b></i></div></div> </div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1235681985"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1237033735"><div class="side-box side-box-right plainlinks sistersitebox"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1126788409"> <div class="side-box-flex"> <div class="side-box-image"><span class="noviewer" typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/30px-Commons-logo.svg.png" decoding="async" width="30" height="40" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/45px-Commons-logo.svg.png 1.5x, //upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/59px-Commons-logo.svg.png 2x" data-file-width="1024" data-file-height="1376" /></span></span></div> <div class="side-box-text plainlist">Wikimedia Commons has media related to <span style="font-weight: bold; font-style: italic;"><a href="https://commons.wikimedia.org/wiki/Category:Soils" class="extiw" title="commons:Category:Soils">Soils</a></span>.</div></div> </div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1235681985"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1237033735"><div class="side-box side-box-right plainlinks sistersitebox"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1126788409"> <div class="side-box-flex"> <div class="side-box-image"><span class="noviewer" typeof="mw:File"><span><img alt="" src="//upload.wikimedia.org/wikipedia/commons/thumb/f/fa/Wikiquote-logo.svg/34px-Wikiquote-logo.svg.png" decoding="async" width="34" height="40" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/f/fa/Wikiquote-logo.svg/51px-Wikiquote-logo.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/f/fa/Wikiquote-logo.svg/68px-Wikiquote-logo.svg.png 2x" data-file-width="300" data-file-height="355" /></span></span></div> <div class="side-box-text plainlist">Wikiquote has quotations related to <i><b><a href="https://en.wikiquote.org/wiki/Special:Search/Soil" class="extiw" title="q:Special:Search/Soil">Soil</a></b></i>.</div></div> </div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1184024115"><div class="div-col"> <ul><li><a rel="nofollow" class="external text" href="https://www.theguardian.com/environment/video/2019/jul/11/its-time-we-stopped-treating-soil-like-dirt-video">Short video explaining soil basics</a></li> <li><a rel="nofollow" class="external text" href="http://www.edaphic.com.au/soil-water-compendium/">The Soil Water Compendium (soil water content sensors explained)</a></li> <li><a rel="nofollow" class="external text" href="http://www.fao.org/globalsoilpartnership/en/">Global Soil Partnership</a></li> <li><a rel="nofollow" class="external text" href="http://www.fao.org/soils-portal/en/">FAO Soils Portal</a></li> <li><a rel="nofollow" class="external text" href="https://wrb.isric.org/">World Reference Base for Soil Resources</a></li> <li><a rel="nofollow" class="external text" href="https://www.isric.org/">ISRIC – World Soil Information (ISC World Data Centre for Soils)</a></li> <li><a rel="nofollow" class="external text" href="https://www.isric.org/explore/library">ISRIC -World Soil Library and Maps</a></li> <li><a rel="nofollow" class="external text" href="https://wsm.isric.org/">ISRIC - World Soil Museum (WSM virtual)</a></li> <li><a rel="nofollow" class="external text" href="https://data.isric.org/">ISRIC - Soil data hub</a></li> <li><a rel="nofollow" class="external text" href="http://www.wossac.com/">Wossac the world soil survey archive and catalogue</a></li> <li><a rel="nofollow" class="external text" href="http://csss.ca/">Canadian Society of Soil Science</a></li> <li><a rel="nofollow" class="external text" href="https://www.soils.org/">Soil Science Society of America</a></li> <li><a rel="nofollow" class="external text" href="https://websoilsurvey.nrcs.usda.gov/app/HomePage.htm">USDA-NRCS Web Soil Survey</a></li> <li><a rel="nofollow" class="external text" href="http://eusoils.jrc.ec.europa.eu/">European Soil Portal</a> (wiki)</li> <li><a rel="nofollow" class="external text" href="http://www.cranfield.ac.uk/sas/nsri">National Soil Resources Institute UK</a></li> <li><a rel="nofollow" class="external text" href="http://passel.unl.edu/">Plant and Soil Sciences eLibrary</a></li> <li><a rel="nofollow" class="external text" href="https://archive.org/details/yoa1957">Copies of the reference 'Soil: The Yearbook of Agriculture 1957' in multiple formats</a></li></ul></div> <p class="mw-empty-elt"> </p> <div class="navbox-styles"><style data-mw-deduplicate="TemplateStyles:r1129693374">.mw-parser-output .hlist dl,.mw-parser-output .hlist ol,.mw-parser-output .hlist ul{margin:0;padding:0}.mw-parser-output .hlist dd,.mw-parser-output .hlist dt,.mw-parser-output .hlist li{margin:0;display:inline}.mw-parser-output .hlist.inline,.mw-parser-output .hlist.inline dl,.mw-parser-output .hlist.inline ol,.mw-parser-output .hlist.inline ul,.mw-parser-output .hlist dl dl,.mw-parser-output .hlist dl ol,.mw-parser-output .hlist dl ul,.mw-parser-output .hlist ol dl,.mw-parser-output .hlist ol ol,.mw-parser-output .hlist ol ul,.mw-parser-output .hlist ul dl,.mw-parser-output .hlist ul ol,.mw-parser-output .hlist ul ul{display:inline}.mw-parser-output .hlist .mw-empty-li{display:none}.mw-parser-output .hlist dt::after{content:": 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title="Pedology">Pedology</a></li> <li><a href="/wiki/Edaphology" title="Edaphology">Edaphology</a></li> <li><a href="/wiki/Soil_biology" title="Soil biology">Soil biology</a></li> <li><a href="/wiki/Soil_microbiology" title="Soil microbiology">Soil microbiology</a></li> <li><a href="/wiki/Soil_zoology" title="Soil zoology">Soil zoology</a></li> <li><a href="/wiki/Soil_ecology" title="Soil ecology">Soil ecology</a></li> <li><a href="/wiki/Soil_physics" title="Soil physics">Soil physics</a></li> <li><a href="/wiki/Soil_mechanics" title="Soil mechanics">Soil mechanics</a></li> <li><a href="/wiki/Soil_chemistry" title="Soil chemistry">Soil chemistry</a></li> <li><a href="/wiki/Environmental_soil_science" title="Environmental soil science">Environmental soil science</a></li> <li><a href="/wiki/Agricultural_soil_science" title="Agricultural soil science">Agricultural soil science</a></li></ul> </div></td><td class="noviewer navbox-image" rowspan="8" style="width:1px;padding:0 0 0 2px"><div><span class="mw-image-border" typeof="mw:File"><a href="/wiki/File:Soil_profile.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/b/b8/Soil_profile.svg/110px-Soil_profile.svg.png" decoding="async" width="110" height="159" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/b/b8/Soil_profile.svg/165px-Soil_profile.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/b/b8/Soil_profile.svg/220px-Soil_profile.svg.png 2x" data-file-width="456" data-file-height="660" /></a></span></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Soil topics</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a class="mw-selflink selflink">Soil</a></li> <li><a href="/wiki/Pedosphere" title="Pedosphere">Pedosphere</a> <ul><li><a href="/wiki/Soil_morphology" title="Soil morphology">Soil morphology</a></li> <li><a href="/wiki/Pedodiversity" title="Pedodiversity">Pedodiversity</a></li> <li><a href="/wiki/Soil_formation" title="Soil formation">Soil formation</a></li></ul></li> <li><a href="/wiki/Soil_erosion" title="Soil erosion">Soil erosion</a></li> <li><a href="/wiki/Soil_contamination" title="Soil contamination">Soil contamination</a></li> <li><a href="/wiki/Soil_retrogression_and_degradation" title="Soil retrogression and degradation">Soil retrogression and degradation</a></li> <li><a href="/wiki/Soil_compaction" title="Soil compaction">Soil compaction</a> <ul><li><a href="/wiki/Soil_compaction_(agriculture)" title="Soil compaction (agriculture)">Soil compaction (agriculture)</a></li></ul></li> <li><a href="/wiki/Soil_sealing" title="Soil sealing">Soil sealing</a></li> <li><a href="/wiki/Soil_salinity" title="Soil salinity">Soil salinity</a> <ul><li><a href="/wiki/Alkali_soil" title="Alkali soil">Alkali soil</a></li></ul></li> <li><a href="/wiki/Soil_pH" title="Soil pH">Soil pH</a> <ul><li><a href="/wiki/Soil_acidification" title="Soil acidification">Soil acidification</a></li></ul></li> <li><a href="/wiki/Soil_health" title="Soil health">Soil health</a></li> <li><a href="/wiki/Soil_life" class="mw-redirect" title="Soil life">Soil life</a></li> <li><a href="/wiki/Soil_biodiversity" title="Soil biodiversity">Soil biodiversity</a></li> <li><a href="/wiki/Soil_quality" title="Soil quality">Soil quality</a></li> <li><a href="/wiki/Soil_value" title="Soil value">Soil value</a></li> <li><a href="/wiki/Soil_fertility" title="Soil fertility">Soil fertility</a></li> <li><a href="/wiki/Soil_resilience" title="Soil resilience">Soil resilience</a></li> <li><a href="/wiki/Soil_color" title="Soil color">Soil color</a></li> <li><a href="/wiki/Soil_texture" title="Soil texture">Soil texture</a></li> <li><a href="/wiki/Soil_structure" title="Soil structure">Soil structure</a> <ul><li><a href="/wiki/Pore_space_in_soil" title="Pore space in soil">Pore space in soil</a></li> <li><a href="/wiki/Pore_water_pressure" title="Pore water pressure">Pore water pressure</a></li></ul></li> <li><a href="/wiki/Soil_crust" title="Soil crust">Soil crust</a></li> <li><a href="/wiki/Soil_horizon" title="Soil horizon">Soil horizon</a></li> <li><a href="/wiki/Soil_biomantle" title="Soil biomantle">Soil biomantle</a></li> <li><a href="/wiki/Soil_carbon" title="Soil carbon">Soil carbon</a></li> <li><a href="/wiki/Soil_gas" title="Soil gas">Soil gas</a> <ul><li><a href="/wiki/Soil_respiration" title="Soil respiration">Soil respiration</a></li></ul></li> <li><a href="/wiki/Soil_organic_matter" title="Soil organic matter">Soil organic matter</a></li> <li><a href="/wiki/Soil_moisture" title="Soil moisture">Soil moisture</a> <ul><li><a href="/wiki/Soil_water_(retention)" title="Soil water (retention)">Soil water (retention)</a></li></ul></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Soil_type" title="Soil type">Soil type</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"><div class="navbox-styles"></div><div role="navigation" class="navbox" aria-labelledby="Soil_classification" style="padding:3px"><table class="nowraplinks mw-collapsible autocollapse navbox-inner" style="border-spacing:0;background:transparent;color:inherit"><tbody><tr><th scope="col" class="navbox-title" colspan="2"><div class="navbar plainlinks hlist navbar-mini"><ul><li class="nv-view"><a href="/wiki/Template:Soil_type" title="Template:Soil type"><abbr title="View this template">v</abbr></a></li><li class="nv-talk"><a href="/wiki/Template_talk:Soil_type" title="Template talk:Soil type"><abbr title="Discuss this template">t</abbr></a></li><li class="nv-edit"><a href="/wiki/Special:EditPage/Template:Soil_type" title="Special:EditPage/Template:Soil type"><abbr title="Edit this template">e</abbr></a></li></ul></div><div id="Soil_classification" style="font-size:114%;margin:0 4em"><a href="/wiki/Soil_classification" title="Soil classification">Soil classification</a></div></th></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/World_Reference_Base_for_Soil_Resources" title="World Reference Base for Soil Resources">World Reference Base<br /> for Soil Resources</a> (1998–)</th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Acrisol" title="Acrisol">Acrisols</a></li> <li><a href="/wiki/Alisols" class="mw-redirect" title="Alisols">Alisols</a></li> <li><a href="/wiki/Andosol" title="Andosol">Andosols</a></li> <li><a href="/wiki/Anthrosol" title="Anthrosol">Anthrosols</a></li> <li><a href="/wiki/Psamment" title="Psamment">Arenosols</a></li> <li><a href="/wiki/Calcisol" title="Calcisol">Calcisols</a></li> <li><a href="/wiki/Cambisol" title="Cambisol">Cambisols</a></li> <li><a href="/wiki/Chernozem" title="Chernozem">Chernozem</a></li> <li><a href="/wiki/Cryosols" class="mw-redirect" title="Cryosols">Cryosols</a></li> <li><a href="/wiki/Durisol" title="Durisol">Durisols</a></li> <li><a href="/wiki/Ferralsols" class="mw-redirect" title="Ferralsols">Ferralsols</a></li> <li><a href="/wiki/Fluvisol" title="Fluvisol">Fluvisols</a></li> <li><a href="/wiki/Gleysol" title="Gleysol">Gleysols</a></li> <li><a href="/wiki/Gypsisols" class="mw-redirect" title="Gypsisols">Gypsisols</a></li> <li><a href="/wiki/Histosol" title="Histosol">Histosol</a></li> <li><a href="/wiki/Kastanozem" title="Kastanozem">Kastanozems</a></li> <li><a href="/wiki/Leptosol" title="Leptosol">Leptosols</a></li> <li><a href="/wiki/Lixisol" title="Lixisol">Lixisols</a></li> <li><a href="/wiki/Luvisol" title="Luvisol">Luvisols</a></li> <li><a href="/wiki/Nitisol" title="Nitisol">Nitisols</a></li> <li><a href="/wiki/Phaeozem" title="Phaeozem">Phaeozems</a></li> <li><a href="/wiki/Planosol" title="Planosol">Planosols</a></li> <li><a href="/wiki/Plinthosol" title="Plinthosol">Plinthosols</a></li> <li><a href="/wiki/Podzol" title="Podzol">Podzols</a></li> <li><a href="/wiki/Regosol" title="Regosol">Regosols</a></li> <li><a href="/wiki/Retisol" title="Retisol">Retisols</a></li> <li><a href="/wiki/Solonchak" title="Solonchak">Solonchaks</a></li> <li><a href="/wiki/Solonetz" title="Solonetz">Solonetz</a></li> <li><a href="/wiki/Stagnosol" title="Stagnosol">Stagnosol</a></li> <li><a href="/wiki/Technosol" title="Technosol">Technosols</a></li> <li><a href="/wiki/Umbrisol" title="Umbrisol">Umbrisols</a></li> <li><a href="/wiki/Vertisol" title="Vertisol">Vertisols</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/USDA_soil_taxonomy" title="USDA soil taxonomy">USDA soil taxonomy</a></th><td class="navbox-list-with-group navbox-list navbox-even hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Alfisol" title="Alfisol">Alfisols</a></li> <li><a href="/wiki/Andisol" title="Andisol">Andisols</a></li> <li><a href="/wiki/Aridisol" title="Aridisol">Aridisols</a></li> <li><a href="/wiki/Entisol" title="Entisol">Entisols</a></li> <li><a href="/wiki/Gelisol" title="Gelisol">Gelisols</a></li> <li><a href="/wiki/Histosol" title="Histosol">Histosols</a></li> <li><a href="/wiki/Inceptisol" title="Inceptisol">Inceptisols</a></li> <li><a href="/wiki/Mollisol" title="Mollisol">Mollisols</a></li> <li><a href="/wiki/Oxisol" title="Oxisol">Oxisols</a></li> <li><a href="/wiki/Podzol" title="Podzol">Spodosols</a></li> <li><a href="/wiki/Ultisol" title="Ultisol">Ultisols</a></li> <li><a href="/wiki/Vertisol" title="Vertisol">Vertisols</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Other systems</th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/FAO_soil_classification" title="FAO soil classification">FAO soil classification</a> (1974–1998)</li> <li><a href="/wiki/Unified_Soil_Classification_System" title="Unified Soil Classification System">Unified Soil Classification System</a></li> <li><a href="/wiki/AASHTO_Soil_Classification_System" title="AASHTO Soil Classification System">AASHTO Soil Classification System</a></li> <li><a href="/wiki/R%C3%A9f%C3%A9rentiel_p%C3%A9dologique" title="Référentiel pédologique">Référentiel pédologique</a> (French classification system)</li> <li><a href="/wiki/Canadian_system_of_soil_classification" title="Canadian system of soil classification">Canadian system of soil classification</a></li> <li><a href="/wiki/Australian_Soil_Classification" title="Australian Soil Classification">Australian Soil Classification</a></li> <li><a href="/wiki/Polish_Soil_Classification" title="Polish Soil Classification">Polish Soil Classification</a></li> <li><a href="/wiki/1938_USDA_soil_taxonomy" title="1938 USDA soil taxonomy">1938 USDA soil taxonomy</a></li> <li><a href="/wiki/List_of_U.S._state_soils" title="List of U.S. state soils">List of U.S. state soils</a></li> <li><a href="/wiki/List_of_vineyard_soil_types" title="List of vineyard soil types">List of vineyard soil types</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Non-systematic soil types</th><td class="navbox-list-with-group navbox-list navbox-even hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Sand" title="Sand">Sand</a></li> <li><a href="/wiki/Silt" title="Silt">Silt</a></li> <li><a href="/wiki/Clay" title="Clay">Clay</a></li> <li><a href="/wiki/Loam" title="Loam">Loam</a></li> <li><a href="/wiki/Topsoil" title="Topsoil">Topsoil</a></li> <li><a href="/wiki/Subsoil" title="Subsoil">Subsoil</a></li> <li><a href="/wiki/Soil_crust" title="Soil crust">Soil crust</a></li> <li><a href="/wiki/Claypan" title="Claypan">Claypan</a></li> <li><a href="/wiki/Hardpan" title="Hardpan">Hardpan</a></li> <li><a href="/wiki/Gypcrust" title="Gypcrust">Gypcrust</a></li> <li><a href="/wiki/Caliche" title="Caliche">Caliche</a></li> <li><a href="/wiki/Parent_material" title="Parent material">Parent material</a></li> <li><a href="/wiki/Pedosphere" title="Pedosphere">Pedosphere</a></li> <li><a href="/wiki/Laimosphere" title="Laimosphere">Laimosphere</a></li> <li><a href="/wiki/Rhizosphere" title="Rhizosphere">Rhizosphere</a></li> <li><a href="/wiki/Bulk_soil" title="Bulk soil">Bulk soil</a></li> <li><a href="/wiki/Alkali_soil" title="Alkali soil">Alkali soil</a></li> <li><a href="/wiki/Bay_mud" title="Bay mud">Bay mud</a></li> <li><a href="/wiki/Blue_goo" title="Blue goo">Blue goo</a></li> <li><a href="/wiki/Brickearth" title="Brickearth">Brickearth</a></li> <li><a href="/wiki/Brown_earth" title="Brown earth">Brown earth</a></li> <li><a href="/wiki/Calcareous_grassland" title="Calcareous grassland">Calcareous grassland</a></li> <li><a href="/wiki/Dark_earth" title="Dark earth">Dark earth</a></li> <li><a href="/wiki/Dry_quicksand" title="Dry quicksand">Dry quicksand</a></li> <li><a href="/wiki/Duplex_soil" title="Duplex soil">Duplex soil</a></li> <li><a href="/wiki/Eluvium" title="Eluvium">Eluvium</a></li> <li><a href="/wiki/Expansive_clay" title="Expansive clay">Expansive clay</a></li> <li><a href="/wiki/Fill_dirt" title="Fill dirt">Fill dirt</a></li> <li><a href="/wiki/Fuller%27s_earth" title="Fuller&#39;s earth">Fuller's earth</a></li> <li><a href="/wiki/Hydrophobic_soil" title="Hydrophobic soil">Hydrophobic soil</a></li> <li><a href="/wiki/Loess" title="Loess">Loess</a></li> <li><a href="/wiki/Lunar_soil" class="mw-redirect" title="Lunar soil">Lunar soil</a></li> <li><a href="/wiki/Martian_soil" class="mw-redirect" title="Martian soil">Martian soil</a></li> <li><a href="/wiki/Mud" title="Mud">Mud</a></li> <li><a href="/wiki/Muskeg" title="Muskeg">Muskeg</a></li> <li><a href="/wiki/Paleosol" title="Paleosol">Paleosol</a></li> <li><a href="/wiki/Peat" title="Peat">Peat</a></li> <li><a href="/wiki/Prime_farmland" title="Prime farmland">Prime farmland</a></li> <li><a href="/wiki/Quicksand" title="Quicksand">Quicksand</a></li> <li><a href="/wiki/Serpentine_soil" title="Serpentine soil">Serpentine soil</a></li> <li><a href="/wiki/Spodic_soil" class="mw-redirect" title="Spodic soil">Spodic soil</a></li> <li><a href="/wiki/Stagnogley" title="Stagnogley">Stagnogley</a></li> <li><a href="/wiki/Subaqueous_soil" title="Subaqueous soil">Subaqueous soil</a></li> <li><a href="/wiki/Takir_(soil)" title="Takir (soil)">Takir</a></li> <li><a href="/wiki/Terra_preta" title="Terra preta">Terra preta</a></li> <li><a href="/wiki/Terra_rossa_(soil)" title="Terra rossa (soil)">Terra rossa</a></li> <li><a href="/wiki/Tropical_peat" title="Tropical peat">Tropical peat</a></li> <li><a href="/wiki/Yedoma" title="Yedoma">Yedoma</a></li></ul> </div></td></tr><tr><td class="navbox-abovebelow" colspan="2"><div><span class="noviewer" typeof="mw:File"><span title="Category"><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/9/96/Symbol_category_class.svg/16px-Symbol_category_class.svg.png" decoding="async" width="16" height="16" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/en/thumb/9/96/Symbol_category_class.svg/23px-Symbol_category_class.svg.png 1.5x, //upload.wikimedia.org/wikipedia/en/thumb/9/96/Symbol_category_class.svg/31px-Symbol_category_class.svg.png 2x" data-file-width="180" data-file-height="185" /></span></span> <a href="/wiki/Category:Types_of_soil" title="Category:Types of soil">Types of soil</a></div></td></tr></tbody></table></div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Applications</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Soil_conservation" title="Soil conservation">Soil conservation</a></li> <li><a href="/wiki/Soil_management" title="Soil management">Soil management</a></li> <li><a href="/wiki/Soil_guideline_value" title="Soil guideline value">Soil guideline value</a></li> <li><a href="/wiki/Soil_survey" title="Soil survey">Soil survey</a></li> <li><a href="/wiki/Soil_test" title="Soil test">Soil test</a></li> <li><a href="/wiki/Soil_governance" title="Soil governance">Soil governance</a></li> <li><a href="/wiki/Soil_value" title="Soil value">Soil value</a></li> <li><a href="/wiki/Soil_salinity_control" title="Soil salinity control">Soil salinity control</a></li> <li><a href="/wiki/Erosion_control" title="Erosion control">Erosion control</a></li> <li><a href="/wiki/Agroecology" title="Agroecology">Agroecology</a></li> <li><a href="/wiki/Liming_(soil)" title="Liming (soil)">Liming (soil)</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Related fields</th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Geology" title="Geology">Geology</a></li> <li><a href="/wiki/Geochemistry" title="Geochemistry">Geochemistry</a></li> <li><a href="/wiki/Petrology" title="Petrology">Petrology</a></li> <li><a href="/wiki/Geomorphology" title="Geomorphology">Geomorphology</a></li> <li><a href="/wiki/Geotechnical_engineering" title="Geotechnical engineering">Geotechnical engineering</a></li> <li><a href="/wiki/Hydrology" title="Hydrology">Hydrology</a></li> <li><a href="/wiki/Hydrogeology" title="Hydrogeology">Hydrogeology</a></li> <li><a href="/wiki/Biogeography" title="Biogeography">Biogeography</a></li> <li><a href="/wiki/Earth_materials" title="Earth materials">Earth materials</a></li> <li><a href="/wiki/Archaeology" title="Archaeology">Archaeology</a></li> <li><a href="/wiki/Agricultural_science" title="Agricultural science">Agricultural science</a> <ul><li><a href="/wiki/Agrology" class="mw-redirect" title="Agrology">Agrology</a></li></ul></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Societies, Initiatives</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Australian_Society_of_Soil_Science_Incorporated" title="Australian Society of Soil Science Incorporated">Australian Society of Soil Science Incorporated</a></li> <li><a href="/wiki/Canadian_Society_of_Soil_Science" title="Canadian Society of Soil Science">Canadian Society of Soil Science</a></li> <li><a href="/wiki/Central_Soil_Salinity_Research_Institute" title="Central Soil Salinity Research Institute">Central Soil Salinity Research Institute</a> (India)</li> <li><a href="/wiki/German_Soil_Science_Society" title="German Soil Science Society">German Soil Science Society</a></li> <li><a href="/wiki/Indian_Institute_of_Soil_Science" title="Indian Institute of Soil Science">Indian Institute of Soil Science</a></li> <li><a href="/wiki/International_Union_of_Soil_Sciences" title="International Union of Soil Sciences">International Union of Soil Sciences</a></li> <li><a href="/wiki/International_Year_of_Soil" title="International Year of Soil">International Year of Soil</a></li> <li><a href="/wiki/National_Society_of_Consulting_Soil_Scientists" title="National Society of Consulting Soil Scientists">National Society of Consulting Soil Scientists</a> (US)</li> <li><a href="/wiki/OPAL_Soil_Centre" title="OPAL Soil Centre">OPAL Soil Centre</a> (UK)</li> <li><a href="/wiki/Soil_Science_Society_of_Poland" title="Soil Science Society of Poland">Soil Science Society of Poland</a></li> <li><a href="/wiki/Soil_and_Water_Conservation_Society" title="Soil and Water Conservation Society">Soil and Water Conservation Society</a> (US)</li> <li><a href="/wiki/Soil_Science_Society_of_America" title="Soil Science Society of America">Soil Science Society of America</a></li> <li><a href="/wiki/World_Congress_of_Soil_Science" title="World Congress of Soil Science">World Congress of Soil Science</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Scientific journals</th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><i><a href="/wiki/Acta_Agriculturae_Scandinavica_B" title="Acta Agriculturae Scandinavica B">Acta Agriculturae Scandinavica B</a></i></li> <li><i><a href="/wiki/Journal_of_Soil_and_Water_Conservation" title="Journal of Soil and Water Conservation">Journal of Soil and Water Conservation</a></i></li> <li><i><a href="/wiki/Plant_and_Soil" title="Plant and Soil">Plant and Soil</a></i></li> <li><i><a href="/wiki/Pochvovedenie" title="Pochvovedenie">Pochvovedenie</a></i></li> <li><i><a href="/wiki/Soil_Research" title="Soil Research">Soil Research</a></i></li> <li><i><a href="/wiki/Soil_Science_Society_of_America_Journal" title="Soil Science Society of America Journal">Soil Science Society of America Journal</a></i></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">See also</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Land_use" title="Land use">Land use</a></li> <li><a href="/wiki/Land_conversion" class="mw-redirect" title="Land conversion">Land conversion</a></li> <li><a href="/wiki/Land_management" title="Land management">Land management</a></li> <li><a href="/wiki/Vegetation" title="Vegetation">Vegetation</a></li> <li><a href="/wiki/Infiltration_(hydrology)" title="Infiltration (hydrology)">Infiltration (hydrology)</a></li> <li><a href="/wiki/Groundwater" title="Groundwater">Groundwater</a></li> <li><a href="/wiki/Crust_(geology)" title="Crust (geology)">Crust (geology)</a></li> <li><a href="/wiki/Impervious_surface" title="Impervious surface">Impervious surface</a>/<a href="/wiki/Surface_runoff" title="Surface runoff">Surface runoff</a></li> <li><a href="/wiki/Petrichor" title="Petrichor">Petrichor</a></li></ul> </div></td></tr><tr><td class="navbox-abovebelow" colspan="3"><div> <ul><li><span class="noviewer" typeof="mw:File"><span title="Project page"><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/7/72/Symbol_project_class.svg/16px-Symbol_project_class.svg.png" decoding="async" width="16" height="16" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/en/thumb/7/72/Symbol_project_class.svg/23px-Symbol_project_class.svg.png 1.5x, //upload.wikimedia.org/wikipedia/en/thumb/7/72/Symbol_project_class.svg/31px-Symbol_project_class.svg.png 2x" data-file-width="180" data-file-height="185" /></span></span> <a href="/wiki/Wikipedia:WikiProject_Soil" title="Wikipedia:WikiProject Soil">Wikipedia:WikiProject Soil</a></li> <li>&#160;<span class="noviewer" typeof="mw:File"><span title="Category"><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/9/96/Symbol_category_class.svg/16px-Symbol_category_class.svg.png" decoding="async" width="16" height="16" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/en/thumb/9/96/Symbol_category_class.svg/23px-Symbol_category_class.svg.png 1.5x, //upload.wikimedia.org/wikipedia/en/thumb/9/96/Symbol_category_class.svg/31px-Symbol_category_class.svg.png 2x" data-file-width="180" data-file-height="185" /></span></span> <a href="/wiki/Category:Soil" title="Category:Soil">Category soil</a></li> <li>&#160; <a href="/wiki/Category:Soil_science" title="Category:Soil science">Category soil science</a></li> <li><span class="noviewer" typeof="mw:File"><span title="List-Class article"><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/d/db/Symbol_list_class.svg/16px-Symbol_list_class.svg.png" decoding="async" width="16" height="16" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/en/thumb/d/db/Symbol_list_class.svg/23px-Symbol_list_class.svg.png 1.5x, //upload.wikimedia.org/wikipedia/en/thumb/d/db/Symbol_list_class.svg/31px-Symbol_list_class.svg.png 2x" data-file-width="180" data-file-height="185" /></span></span> <a href="/wiki/List_of_soil_scientists" title="List of soil scientists">List of soil scientists</a></li></ul> </div></td></tr></tbody></table></div> <div class="navbox-styles"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1129693374"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236075235"></div><div role="navigation" class="navbox" aria-labelledby="Geotechnical_engineering" style="padding:3px"><table class="nowraplinks mw-collapsible autocollapse navbox-inner" style="border-spacing:0;background:transparent;color:inherit"><tbody><tr><th scope="col" class="navbox-title" colspan="2"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1129693374"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1239400231"><div class="navbar plainlinks hlist navbar-mini"><ul><li class="nv-view"><a href="/wiki/Template:Geotechnical_engineering" title="Template:Geotechnical engineering"><abbr title="View this template">v</abbr></a></li><li class="nv-talk"><a href="/wiki/Template_talk:Geotechnical_engineering" title="Template talk:Geotechnical engineering"><abbr title="Discuss this template">t</abbr></a></li><li class="nv-edit"><a href="/wiki/Special:EditPage/Template:Geotechnical_engineering" title="Special:EditPage/Template:Geotechnical engineering"><abbr title="Edit this template">e</abbr></a></li></ul></div><div id="Geotechnical_engineering" style="font-size:114%;margin:0 4em"><a href="/wiki/Geotechnical_engineering" title="Geotechnical engineering">Geotechnical engineering</a></div></th></tr><tr><td class="navbox-abovebelow" colspan="2"><div><a href="/wiki/Offshore_geotechnical_engineering" title="Offshore geotechnical engineering">Offshore geotechnical engineering</a></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Geotechnical_investigation" title="Geotechnical investigation">Investigation</a> <br />and<br />instrumentation</th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"></div><table class="nowraplinks navbox-subgroup" style="border-spacing:0"><tbody><tr><th scope="row" class="navbox-group" style="width:10.0em;font-weight: normal;">Field (<i>in situ</i>)</th><td class="navbox-list-with-group navbox-list navbox-odd" style="padding:0"><div style="padding:0 0.25em"><div class="div-col" style="column-width: 33em;"> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Core_sample.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/5/5e/Core_sample.svg/20px-Core_sample.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/5/5e/Core_sample.svg/30px-Core_sample.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/5/5e/Core_sample.svg/40px-Core_sample.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Core_drill" title="Core drill">Core drill</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Cone_penetration_test.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/2/28/Cone_penetration_test.svg/20px-Cone_penetration_test.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/2/28/Cone_penetration_test.svg/30px-Cone_penetration_test.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/2/28/Cone_penetration_test.svg/40px-Cone_penetration_test.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Cone_penetration_test" title="Cone penetration test">Cone penetration test</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Geo-electrical_sounding.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/1/10/Geo-electrical_sounding.svg/20px-Geo-electrical_sounding.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/1/10/Geo-electrical_sounding.svg/30px-Geo-electrical_sounding.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/1/10/Geo-electrical_sounding.svg/40px-Geo-electrical_sounding.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/w/index.php?title=Geo-electrical_sounding&amp;action=edit&amp;redlink=1" class="new" title="Geo-electrical sounding (page does not exist)">Geo-electrical sounding</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:In_situ_permeameter_test.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/7b/In_situ_permeameter_test.svg/20px-In_situ_permeameter_test.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/7b/In_situ_permeameter_test.svg/30px-In_situ_permeameter_test.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/7b/In_situ_permeameter_test.svg/40px-In_situ_permeameter_test.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Permeability_(Earth_sciences)" class="mw-redirect" title="Permeability (Earth sciences)">Permeability test</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Load_test.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/a/a2/Load_test.svg/20px-Load_test.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/a/a2/Load_test.svg/30px-Load_test.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/a/a2/Load_test.svg/40px-Load_test.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Load_test" class="mw-redirect" title="Load test">Load test</a> <ul><li><a href="/wiki/Static_load_testing" title="Static load testing">Static</a></li> <li><a href="/wiki/Dynamic_load_testing" title="Dynamic load testing">Dynamic</a></li> <li><a href="/wiki/Statnamic_load_test" title="Statnamic load test">Statnamic</a></li></ul></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Pore_pressure_measurement.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/f/fe/Pore_pressure_measurement.svg/20px-Pore_pressure_measurement.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/f/fe/Pore_pressure_measurement.svg/30px-Pore_pressure_measurement.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/f/fe/Pore_pressure_measurement.svg/40px-Pore_pressure_measurement.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> Pore pressure measurement <ul><li><a href="/wiki/Piezometer" class="mw-redirect" title="Piezometer">Piezometer</a></li> <li><a href="/wiki/Well#Classification" title="Well">Well</a></li></ul></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Ram_sounding.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/5/5d/Ram_sounding.svg/20px-Ram_sounding.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/5/5d/Ram_sounding.svg/30px-Ram_sounding.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/5/5d/Ram_sounding.svg/40px-Ram_sounding.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/w/index.php?title=Ram_sounding&amp;action=edit&amp;redlink=1" class="new" title="Ram sounding (page does not exist)">Ram sounding</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Rock_control_drilling.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/e/e4/Rock_control_drilling.svg/20px-Rock_control_drilling.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/e/e4/Rock_control_drilling.svg/30px-Rock_control_drilling.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/e/e4/Rock_control_drilling.svg/40px-Rock_control_drilling.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/w/index.php?title=Rock_control_drilling&amp;action=edit&amp;redlink=1" class="new" title="Rock control drilling (page does not exist)">Rock control drilling</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Rotary_pressure_sounding.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/8/81/Rotary_pressure_sounding.svg/20px-Rotary_pressure_sounding.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/8/81/Rotary_pressure_sounding.svg/30px-Rotary_pressure_sounding.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/8/81/Rotary_pressure_sounding.svg/40px-Rotary_pressure_sounding.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Rotary-pressure_sounding" title="Rotary-pressure sounding">Rotary-pressure sounding</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Rotary_weight_sounding.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/f/f9/Rotary_weight_sounding.svg/20px-Rotary_weight_sounding.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/f/f9/Rotary_weight_sounding.svg/30px-Rotary_weight_sounding.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/f/f9/Rotary_weight_sounding.svg/40px-Rotary_weight_sounding.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/w/index.php?title=Rotary_weight_sounding&amp;action=edit&amp;redlink=1" class="new" title="Rotary weight sounding (page does not exist)">Rotary weight sounding</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Sample_series.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/0/05/Sample_series.svg/20px-Sample_series.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/0/05/Sample_series.svg/30px-Sample_series.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/0/05/Sample_series.svg/40px-Sample_series.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Soil_test#Soil_testing" title="Soil test">Sample series</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Screw_plate_test.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/75/Screw_plate_test.svg/20px-Screw_plate_test.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/75/Screw_plate_test.svg/30px-Screw_plate_test.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/75/Screw_plate_test.svg/40px-Screw_plate_test.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/w/index.php?title=Screw_plate_test&amp;action=edit&amp;redlink=1" class="new" title="Screw plate test (page does not exist)">Screw plate test</a></li></ul> <ul><li><a href="/wiki/Deformation_monitoring" title="Deformation monitoring">Deformation monitoring</a> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Inclinometer.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/c/c6/Inclinometer.svg/20px-Inclinometer.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/c/c6/Inclinometer.svg/30px-Inclinometer.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/c/c6/Inclinometer.svg/40px-Inclinometer.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Inclinometer" title="Inclinometer">Inclinometer</a></li> <li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Settlement_recordings.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/3/35/Settlement_recordings.svg/20px-Settlement_recordings.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/3/35/Settlement_recordings.svg/30px-Settlement_recordings.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/3/35/Settlement_recordings.svg/40px-Settlement_recordings.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Soil_consolidation" title="Soil consolidation">Settlement recordings</a></li></ul></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Shear_vane_test.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/a/ae/Shear_vane_test.svg/20px-Shear_vane_test.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/a/ae/Shear_vane_test.svg/30px-Shear_vane_test.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/a/ae/Shear_vane_test.svg/40px-Shear_vane_test.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Shear_vane_test" title="Shear vane test">Shear vane test</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Simple_sounding.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/d/d4/Simple_sounding.svg/20px-Simple_sounding.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/d/d4/Simple_sounding.svg/30px-Simple_sounding.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/d/d4/Simple_sounding.svg/40px-Simple_sounding.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/w/index.php?title=Simple_sounding&amp;action=edit&amp;redlink=1" class="new" title="Simple sounding (page does not exist)">Simple sounding</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Standard_penetration_test.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/0/0d/Standard_penetration_test.svg/20px-Standard_penetration_test.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/0/0d/Standard_penetration_test.svg/30px-Standard_penetration_test.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/0/0d/Standard_penetration_test.svg/40px-Standard_penetration_test.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Standard_penetration_test" title="Standard penetration test">Standard penetration test</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Total_sounding.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/6/60/Total_sounding.svg/20px-Total_sounding.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/6/60/Total_sounding.svg/30px-Total_sounding.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/6/60/Total_sounding.svg/40px-Total_sounding.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Total_sounding" title="Total sounding">Total sounding</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Trial_pit.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/71/Trial_pit.svg/20px-Trial_pit.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/71/Trial_pit.svg/30px-Trial_pit.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/71/Trial_pit.svg/40px-Trial_pit.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Trial_pit" title="Trial pit">Trial pit</a></li></ul> <ul><li><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Visible_rock.svg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/1/14/Visible_rock.svg/20px-Visible_rock.svg.png" decoding="async" width="20" height="20" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/1/14/Visible_rock.svg/30px-Visible_rock.svg.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/1/14/Visible_rock.svg/40px-Visible_rock.svg.png 2x" data-file-width="512" data-file-height="512" /></a></span> <a href="/wiki/Bedrock" title="Bedrock">Visible bedrock</a></li></ul> <ul><li><a href="/wiki/Nuclear_densometer" class="mw-redirect" title="Nuclear densometer">Nuclear densometer test</a></li></ul> <ul><li><a href="/wiki/Exploration_geophysics" title="Exploration geophysics">Exploration geophysics</a></li></ul> <ul><li><a href="/wiki/Crosshole_sonic_logging" title="Crosshole sonic logging">Crosshole sonic logging</a></li></ul> <ul><li><a href="/wiki/Pile_integrity_test" title="Pile integrity test">Pile integrity test</a></li></ul> <ul><li><a href="/wiki/Wave_equation_analysis" title="Wave equation analysis">Wave equation analysis</a></li></ul></div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:10.0em;font-weight: normal;"><a href="/wiki/Soil_test" title="Soil test">Laboratory <br />testing</a></th><td class="navbox-list-with-group navbox-list navbox-even" style="padding:0"><div style="padding:0 0.25em"> <li><a href="/wiki/Soil_classification" title="Soil classification">Soil classification</a></li> <li><a href="/wiki/Atterberg_limits" title="Atterberg limits">Atterberg limits</a></li> <li><a href="/wiki/California_bearing_ratio" title="California bearing ratio">California bearing ratio</a></li> <li><a href="/wiki/Direct_shear_test" title="Direct shear test">Direct shear test</a></li> <li><a href="/wiki/Hydrometer" title="Hydrometer">Hydrometer</a></li> <li><a href="/wiki/Proctor_compaction_test" title="Proctor compaction test">Proctor compaction test</a></li> <li><a href="/wiki/R-value_(soils)" title="R-value (soils)">R-value</a></li> <li><a href="/wiki/Sieve_analysis" title="Sieve analysis">Sieve analysis</a></li> <li><a href="/wiki/Triaxial_shear_test" title="Triaxial shear test">Triaxial shear test</a></li> <li><a href="/wiki/Oedometer_test" title="Oedometer test">Oedometer test</a></li> <li><a href="/wiki/Hydraulic_conductivity#Experimental_approach" title="Hydraulic conductivity">Hydraulic conductivity tests</a></li> <li><a href="/wiki/Water_content#Measurement" title="Water content">Water content tests</a></li> </div></td></tr></tbody></table><div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a class="mw-selflink selflink">Soil</a></th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"></div><table class="nowraplinks navbox-subgroup" style="border-spacing:0"><tbody><tr><th scope="row" class="navbox-group" style="width:10.0em;font-weight: normal;">Types</th><td class="navbox-list-with-group navbox-list navbox-odd" style="padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Clay" title="Clay">Clay</a></li> <li><a href="/wiki/Silt" title="Silt">Silt</a></li> <li><a href="/wiki/Sand" title="Sand">Sand</a></li> <li><a href="/wiki/Gravel" title="Gravel">Gravel</a></li> <li><a href="/wiki/Peat" title="Peat">Peat</a></li> <li><a href="/wiki/Loam" title="Loam">Loam</a></li> <li><a href="/wiki/Loess" title="Loess">Loess</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:10.0em;font-weight: normal;">Properties</th><td class="navbox-list-with-group navbox-list navbox-even" style="padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Hydraulic_conductivity" title="Hydraulic conductivity">Hydraulic conductivity</a></li> <li><a href="/wiki/Water_content" title="Water content">Water content</a></li> <li><a href="/wiki/Void_ratio" title="Void ratio">Void ratio</a></li> <li><a href="/wiki/Bulk_density" title="Bulk density">Bulk density</a></li> <li><a href="/wiki/Thixotropy" title="Thixotropy">Thixotropy</a></li> <li><a href="/wiki/Reynolds%27_dilatancy" class="mw-redirect" title="Reynolds&#39; dilatancy">Reynolds' dilatancy</a></li> <li><a href="/wiki/Angle_of_repose" title="Angle of repose">Angle of repose</a></li> <li><a href="/wiki/Friction#Angle_of_friction" title="Friction">Friction angle</a></li> <li><a href="/wiki/Cohesion_(geology)" title="Cohesion (geology)">Cohesion</a></li> <li><a href="/wiki/Porosity" title="Porosity">Porosity</a></li> <li><a href="/wiki/Permeability_(earth_sciences)" class="mw-redirect" title="Permeability (earth sciences)">Permeability</a></li> <li><a href="/wiki/Specific_storage" title="Specific storage">Specific storage</a></li> <li><a href="/wiki/Shear_strength_(soil)" title="Shear strength (soil)">Shear strength</a></li> <li><a href="/wiki/Soil_liquefaction" title="Soil liquefaction">Sensitivity</a></li></ul> </div></td></tr></tbody></table><div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Structures <br />(<a href="/wiki/Soil-structure_interaction" title="Soil-structure interaction">Interaction</a>)</th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"></div><table class="nowraplinks navbox-subgroup" style="border-spacing:0"><tbody><tr><th scope="row" class="navbox-group" style="width:10.0em;font-weight: normal;">Natural features</th><td class="navbox-list-with-group navbox-list navbox-odd" style="padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Topography" title="Topography">Topography</a></li> <li><a href="/wiki/Vegetation" title="Vegetation">Vegetation</a></li> <li><a href="/wiki/Terrain" title="Terrain">Terrain</a></li> <li><a href="/wiki/Topsoil" title="Topsoil">Topsoil</a></li> <li><a href="/wiki/Water_table" title="Water table">Water table</a></li> <li><a href="/wiki/Bedrock" title="Bedrock">Bedrock</a></li> <li><a href="/wiki/Subgrade" title="Subgrade">Subgrade</a></li> <li><a href="/wiki/Subsoil" title="Subsoil">Subsoil</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:10.0em;font-weight: normal;"><a href="/wiki/Earthworks_(engineering)" title="Earthworks (engineering)">Earthworks</a></th><td class="navbox-list-with-group navbox-list navbox-even" style="padding:0"><div style="padding:0 0.25em"> <ul><li>Shoring structures <ul><li><a href="/wiki/Retaining_wall" title="Retaining wall">Retaining walls</a></li> <li><a href="/wiki/Gabion" title="Gabion">Gabion</a></li> <li><a href="/wiki/Ground_freezing" title="Ground freezing">Ground freezing</a></li> <li><a href="/wiki/Mechanically_stabilized_earth" title="Mechanically stabilized earth">Mechanically stabilized earth</a></li> <li><a href="/wiki/Pressure_grouting" title="Pressure grouting">Pressure grouting</a></li> <li><a href="/wiki/Slurry_wall" title="Slurry wall">Slurry wall</a></li> <li><a href="/wiki/Soil_nailing" title="Soil nailing">Soil nailing</a></li> <li><a href="/wiki/Tieback_(geotechnical)" title="Tieback (geotechnical)">Tieback</a></li></ul></li> <li><a href="/wiki/Land_development" title="Land development">Land development</a></li> <li><a href="/wiki/Landfill" title="Landfill">Landfill</a></li> <li><a href="/wiki/Digging" title="Digging">Excavation</a></li> <li><a href="/wiki/Trench" title="Trench">Trench</a></li> <li><a href="/wiki/Embankment_(earthworks)" title="Embankment (earthworks)">Embankment</a></li> <li><a href="/wiki/Cut_(earthworks)" title="Cut (earthworks)">Cut</a></li> <li><a href="/wiki/Causeway" title="Causeway">Causeway</a></li> <li><a href="/wiki/Terrace_(earthworks)" title="Terrace (earthworks)">Terracing</a></li> <li><a href="/wiki/Tunnel#Cut-and-cover" title="Tunnel">Cut-and-cover</a></li> <li><a href="/wiki/Cut_and_fill" title="Cut and fill">Cut and fill</a></li> <li><a href="/wiki/Fill_dirt" title="Fill dirt">Fill dirt</a></li> <li><a href="/wiki/Grading_(engineering)" class="mw-redirect" title="Grading (engineering)">Grading</a></li> <li><a href="/wiki/Land_reclamation" title="Land reclamation">Land reclamation</a></li> <li><a href="/wiki/Track_bed" title="Track bed">Track bed</a></li> <li><a href="/wiki/Erosion_control" title="Erosion control">Erosion control</a></li> <li><a href="/wiki/Earth_structure" title="Earth structure">Earth structure</a></li> <li><a href="/wiki/Expanded_clay_aggregate" title="Expanded clay aggregate">Expanded clay aggregate</a></li> <li><a href="/wiki/Crushed_stone" title="Crushed stone">Crushed stone</a></li> <li><a href="/wiki/Geosynthetics" title="Geosynthetics">Geosynthetics</a> <ul><li><a href="/wiki/Geotextile" title="Geotextile">Geotextile</a></li> <li><a href="/wiki/Geomembrane" title="Geomembrane">Geomembrane</a></li> <li><a href="/wiki/Geosynthetic_clay_liner" title="Geosynthetic clay liner">Geosynthetic clay liner</a></li> <li><a href="/wiki/Cellular_confinement" title="Cellular confinement">Cellular confinement</a></li></ul></li> <li><a href="/wiki/Infiltration_(hydrology)" title="Infiltration (hydrology)">Infiltration</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:10.0em;font-weight: normal;"><a href="/wiki/Foundation_(engineering)" title="Foundation (engineering)">Foundations</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Shallow_foundation" title="Shallow foundation">Shallow</a></li> <li><a href="/wiki/Deep_foundation" title="Deep foundation">Deep</a></li></ul> </div></td></tr></tbody></table><div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Soil_mechanics" title="Soil mechanics">Mechanics</a></th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"></div><table class="nowraplinks navbox-subgroup" style="border-spacing:0"><tbody><tr><th scope="row" class="navbox-group" style="width:10.0em;font-weight: normal;">Forces</th><td class="navbox-list-with-group navbox-list navbox-even" style="padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Effective_stress" title="Effective stress">Effective stress</a></li> <li><a href="/wiki/Pore_water_pressure" title="Pore water pressure">Pore water pressure</a></li> <li><a href="/wiki/Lateral_earth_pressure" title="Lateral earth pressure">Lateral earth pressure</a></li> <li><a href="/wiki/Overburden_pressure" title="Overburden pressure">Overburden pressure</a></li> <li><a href="/wiki/Preconsolidation_pressure" title="Preconsolidation pressure">Preconsolidation pressure</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:10.0em;font-weight: normal;">Phenomena/<br />problems</th><td class="navbox-list-with-group navbox-list navbox-odd" style="padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Permafrost" title="Permafrost">Permafrost</a></li> <li><a href="/wiki/Frost_heaving" title="Frost heaving">Frost heaving</a></li> <li><a href="/wiki/Consolidation_(soil)" class="mw-redirect" title="Consolidation (soil)">Consolidation</a></li> <li><a href="/wiki/Soil_compaction" title="Soil compaction">Compaction</a></li> <li><a href="/wiki/Earthquake" title="Earthquake">Earthquake</a> <ul><li><a href="/wiki/Response_spectrum" title="Response spectrum">Response spectrum</a></li> <li><a href="/wiki/Seismic_hazard" title="Seismic hazard">Seismic hazard</a></li> <li><a href="/wiki/S_wave" title="S wave">Shear wave</a></li></ul></li> <li><a href="/wiki/Landslide" title="Landslide">Landslide</a> analysis <ul><li><a href="/wiki/Slope_stability_analysis" title="Slope stability analysis">Stability analysis</a></li> <li><a href="/wiki/Landslide_mitigation" title="Landslide mitigation">Mitigation</a></li> <li><a href="/wiki/Landslide_classification" title="Landslide classification">Classification</a></li> <li><a href="/wiki/Sliding_criterion_(geotechnical_engineering)" title="Sliding criterion (geotechnical engineering)">Sliding criterion</a></li> <li><a href="/wiki/Road#Slab_stabilization" title="Road">Slab stabilisation</a></li></ul></li> <li><a href="/wiki/Bearing_capacity" title="Bearing capacity">Bearing capacity</a> * <a href="/wiki/Stress_distribution_in_soil" title="Stress distribution in soil">Stress distribution in soil</a></li></ul> </div></td></tr></tbody></table><div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Software" title="Software">Numerical analysis <br />software</a></th><td class="navbox-list-with-group navbox-list navbox-even hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/SEEP2D" title="SEEP2D">SEEP2D</a></li> <li><a href="/w/index.php?title=STABL&amp;action=edit&amp;redlink=1" class="new" title="STABL (page does not exist)">STABL</a></li> <li><a href="/wiki/SVFlux" title="SVFlux">SVFlux</a></li> <li><a href="/wiki/SVSlope" title="SVSlope">SVSlope</a></li> <li><a href="/wiki/UTEXAS" title="UTEXAS">UTEXAS</a></li> <li><a href="/wiki/Plaxis" title="Plaxis">Plaxis</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Geoprofessions" title="Geoprofessions">Related fields</a></th><td class="navbox-list-with-group navbox-list navbox-odd hlist" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Geology" title="Geology">Geology</a></li> <li><a href="/wiki/Geochemistry" title="Geochemistry">Geochemistry</a></li> <li><a href="/wiki/Petrology" title="Petrology">Petrology</a></li> <li><a href="/wiki/Earthquake_engineering" title="Earthquake engineering">Earthquake engineering</a></li> <li><a href="/wiki/Geomorphology" title="Geomorphology">Geomorphology</a></li> <li><a href="/wiki/Soil_science" title="Soil science">Soil science</a></li> <li><a href="/wiki/Hydrology" title="Hydrology">Hydrology</a></li> <li><a href="/wiki/Hydrogeology" title="Hydrogeology">Hydrogeology</a></li> <li><a href="/wiki/Biogeography" title="Biogeography">Biogeography</a></li> <li><a href="/wiki/Earth_materials" title="Earth materials">Earth materials</a></li> <li><a href="/wiki/Archaeology" title="Archaeology">Archaeology</a></li> <li><a href="/wiki/Agricultural_science" title="Agricultural science">Agricultural science</a> <ul><li><a href="/wiki/Agrology" class="mw-redirect" title="Agrology">Agrology</a></li></ul></li></ul> </div></td></tr></tbody></table></div> <div class="navbox-styles"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1129693374"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236075235"></div><div role="navigation" class="navbox" aria-labelledby="Natural_resources" style="padding:3px"><table class="nowraplinks hlist mw-collapsible autocollapse navbox-inner" style="border-spacing:0;background:transparent;color:inherit"><tbody><tr><th scope="col" class="navbox-title" colspan="2"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1129693374"><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1239400231"><div class="navbar plainlinks hlist navbar-mini"><ul><li class="nv-view"><a href="/wiki/Template:Natural_resources" title="Template:Natural resources"><abbr title="View this template">v</abbr></a></li><li class="nv-talk"><a href="/wiki/Template_talk:Natural_resources" title="Template talk:Natural resources"><abbr title="Discuss this template">t</abbr></a></li><li class="nv-edit"><a href="/wiki/Special:EditPage/Template:Natural_resources" title="Special:EditPage/Template:Natural resources"><abbr title="Edit this template">e</abbr></a></li></ul></div><div id="Natural_resources" style="font-size:114%;margin:0 4em"><a href="/wiki/Natural_resource" title="Natural resource">Natural resources</a></div></th></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Atmosphere_of_Earth" title="Atmosphere of Earth">Air</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"></div><table class="nowraplinks navbox-subgroup" style="border-spacing:0"><tbody><tr><th scope="row" class="navbox-group" style="width:7.0em;font-weight:normal;"><a href="/wiki/Air_pollution" title="Air pollution">Pollution&#160;/&#32;quality</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/National_Ambient_Air_Quality_Standards" title="National Ambient Air Quality Standards">Ambient standards <span style="font-size:85%;">(US)</span></a></li> <li><a href="/wiki/Air_quality_index" title="Air quality index">Index</a></li> <li><a href="/wiki/Indoor_air_quality" title="Indoor air quality">Indoor</a></li> <li><a href="/wiki/Air_quality_law" title="Air quality law">Law</a> <ul><li><a href="/wiki/Clean_Air_Act_(United_States)" title="Clean Air Act (United States)">Clean Air Act <span style="font-size:85%;">(US)</span></a></li></ul></li> <li><a href="/wiki/Ozone_depletion" title="Ozone depletion">Ozone depletion</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:7.0em;font-weight:normal;">Emissions</th><td class="navbox-list-with-group navbox-list navbox-even" style="padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Airshed" title="Airshed">Airshed</a></li> <li><a href="/wiki/Emissions_trading" title="Emissions trading">Trading</a></li> <li><a href="/wiki/Reducing_emissions_from_deforestation_and_forest_degradation" class="mw-redirect" title="Reducing emissions from deforestation and forest degradation">Deforestation (REDD)</a></li></ul> </div></td></tr></tbody></table><div></div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Energy" title="Energy">Energy</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Bioenergy" title="Bioenergy">Bio</a></li> <li><a href="/wiki/Energy_law" title="Energy law">Law</a></li> <li><a href="/wiki/Energy_resources" class="mw-redirect" title="Energy resources">Resources</a></li> <li><a href="/wiki/Fossil_fuel" title="Fossil fuel">Fossil fuels</a>&#160;(<a href="/wiki/Fuel_gas" title="Fuel gas">gas</a>, <a href="/wiki/Peak_coal" title="Peak coal">peak coal</a>, <a href="/wiki/Peak_gas" title="Peak gas">peak gas</a>, <a href="/wiki/Peak_oil" title="Peak oil">peak oil</a>)</li> <li><a href="/wiki/Geothermal_energy" title="Geothermal energy">Geothermal</a></li> <li><a href="/wiki/Hydropower" title="Hydropower">Hydro</a></li> <li><a href="/wiki/Nuclear_power" title="Nuclear power">Nuclear</a></li> <li><a href="/wiki/Solar_energy" title="Solar energy">Solar</a> <ul><li><a href="/wiki/Sunlight" title="Sunlight">sunlight</a></li> <li><a href="/wiki/Shade_(shadow)" title="Shade (shadow)">shade</a></li></ul></li> <li><a href="/wiki/Wind_power" title="Wind power">Wind</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Land" title="Land">Land</a></th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Agricultural_land" title="Agricultural land">Agricultural</a> <ul><li><a href="/wiki/Arable_land" title="Arable land">arable</a> <ul><li><a href="/wiki/Peak_farmland" title="Peak farmland">peak farmland</a></li></ul></li></ul></li> <li><a href="/wiki/Land_degradation" title="Land degradation">Degradation</a></li> <li><a href="/wiki/Field_(agriculture)" title="Field (agriculture)">Field</a></li> <li><a href="/wiki/Landscape" title="Landscape">Landscape</a> <ul><li><a href="/wiki/Cityscape" title="Cityscape">cityscape</a></li> <li><a href="/wiki/Seascape" title="Seascape">seascape</a></li> <li><a href="/wiki/Soundscape" title="Soundscape">soundscape</a></li> <li><a href="/wiki/Viewshed" title="Viewshed">viewshed</a></li></ul></li> <li><a href="/wiki/Land_law" title="Land law">Law</a> <ul><li><a href="/wiki/Property_law" title="Property law">property</a></li></ul></li> <li><a href="/wiki/Land_management" title="Land management">Management</a> <ul><li><a href="/wiki/Habitat_conservation" title="Habitat conservation">habitat conservation</a></li></ul></li> <li><a href="/wiki/Mineral" title="Mineral">Minerals</a> <ul><li><a href="/wiki/Gemstone" title="Gemstone">gemstone</a></li> <li><a href="/wiki/Industrial_mineral" title="Industrial mineral">industrial</a></li> <li><a href="/wiki/Ore" title="Ore">ore</a> <ul><li><a href="/wiki/Metal" title="Metal">metal</a></li></ul></li> <li><a href="/wiki/Mining" title="Mining">mining</a> <ul><li><a href="/wiki/Mining_law" title="Mining law">law</a></li> <li><a href="/wiki/Sand_mining" title="Sand mining">sand</a></li></ul></li> <li><a href="/wiki/Peak_minerals" title="Peak minerals">peak</a> <ul><li><a href="/wiki/Peak_copper" class="mw-redirect" title="Peak copper">copper</a></li> <li><a href="/wiki/Peak_phosphorus" class="mw-redirect" title="Peak phosphorus">phosphorus</a></li></ul></li> <li><a href="/wiki/Mineral_rights" title="Mineral rights">rights</a></li></ul></li> <li><a class="mw-selflink selflink">Soil</a> <ul><li><a href="/wiki/Soil_conservation" title="Soil conservation">conservation</a></li> <li><a href="/wiki/Soil_fertility" title="Soil fertility">fertility</a></li> <li><a href="/wiki/Soil_health" title="Soil health">health</a></li> <li><a href="/wiki/Soil_resilience" title="Soil resilience">resilience</a></li></ul></li> <li><a href="/wiki/Land_use" title="Land use">Use</a> <ul><li><a href="/wiki/Land-use_planning" title="Land-use planning">planning</a></li> <li><a href="/wiki/Open_space_reserve" title="Open space reserve">reserve</a></li></ul></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Life" title="Life">Life</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Biodiversity" title="Biodiversity">Biodiversity</a></li> <li><a href="/wiki/Bioprospecting" title="Bioprospecting">Bioprospecting</a> <ul><li><a href="/wiki/Biopiracy" title="Biopiracy">biopiracy</a></li></ul></li> <li><a href="/wiki/Biosphere" title="Biosphere">Biosphere</a></li> <li><a href="/wiki/Bushfood" class="mw-redirect" title="Bushfood">Bushfood</a></li> <li><a href="/wiki/Bushmeat" title="Bushmeat">Bushmeat</a></li> <li><a href="/wiki/Fishery" title="Fishery">Fisheries</a> <ul><li><a href="/wiki/Climate_change_and_fisheries" title="Climate change and fisheries">climate change</a></li> <li><a href="/wiki/Fisheries_law" title="Fisheries law">law</a></li> <li><a href="/wiki/Fisheries_management" title="Fisheries management">management</a></li></ul></li> <li><a href="/wiki/Forest" title="Forest">Forests</a> <ul><li><a href="/wiki/Forest_genetic_resources" title="Forest genetic resources">genetic resources</a></li> <li><a href="/wiki/Forestry_law" title="Forestry law">law</a></li> <li><a href="/wiki/Forest_management" title="Forest management">management</a></li> <li><a href="/wiki/Non-timber_forest_product" title="Non-timber forest product">non-timber products</a></li></ul></li> <li><a href="/wiki/Game_(food)" class="mw-redirect" title="Game (food)">Game</a> <ul><li><a href="/wiki/Game_law" title="Game law">law</a></li></ul></li> <li><a href="/wiki/Marine_conservation" title="Marine conservation">Marine conservation</a></li> <li><a href="/wiki/Meadow" title="Meadow">Meadow</a></li> <li><a href="/wiki/Pasture" title="Pasture">Pasture</a></li> <li><a href="/wiki/Plant" title="Plant">Plants</a> <ul><li><a href="/wiki/Plant_Treaty" class="mw-redirect" title="Plant Treaty">FAO Plant Treaty</a></li> <li><a href="/wiki/Food" title="Food">food</a></li> <li><a href="/wiki/Plant_genetic_resources" title="Plant genetic resources">genetic resources</a></li> <li><a href="/wiki/Gene_bank" title="Gene bank">gene banks</a></li> <li><a href="/wiki/List_of_plants_used_in_herbalism" title="List of plants used in herbalism">herbal medicines</a></li> <li><a href="/wiki/UPOV" class="mw-redirect" title="UPOV">UPOV Convention</a></li> <li><a href="/wiki/Wood" title="Wood">wood</a></li></ul></li> <li><a href="/wiki/Rangeland" title="Rangeland">Rangeland</a></li> <li><a href="/wiki/Seed_bank" title="Seed bank">Seed bank</a></li> <li><a href="/wiki/Wildlife" title="Wildlife">Wildlife</a> <ul><li><a href="/wiki/Wildlife_conservation" title="Wildlife conservation">conservation</a></li> <li><a href="/wiki/Wildlife_management" title="Wildlife management">management</a></li></ul></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Water" title="Water">Water</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"></div><table class="nowraplinks navbox-subgroup" style="border-spacing:0"><tbody><tr><th scope="row" class="navbox-group" style="width:7.0em;font-weight:normal;">Types&#160;/&#32;location</th><td class="navbox-list-with-group navbox-list navbox-even" style="padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Aquifer" title="Aquifer">Aquifer</a> <ul><li><a href="/wiki/Aquifer_storage_and_recovery" title="Aquifer storage and recovery">storage and recovery</a></li></ul></li> <li><a href="/wiki/Drinking_water" title="Drinking water">Drinking</a></li> <li><a href="/wiki/Fresh_water" title="Fresh water">Fresh</a></li> <li><a href="/wiki/Groundwater" title="Groundwater">Groundwater</a> <ul><li><a href="/wiki/Groundwater_pollution" title="Groundwater pollution">pollution</a></li> <li><a href="/wiki/Groundwater_recharge" title="Groundwater recharge">recharge</a></li> <li><a href="/wiki/Groundwater_remediation" title="Groundwater remediation">remediation</a></li></ul></li> <li><a href="/wiki/Hydrosphere" title="Hydrosphere">Hydrosphere</a></li> <li><a href="/wiki/Ice" title="Ice">Ice</a> <ul><li><a href="/wiki/Iceberg" title="Iceberg">bergs</a></li> <li><a href="/wiki/Glacier" title="Glacier">glacial</a></li> <li><a href="/wiki/Polar_ice_cap" title="Polar ice cap">polar</a></li></ul></li> <li><a href="/wiki/Irrigation" title="Irrigation">Irrigation</a> <ul><li><i><a href="/wiki/Huerta" title="Huerta">huerta</a></i></li></ul></li> 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[\"CITEREFBlakeslee2010\"] = 1,\n [\"CITEREFBollandPosnerQuirk1980\"] = 1,\n [\"CITEREFBotBenites2005\"] = 1,\n [\"CITEREFBoussingault1860–1874\"] = 1,\n [\"CITEREFBradfordWiederBonanFierer2016\"] = 1,\n [\"CITEREFBrady1984\"] = 1,\n [\"CITEREFBradyWeil2007\"] = 1,\n [\"CITEREFBrodowskiAmelungHaumaierZech2007\"] = 1,\n [\"CITEREFBronickLal2005\"] = 1,\n [\"CITEREFBrown1978\"] = 1,\n [\"CITEREFBuolSouthardGrahamMcDaniel2011\"] = 1,\n [\"CITEREFBurnsDeForestMarxsenSinsabaugh2013\"] = 1,\n [\"CITEREFBuzuleciuCraneParker2016\"] = 1,\n [\"CITEREFCalmanoHongFörstner1993\"] = 1,\n [\"CITEREFCarcaillet2001\"] = 1,\n [\"CITEREFChakraborty2022\"] = 1,\n [\"CITEREFChaneyBrownTiffin1972\"] = 1,\n [\"CITEREFChang2010\"] = 1,\n [\"CITEREFChangLoomis1945\"] = 1,\n [\"CITEREFChesworth2008\"] = 1,\n [\"CITEREFCollege_of_Tropical_Agriculture_and_Human_Resources\"] = 1,\n [\"CITEREFColumella1745\"] = 1,\n [\"CITEREFCriscuoliAlbertiBarontiFavilli2014\"] = 1,\n [\"CITEREFDakoraPhillips2002\"] = 1,\n [\"CITEREFDavidsonJanssens2006\"] = 2,\n [\"CITEREFDawsonHillier2010\"] = 1,\n [\"CITEREFDe_AlbaLindstromSchumacherMalo2004\"] = 1,\n [\"CITEREFDe_DeynVan_der_Putten2005\"] = 1,\n [\"CITEREFDean1957\"] = 1,\n [\"CITEREFDenmeadShaw1962\"] = 1,\n [\"CITEREFDiamondKinter1965\"] = 1,\n [\"CITEREFDiplockMardlinKillhamPaton2009\"] = 1,\n [\"CITEREFDojaniLakatosRascherWaneck2007\"] = 1,\n [\"CITEREFDokuchaev1967\"] = 1,\n [\"CITEREFDominatiPattersonMackay2010\"] = 1,\n [\"CITEREFDonahueMillerShickluna1977\"] = 1,\n [\"CITEREFDooley2006\"] = 1,\n [\"CITEREFDreverVance1994\"] = 1,\n [\"CITEREFDykhuizen1998\"] = 1,\n [\"CITEREFEnvironment2021\"] = 1,\n [\"CITEREFFallou1857\"] = 1,\n [\"CITEREFFarinaSumnerPlankLetzsch1980\"] = 1,\n [\"CITEREFFiererSchimelCatesZou2001\"] = 1,\n [\"CITEREFFoth1984\"] = 1,\n [\"CITEREFFronæus1953\"] = 1,\n [\"CITEREFFrouzPrachPizlHáněl2008\"] = 1,\n [\"CITEREFFujii2003\"] = 1,\n [\"CITEREFGardiner\"] = 1,\n [\"CITEREFGardnerLaryeaUnger1999\"] = 1,\n [\"CITEREFGilletPonge2002\"] = 1,\n [\"CITEREFGillulyWatersWoodford1975\"] = 1,\n [\"CITEREFGlaserHaumaierGuggenbergerZech2001\"] = 1,\n [\"CITEREFGlinka1914\"] = 1,\n [\"CITEREFGlinka1927\"] = 1,\n [\"CITEREFGoldich1938\"] = 1,\n [\"CITEREFGouldingBaileyBradburyHargreaves1998\"] = 1,\n [\"CITEREFGregoryNortcliff2013\"] = 1,\n [\"CITEREFGuSchulz1991\"] = 1,\n [\"CITEREFGuoFujimuraSatoSuda2014\"] = 1,\n [\"CITEREFHajnosJozefaciukSokołowskaGreiffenhagen2003\"] = 1,\n [\"CITEREFHansenSatoKharechaBeerling2008\"] = 1,\n [\"CITEREFHartmannBuchmannNiklaus2011\"] = 1,\n [\"CITEREFHeckFaccioRichterThöny-Meyer2013\"] = 1,\n [\"CITEREFHilgard1907\"] = 1,\n [\"CITEREFHillel1992\"] = 1,\n [\"CITEREFHiltpoldToepferKuhlmannTurlings2010\"] = 1,\n [\"CITEREFHinsinger2001\"] = 1,\n [\"CITEREFHouseBergmannStompFrederick1999\"] = 1,\n [\"CITEREFHuggett1998\"] = 1,\n [\"CITEREFHuggett2011\"] = 1,\n [\"CITEREFHungLeeBennett2015\"] = 1,\n [\"CITEREFHåkanssonLipiec2000\"] = 1,\n [\"CITEREFIUSS_Working_Group_WRB2022\"] = 1,\n [\"CITEREFIbn_al-\u0026#039;Awwam1864\"] = 1,\n [\"CITEREFInternational_Water_Management_Institute2010\"] = 1,\n [\"CITEREFJefferyGardiArwyn2010\"] = 1,\n [\"CITEREFJelinek1982\"] = 1,\n [\"CITEREFJenny1941\"] = 1,\n [\"CITEREFJiKapplerBrune2000\"] = 1,\n [\"CITEREFJoanisseBradleyPrestonBending2009\"] = 1,\n [\"CITEREFJohnsonAmbroseBassettBowen1997\"] = 1,\n [\"CITEREFJones1976\"] = 1,\n [\"CITEREFKabalaKubicz2012\"] = 1,\n [\"CITEREFKabalaZapart2012\"] = 1,\n [\"CITEREFKaramNicell1997\"] = 1,\n [\"CITEREFKarbergPregitzerKingFriend2005\"] = 1,\n [\"CITEREFKauppiKämäriPoschKauppi1986\"] = 1,\n [\"CITEREFKavithaPullagurala_Venkata_LaxmaKimLee2018\"] = 1,\n [\"CITEREFKellogg1957\"] = 1,\n [\"CITEREFKimVargasBond-LambertyTuretsky2012\"] = 1,\n [\"CITEREFKnechtGöransson2004\"] = 1,\n [\"CITEREFKohneKoehneSimunek2009\"] = 1,\n [\"CITEREFKononova2013\"] = 1,\n [\"CITEREFKopittkeMenziesWangMcKenna2019\"] = 1,\n [\"CITEREFKéfiRietkerkAladosPueyo2007\"] = 1,\n [\"CITEREFKüppersVincent\"] = 1,\n [\"CITEREFLal2004\"] = 1,\n [\"CITEREFLambersMougelJaillardHinsinger2009\"] = 1,\n [\"CITEREFLawrinenkoJingBanikLaird2017\"] = 1,\n [\"CITEREFLawrinenkoLaird2015\"] = 1,\n [\"CITEREFLe_Houérou1996\"] = 1,\n [\"CITEREFLeakeHaege2014\"] = 1,\n [\"CITEREFLehmannKleber2015\"] = 1,\n [\"CITEREFLemieuxGermain2000\"] = 1,\n [\"CITEREFLinnDoran1984\"] = 1,\n [\"CITEREFLynchLynch1958\"] = 1,\n [\"CITEREFLyuShiHanLiu2020\"] = 1,\n [\"CITEREFLäuchliGrattan2012\"] = 1,\n [\"CITEREFManjaiahKumarSachdevSachdev2010\"] = 1,\n [\"CITEREFMcCarthy2014\"] = 1,\n [\"CITEREFMcClellan\"] = 1,\n [\"CITEREFMcDowellMarshallQiMattson1999\"] = 1,\n [\"CITEREFMcFeeKellyBeck1977\"] = 1,\n [\"CITEREFMeleroMadejónRuizHerencia2007\"] = 1,\n [\"CITEREFMendonçaRowell1996\"] = 1,\n [\"CITEREFMiller\"] = 1,\n [\"CITEREFMinayevaTrofimovChichagovaDorofeyeva2008\"] = 1,\n [\"CITEREFMitchellVan_der_KnaapVan_LeeuwenButtler2001\"] = 1,\n [\"CITEREFMoayediKazemian2012\"] = 1,\n [\"CITEREFMoeckelNizzettoDi_GuardoSteinnes2008\"] = 1,\n [\"CITEREFMondiniContinLeitaDe_Nobili2002\"] = 1,\n [\"CITEREFMooreDalva1993\"] = 1,\n [\"CITEREFNavarro-GonzálezRaineyMolinaBagaley2003\"] = 1,\n [\"CITEREFOldeman1993\"] = 1,\n [\"CITEREFOosterbaan\"] = 1,\n [\"CITEREFOosterbaan1988\"] = 1,\n [\"CITEREFPanZhao2007\"] = 1,\n [\"CITEREFParfittGiltrapWhitton1995\"] = 1,\n [\"CITEREFPaulPaustianElliottCole1997\"] = 1,\n [\"CITEREFPengHorn2007\"] = 1,\n [\"CITEREFPettit\"] = 2,\n [\"CITEREFPeñuelasAsensioThollWenke2014\"] = 1,\n [\"CITEREFPhillipsMarion2004\"] = 1,\n [\"CITEREFPiccolo1996\"] = 1,\n [\"CITEREFPiccolo2002\"] = 1,\n [\"CITEREFPimentelHarveyResosudarmoSinclair1995\"] = 1,\n [\"CITEREFPonge2003\"] = 2,\n [\"CITEREFPonge2015\"] = 1,\n [\"CITEREFPouyatGroffmanYesilonisHernandez2002\"] = 1,\n [\"CITEREFPowlson2005\"] = 1,\n [\"CITEREFPrapagarIndraratnePremanandharajah2012\"] = 1,\n [\"CITEREFPrescott2010\"] = 1,\n [\"CITEREFPurringtonKendallBaterStinner1991\"] = 1,\n [\"CITEREFQiMarshallMattson1994\"] = 1,\n [\"CITEREFRajamathiThomasKamath2001\"] = 1,\n [\"CITEREFRanLuXin2014\"] = 1,\n [\"CITEREFRaynaudNunan2014\"] = 1,\n [\"CITEREFRenZengTangWang2018\"] = 1,\n [\"CITEREFRengasamy2006\"] = 1,\n [\"CITEREFRetallack1991\"] = 1,\n [\"CITEREFRetallackKrinsleyFischerRazink2016\"] = 1,\n [\"CITEREFRezaeiGuestFriedrichFayazi2009\"] = 1,\n [\"CITEREFRitter\"] = 1,\n [\"CITEREFRobertson\"] = 1,\n [\"CITEREFRoyFinckBlairTandon2006\"] = 1,\n [\"CITEREFRumpelChaplotPlanchonBernadou2006\"] = 1,\n [\"CITEREFRuserFlessaRussowSchmidt2006\"] = 1,\n [\"CITEREFRussel1957\"] = 1,\n [\"CITEREFRussell1957\"] = 1,\n [\"CITEREFRyuFaragHuReddy2003\"] = 1,\n [\"CITEREFSalethInocencioNobleRuaysoongnern2009\"] = 1,\n [\"CITEREFSalmonPonge2001\"] = 1,\n [\"CITEREFSamboNicolettoGiroPii2019\"] = 1,\n [\"CITEREFSanders1964\"] = 1,\n [\"CITEREFSaxtonRawls2006\"] = 1,\n [\"CITEREFScheu2002\"] = 1,\n [\"CITEREFSchlesingerAndrews2000\"] = 1,\n [\"CITEREFSchnürerClarholmRosswall1985\"] = 1,\n [\"CITEREFSchulzBrankatschkDümigKögel-Knabner2013\"] = 1,\n [\"CITEREFSchwerdtfeger1965\"] = 1,\n [\"CITEREFSemaluluMagundaMubiru2015\"] = 1,\n [\"CITEREFSenguptaKushwahaJimTroch2020\"] = 1,\n [\"CITEREFSetzEnzweilerSolferiniAmêndola1999\"] = 1,\n [\"CITEREFShengJohnstonTeppenBoyd2001\"] = 1,\n [\"CITEREFShengLiao1997\"] = 1,\n [\"CITEREFSilberLevkovitchGraber2010\"] = 1,\n [\"CITEREFSimonson1957\"] = 1,\n [\"CITEREFSinghRaghubanshiSinghSrivastava1989\"] = 1,\n [\"CITEREFSingletonEdmeadesSmartWheeler2001\"] = 1,\n [\"CITEREFSixPaustianElliottCombrink2000\"] = 1,\n [\"CITEREFSmithBallConenDobbie2003\"] = 1,\n [\"CITEREFSollinsRobertsonUehara1988\"] = 1,\n [\"CITEREFSparks\"] = 1,\n [\"CITEREFSparling1992\"] = 1,\n [\"CITEREFSpehnJoshiSchmidAlphei2000\"] = 1,\n [\"CITEREFSposito1984\"] = 1,\n [\"CITEREFSpositoSkipperSuttonPark1999\"] = 2,\n [\"CITEREFSpragueHermanHornbergerMills2000\"] = 1,\n [\"CITEREFStefferud1957\"] = 1,\n [\"CITEREFStretchViles2002\"] = 1,\n [\"CITEREFStuartPameVithoonjitViriyangkura2018\"] = 1,\n [\"CITEREFStürckPoortingaVerburg2014\"] = 1,\n [\"CITEREFSumnerNoble2003\"] = 1,\n [\"CITEREFSzatanik-KlocSzerementJózefaciuk2017\"] = 1,\n [\"CITEREFTahirMarschner2017\"] = 1,\n [\"CITEREFTamboli1961\"] = 1,\n [\"CITEREFTandon\"] = 1,\n [\"CITEREFTaylorAshcroft1972\"] = 1,\n [\"CITEREFTheng1982\"] = 1,\n [\"CITEREFTietjenWetzel2003\"] = 1,\n [\"CITEREFTorbertWood1992\"] = 1,\n [\"CITEREFTorsvikØvreås2002\"] = 1,\n [\"CITEREFTurkelboomPoesenOhlerVan_Keer1997\"] = 1,\n [\"CITEREFUgoliniDahlgren2002\"] = 1,\n [\"CITEREFUlrich1983\"] = 1,\n [\"CITEREFUselmanQuallsLilienfein2007\"] = 1,\n [\"CITEREFValentind\u0026#039;HerbèsPoesen1999\"] = 1,\n [\"CITEREFVan_BruggenSemenov2000\"] = 1,\n [\"CITEREFVan_CuykSiegristLoganMasson2001\"] = 1,\n [\"CITEREFVan_SchöllSmitsHoffland2006\"] = 1,\n [\"CITEREFVan_der_PloegBöhmKirkham1999\"] = 1,\n [\"CITEREFVan_der_PloegSchweigertBachmann2001\"] = 1,\n [\"CITEREFVannier1987\"] = 1,\n [\"CITEREFVaradachariGhosh1984\"] = 2,\n [\"CITEREFVerachtertVan_den_EeckhautPoesenDeckers2010\"] = 1,\n [\"CITEREFVirtoImazFernández-UgaldeGartzia-Bengoetxea2015\"] = 1,\n [\"CITEREFVitousekSanford1986\"] = 1,\n [\"CITEREFVoroneyHeck2007\"] = 1,\n [\"CITEREFWagaiMayerKitayamaKnicker2008\"] = 1,\n [\"CITEREFWangAmundsonTrumbmore1996\"] = 1,\n [\"CITEREFWangYangDongZhang2009\"] = 1,\n [\"CITEREFWarington1878\"] = 1,\n [\"CITEREFWay1849\"] = 1,\n [\"CITEREFWay1852\"] = 1,\n [\"CITEREFWeilBrady2016\"] = 1,\n [\"CITEREFWhitmanColemanWiebe1998\"] = 1,\n [\"CITEREFWinogradsky1890\"] = 1,\n [\"CITEREFWoodruff1955\"] = 1,\n [\"CITEREFWynot\"] = 1,\n [\"CITEREFXuNieberGupta1992\"] = 1,\n [\"CITEREFYangKanaeOkiKoike2003\"] = 1,\n [\"CITEREFYuKambojWangCheng2015\"] = 1,\n [\"CITEREFZanellaKatzensteinerPongeJabiol2019\"] = 1,\n [\"CITEREFde_Lavoisier1777\"] = 1,\n [\"CITEREFde_Serres1600\"] = 1,\n [\"CITEREFvan_WindenReichartMcNamaraBenthien2012\"] = 1,\n [\"CITEREFvon_Liebig1840\"] = 1,\n}\ntemplate_list = table#1 {\n [\"=\"] = 1,\n [\"Abbr\"] = 1,\n [\"Authority control\"] = 1,\n [\"Chem\"] = 14,\n [\"Cite book\"] = 44,\n [\"Cite journal\"] = 185,\n [\"Cite web\"] = 35,\n [\"Commons category\"] = 1,\n [\"Convert\"] = 2,\n [\"Dead link\"] = 3,\n [\"Div col\"] = 2,\n [\"For\"] = 2,\n [\"Free-content attribution\"] = 1,\n [\"Further\"] = 3,\n [\"Geotechnical engineering\"] = 1,\n [\"Harvc\"] = 5,\n [\"ISBN\"] = 4,\n [\"Lang\"] = 2,\n [\"Main\"] = 14,\n [\"N/a\"] = 11,\n [\"Natural resources\"] = 1,\n [\"Not a typo\"] = 1,\n [\"Nowrap\"] = 4,\n [\"Other uses\"] = 1,\n [\"Overly detailed\"] = 1,\n [\"Pie chart\"] = 2,\n [\"Portal\"] = 1,\n [\"Pp-move\"] = 1,\n [\"Refbegin\"] = 2,\n [\"Refend\"] = 2,\n [\"Reflist\"] = 1,\n [\"See also\"] = 2,\n [\"Sfn\"] = 23,\n [\"Short description\"] = 1,\n [\"Soil science topics\"] = 1,\n [\"Use dmy dates\"] = 1,\n [\"Webarchive\"] = 2,\n [\"Wikibooks\"] = 1,\n [\"Wikiquote\"] = 1,\n [\"Wikiversity\"] = 1,\n [\"Wiktionary\"] = 1,\n}\narticle_whitelist = table#1 {\n}\n","limitreport-profile":[["?","400","16.3"],["MediaWiki\\Extension\\Scribunto\\Engines\\LuaSandbox\\LuaSandboxCallback::callParserFunction","300","12.2"],["MediaWiki\\Extension\\Scribunto\\Engines\\LuaSandbox\\LuaSandboxCallback::match","180","7.3"],["MediaWiki\\Extension\\Scribunto\\Engines\\LuaSandbox\\LuaSandboxCallback::gsub","160","6.5"],["dataWrapper \u003Cmw.lua:672\u003E","160","6.5"],["recursiveClone 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Inc.","logo":{"@type":"ImageObject","url":"https:\/\/www.wikimedia.org\/static\/images\/wmf-hor-googpub.png"}},"datePublished":"2002-02-05T07:43:26Z","dateModified":"2024-11-20T21:20:15Z","image":"https:\/\/upload.wikimedia.org\/wikipedia\/commons\/4\/46\/Stagnogley.JPG","headline":"natural body consisting of layers that are primarily composed of minerals"}</script> </body> </html>

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