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class="uploads-container" id="social-redesign-work-container"><div class="upload-header"><h2 class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by O. Menyailo</h3></div><div class="js-work-strip profile--work_container" data-work-id="108964575"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/108964575/Single_tree_effects_on_denitrification_and_soil_microbial_biomass_in_agroforestry_systems_and_natural_forests_of_the_Amazon_region"><img alt="Research paper thumbnail of Single tree-effects on denitrification and soil microbial biomass in agroforestry systems and natural forests of the Amazon region" class="work-thumbnail" src="https://attachments.academia-assets.com/107218579/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/108964575/Single_tree_effects_on_denitrification_and_soil_microbial_biomass_in_agroforestry_systems_and_natural_forests_of_the_Amazon_region">Single tree-effects on denitrification and soil microbial biomass in agroforestry systems and natural forests of the Amazon region</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The aim of this study was to find the effect of tree species (Theobroma grandiflorum - cupuacu, B...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The aim of this study was to find the effect of tree species (Theobroma grandiflorum - cupuacu, Bixa orellana - urucum, Vismia spp, Carapa guianensis - andiroba, Ceiba pentandra - sumauma) used in agroforestry system in Amazonian region and natural forests on the total biomass of heterotrophic microorganisms (BH), in Manaus-AM (Brasil).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c65abdddc890c945e3421c261314e377" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":107218579,"asset_id":108964575,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/107218579/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108964575"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108964575"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108964575; 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This study ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Soil CO2 emission is one of the most important components of the global carbon cycle. This study analyzes the seasonal dynamics of soil emission for various land cover types in the middle taiga subzone of central Siberia during five growing seasons. It is shown that, throughout a vast area covered by pine forests and their derivatives formed on sandy soils, seasonal CO2 emission values are determined primarily by the moisture conditions and only secondarily by the temperature regime and ecosystem type. The effect of the forest type is manifested only under the most favorable moisture conditions. A new approach is proposed: divide the growing season into dry and moist periods depending on the threshold soil moisture for areas with different vegetation types.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108964574"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108964574"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108964574; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108964574]").text(description); $(".js-view-count[data-work-id=108964574]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108964574; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108964574']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 108964574, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=108964574]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108964574,"title":"The Impact of Climatic Factors on CО2 Emissions from Soils of Middle-Taiga Forests in Central Siberia: Emission as a Function of Soil Temperature and Moisture","translated_title":"","metadata":{"abstract":"Soil CO2 emission is one of the most important components of the global carbon cycle. 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This study analyzes the seasonal dynamics of soil emission for various land cover types in the middle taiga subzone of central Siberia during five growing seasons. It is shown that, throughout a vast area covered by pine forests and their derivatives formed on sandy soils, seasonal CO2 emission values are determined primarily by the moisture conditions and only secondarily by the temperature regime and ecosystem type. The effect of the forest type is manifested only under the most favorable moisture conditions. 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Menyailo","url":"https://independent.academia.edu/OMenyailo"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":14719,"name":"Carbon Cycle","url":"https://www.academia.edu/Documents/in/Carbon_Cycle"},{"id":83037,"name":"Soil moisture","url":"https://www.academia.edu/Documents/in/Soil_moisture"},{"id":133176,"name":"Moisture","url":"https://www.academia.edu/Documents/in/Moisture"},{"id":278441,"name":"Soil Temperature","url":"https://www.academia.edu/Documents/in/Soil_Temperature"},{"id":373754,"name":"Ecosystem","url":"https://www.academia.edu/Documents/in/Ecosystem"},{"id":845678,"name":"Water Content","url":"https://www.academia.edu/Documents/in/Water_Content"},{"id":1222799,"name":"Soil Water","url":"https://www.academia.edu/Documents/in/Soil_Water"},{"id":1648025,"name":"Taiga","url":"https://www.academia.edu/Documents/in/Taiga"},{"id":2904182,"name":"Middle Taiga","url":"https://www.academia.edu/Documents/in/Middle_Taiga"}],"urls":[{"id":35254849,"url":"http://link.springer.com/content/pdf/10.1134/S1067413620010063.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="108964573"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/108964573/13C_and_15N_natural_abundance_of_the_soil_microbial_biomass"><img alt="Research paper thumbnail of 13C and 15N natural abundance of the soil microbial biomass" class="work-thumbnail" src="https://attachments.academia-assets.com/107218584/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/108964573/13C_and_15N_natural_abundance_of_the_soil_microbial_biomass">13C and 15N natural abundance of the soil microbial biomass</a></div><div class="wp-workCard_item"><span>Soil Biology and Biochemistry</span><span>, 2006</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7289ea94c52452d21d922bd956d62fd4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":107218584,"asset_id":108964573,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/107218584/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108964573"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108964573"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108964573; 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It is often observed that more decomposed soil organic matter is 13 C, and especially 15 N-enriched relative to fresh litter and recent organic matter. We investigated whether this shift in isotope composition relates to the isotope composition of the microbial biomass, an important source for soil organic matter. We developed a new approach to determine the natural abundance C and N isotope composition of the microbial biomass across a broad range of soil types, vegetation, and climates. We found consistently that the soil microbial biomass was 15 N-enriched relative to the total (3.2 %) and extractable N pools (3.7 %), and 13 C-enriched relative to the extractable C pool (2.5 %). The microbial biomass was also 13 C-enriched relative to total C for soils that exhibited a C3-plant signature (1.6 %), but 13 C-depleted for soils with a C4 signature (À1.1 %). The latter was probably associated with an increase of annual C3 forbs in C4 grasslands after an extreme drought. These findings are in agreement with the proposed contribution of microbial products to the stabilized soil organic matter and may help explain the shift in isotope composition during soil organic matter formation.","publication_date":{"day":null,"month":null,"year":2006,"errors":{}},"publication_name":"Soil Biology and Biochemistry","grobid_abstract_attachment_id":107218584},"translated_abstract":null,"internal_url":"https://www.academia.edu/108964573/13C_and_15N_natural_abundance_of_the_soil_microbial_biomass","translated_internal_url":"","created_at":"2023-11-07T10:40:59.108-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":107218584,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/107218584/thumbnails/1.jpg","file_name":"0912f50b9a620c4b87000000.pdf","download_url":"https://www.academia.edu/attachments/107218584/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"13C_and_15N_natural_abundance_of_the_soi.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/107218584/0912f50b9a620c4b87000000-libre.pdf?1699382709=\u0026response-content-disposition=attachment%3B+filename%3D13C_and_15N_natural_abundance_of_the_soi.pdf\u0026Expires=1733220925\u0026Signature=F060xSCAI58SiCDFx67GnvYqgqdM8a5LTdNerhWIWXmuQAL00NxHAeO2GbOO8ou0YVPLygGltd3wWb5laf5KbE9O15a7Wn9sCDiuhcnKN42Noez5THJlWF1Wr45zoKWpy1I6ch6C67Joh2byiiRPNOP-8NNXhsj6yIS9D4CPWDh9d-0svZCnaPceGMSM-xLPCDDjHGrsYQLQJEmtbXIrlgbkjm0h8DTyElU6GcF1BtyqsKta3hhxVMsJYVx5baABoWj285NEnKZ~SsLb~JSur9a5QM16GRtPHwwAcrA37~xoOkNbtwnzHO2ALMl8UpGMZcEMDYdnlfiMeFyg4YU~iw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"13C_and_15N_natural_abundance_of_the_soil_microbial_biomass","translated_slug":"","page_count":10,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="108964572"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/108964572/Age_Dependent_Changes_in_Soil_Respiration_and_Associated_Parameters_in_Siberian_Permafrost_Larch_Stands_Affected_by_Wildfire"><img alt="Research paper thumbnail of Age-Dependent Changes in Soil Respiration and Associated Parameters in Siberian Permafrost Larch Stands Affected by Wildfire" class="work-thumbnail" src="https://attachments.academia-assets.com/107218572/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/108964572/Age_Dependent_Changes_in_Soil_Respiration_and_Associated_Parameters_in_Siberian_Permafrost_Larch_Stands_Affected_by_Wildfire">Age-Dependent Changes in Soil Respiration and Associated Parameters in Siberian Permafrost Larch Stands Affected by Wildfire</a></div><div class="wp-workCard_item"><span>Forests</span><span>, 2021</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The observed high spatial variation in soil respiration (SR) and associated parameters emphasized...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The observed high spatial variation in soil respiration (SR) and associated parameters emphasized the importance of SR heterogeneity at high latitudes and the involvement of many factors in its regulation, especially within fire-affected areas. The problem of estimating CO2 emissions during post-fire recovery in high-latitude ecosystems addresses the mutual influence of wildfires and climate change on the C cycle. Despite its importance, especially in permafrost regions because of their vulnerability, the mutual influence of these factors on CO2 dynamics has rarely been studied. Thus, we aimed to understand the dynamics of soil respiration (SR) in wildfire-affected larch recovery successions. We analyzed 16-year data (1995–2010) on SR and associated soil, biological, and environmental parameters obtained during several field studies in larch stands of different ages (0–276 years) in the Krasnoyarsk region (Russia). We observed a high variation in SR and related parameters among the ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="591626014d28112e4a3267d219a876b4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":107218572,"asset_id":108964572,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/107218572/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108964572"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108964572"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108964572; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108964572]").text(description); $(".js-view-count[data-work-id=108964572]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108964572; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108964572']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 108964572, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "591626014d28112e4a3267d219a876b4" } } $('.js-work-strip[data-work-id=108964572]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108964572,"title":"Age-Dependent Changes in Soil Respiration and Associated Parameters in Siberian Permafrost Larch Stands Affected by Wildfire","translated_title":"","metadata":{"abstract":"The observed high spatial variation in soil respiration (SR) and associated parameters emphasized the importance of SR heterogeneity at high latitudes and the involvement of many factors in its regulation, especially within fire-affected areas. The problem of estimating CO2 emissions during post-fire recovery in high-latitude ecosystems addresses the mutual influence of wildfires and climate change on the C cycle. Despite its importance, especially in permafrost regions because of their vulnerability, the mutual influence of these factors on CO2 dynamics has rarely been studied. Thus, we aimed to understand the dynamics of soil respiration (SR) in wildfire-affected larch recovery successions. We analyzed 16-year data (1995–2010) on SR and associated soil, biological, and environmental parameters obtained during several field studies in larch stands of different ages (0–276 years) in the Krasnoyarsk region (Russia). We observed a high variation in SR and related parameters among the ...","publisher":"MDPI AG","publication_date":{"day":null,"month":null,"year":2021,"errors":{}},"publication_name":"Forests"},"translated_abstract":"The observed high spatial variation in soil respiration (SR) and associated parameters emphasized the importance of SR heterogeneity at high latitudes and the involvement of many factors in its regulation, especially within fire-affected areas. The problem of estimating CO2 emissions during post-fire recovery in high-latitude ecosystems addresses the mutual influence of wildfires and climate change on the C cycle. Despite its importance, especially in permafrost regions because of their vulnerability, the mutual influence of these factors on CO2 dynamics has rarely been studied. Thus, we aimed to understand the dynamics of soil respiration (SR) in wildfire-affected larch recovery successions. We analyzed 16-year data (1995–2010) on SR and associated soil, biological, and environmental parameters obtained during several field studies in larch stands of different ages (0–276 years) in the Krasnoyarsk region (Russia). 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Tree species effects on soil sources of N2O" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95813351/A_new_method_of_quantifying_contributions_from_nitrification_and_denitrification_Tree_species_effects_on_soil_sources_of_N2O">A new method of quantifying contributions from nitrification and denitrification. Tree species effects on soil sources of N2O</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Soil microorganisms produce N2O through denitrification and nitrification. Here we propose the ne...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Soil microorganisms produce N2O through denitrification and nitrification. Here we propose the new method to accurately distinguish contributions of nitrification or denitrification to the N2O production. This method is based on the application of the NH4NO3 (substrate for both processes) with low level of oxygen isotopes enrichment (ca. 1.6 atom excess, %). During nitrification, the first atom of oxygen in nitrous oxide derives from atmospheric O2 and the second from H2O, while in denitrification, all oxygen atoms of the formed N2O originate from oxygen of NO3-. Thus applying enriched 18O-NO3- and measuring 18O-N2O thereafter it is possible to distinguish the two processes. We used the Siberian afforestation experiment with six dominant in Siberia tree species grown artificially for about 30 y on initially homogeneous soil. The soil samples from all species were incubated at the two moisture levels to test whether the isotopic signatures of oxygen in N2O will be more enriched at hi...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95813351"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95813351"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95813351; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95813351]").text(description); $(".js-view-count[data-work-id=95813351]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95813351; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95813351']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 95813351, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=95813351]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95813351,"title":"A new method of quantifying contributions from nitrification and denitrification. Tree species effects on soil sources of N2O","translated_title":"","metadata":{"abstract":"Soil microorganisms produce N2O through denitrification and nitrification. Here we propose the new method to accurately distinguish contributions of nitrification or denitrification to the N2O production. This method is based on the application of the NH4NO3 (substrate for both processes) with low level of oxygen isotopes enrichment (ca. 1.6 atom excess, %). During nitrification, the first atom of oxygen in nitrous oxide derives from atmospheric O2 and the second from H2O, while in denitrification, all oxygen atoms of the formed N2O originate from oxygen of NO3-. Thus applying enriched 18O-NO3- and measuring 18O-N2O thereafter it is possible to distinguish the two processes. We used the Siberian afforestation experiment with six dominant in Siberia tree species grown artificially for about 30 y on initially homogeneous soil. The soil samples from all species were incubated at the two moisture levels to test whether the isotopic signatures of oxygen in N2O will be more enriched at hi..."},"translated_abstract":"Soil microorganisms produce N2O through denitrification and nitrification. Here we propose the new method to accurately distinguish contributions of nitrification or denitrification to the N2O production. This method is based on the application of the NH4NO3 (substrate for both processes) with low level of oxygen isotopes enrichment (ca. 1.6 atom excess, %). During nitrification, the first atom of oxygen in nitrous oxide derives from atmospheric O2 and the second from H2O, while in denitrification, all oxygen atoms of the formed N2O originate from oxygen of NO3-. Thus applying enriched 18O-NO3- and measuring 18O-N2O thereafter it is possible to distinguish the two processes. We used the Siberian afforestation experiment with six dominant in Siberia tree species grown artificially for about 30 y on initially homogeneous soil. The soil samples from all species were incubated at the two moisture levels to test whether the isotopic signatures of oxygen in N2O will be more enriched at hi...","internal_url":"https://www.academia.edu/95813351/A_new_method_of_quantifying_contributions_from_nitrification_and_denitrification_Tree_species_effects_on_soil_sources_of_N2O","translated_internal_url":"","created_at":"2023-01-27T12:05:23.850-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"A_new_method_of_quantifying_contributions_from_nitrification_and_denitrification_Tree_species_effects_on_soil_sources_of_N2O","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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It is shown that N transformation in meadow-alpine soils (Leptic Umbrisols) of the northwestern Caucasus (Teberda Reserve, Karachay-Cherkess Republic) leads to well-expressed differences in isotopic signatures of different N compounds: δ15N of extractable organic matter &gt; δ15Ntotal &gt; δ15N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NH}}_{{\text{4}}}^{ + }$$\end{document} &gt; δ15N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NO}}_{{\text{3}}}^{ - }.$$\end{document} The range of δ15N in this sequence reaches 25‰. Differences in δ15N within the same pool of N in soils of different alpine ecosystems, as well as seasonal dynamics of δ15N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NH}}_{{\text{4}}}^{ + },$$\end{document} are much less pronounced (the range of δ15N is 2–4‰). The values of δ15Ntotal and δ15N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NH}}_{{\text{4}}}^{ + }$$\end{document} positively correlate with N mineralization and nitrification and demonstrate the accumulation of heavy N isotope in soils of the alpine ecosystems with more active N transformation processes. Obviously, nitrification is the key process controlling the isotopic signature of N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NH}}_{{\text{4}}}^{ + }.$$\end{document} The role of N mineralization in the fractionation of N isotopes is less obvious, and 15N accumulation in the extractable organic matter can be related to the significant content of “heavy” microbial N in extractable organic N pool.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="78568964"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="78568964"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 78568964; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=78568964]").text(description); $(".js-view-count[data-work-id=78568964]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 78568964; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='78568964']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 78568964, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=78568964]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":78568964,"title":"Isotopic Composition of Nitrogen and Transformation of Nitrogen Compounds in Meadow-Alpine Soils","translated_title":"","metadata":{"abstract":"Isotopic composition of nitrogen in soils can be an informative indicator of N transformation processes and sources of N nutrition of plants, but data on δ15N of labile N compounds are scarce. It is shown that N transformation in meadow-alpine soils (Leptic Umbrisols) of the northwestern Caucasus (Teberda Reserve, Karachay-Cherkess Republic) leads to well-expressed differences in isotopic signatures of different N compounds: δ15N of extractable organic matter \u0026gt; δ15Ntotal \u0026gt; δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + }$$\\end{document} \u0026gt; δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NO}}_{{\\text{3}}}^{ - }.$$\\end{document} The range of δ15N in this sequence reaches 25‰. Differences in δ15N within the same pool of N in soils of different alpine ecosystems, as well as seasonal dynamics of δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + },$$\\end{document} are much less pronounced (the range of δ15N is 2–4‰). The values of δ15Ntotal and δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + }$$\\end{document} positively correlate with N mineralization and nitrification and demonstrate the accumulation of heavy N isotope in soils of the alpine ecosystems with more active N transformation processes. Obviously, nitrification is the key process controlling the isotopic signature of N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + }.$$\\end{document} The role of N mineralization in the fractionation of N isotopes is less obvious, and 15N accumulation in the extractable organic matter can be related to the significant content of “heavy” microbial N in extractable organic N pool.","publisher":"Pleiades Publishing Ltd","publication_date":{"day":null,"month":null,"year":2019,"errors":{}},"publication_name":"Eurasian Soil Science"},"translated_abstract":"Isotopic composition of nitrogen in soils can be an informative indicator of N transformation processes and sources of N nutrition of plants, but data on δ15N of labile N compounds are scarce. It is shown that N transformation in meadow-alpine soils (Leptic Umbrisols) of the northwestern Caucasus (Teberda Reserve, Karachay-Cherkess Republic) leads to well-expressed differences in isotopic signatures of different N compounds: δ15N of extractable organic matter \u0026gt; δ15Ntotal \u0026gt; δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + }$$\\end{document} \u0026gt; δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NO}}_{{\\text{3}}}^{ - }.$$\\end{document} The range of δ15N in this sequence reaches 25‰. Differences in δ15N within the same pool of N in soils of different alpine ecosystems, as well as seasonal dynamics of δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + },$$\\end{document} are much less pronounced (the range of δ15N is 2–4‰). The values of δ15Ntotal and δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + }$$\\end{document} positively correlate with N mineralization and nitrification and demonstrate the accumulation of heavy N isotope in soils of the alpine ecosystems with more active N transformation processes. 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It has been shown that the ericaceous dwarf shrub Vaccinium vitis-idaea characterized by ericoid mycorrhiza, which releases oxidative and hydrolytic enzymes into the soil, has an effect on the properties of mountain-meadow soil in the alpine phytocenosis. In the presence of V. vitis-idaea, the soil is characterized by increased acidity; higher contents of labile organic matter carbon, microbial biomass nitrogen, and available phosphorus; and higher microbial activity.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="78568963"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="78568963"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 78568963; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=78568963]").text(description); $(".js-view-count[data-work-id=78568963]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 78568963; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='78568963']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 78568963, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=78568963]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":78568963,"title":"The Effect of Vaccinium vitis-idaea on Properties of Mountain-Meadow Soil under Alpine Lichen Heath","translated_title":"","metadata":{"abstract":"Abstract—The study of the effect of mycorrhiza symbiosis on the transformation of carbon and nitrogen compounds in soils is important in view of the necessity to predict variations in the cycles of nutrients under changing environmental conditions. It has been shown that the ericaceous dwarf shrub Vaccinium vitis-idaea characterized by ericoid mycorrhiza, which releases oxidative and hydrolytic enzymes into the soil, has an effect on the properties of mountain-meadow soil in the alpine phytocenosis. In the presence of V. vitis-idaea, the soil is characterized by increased acidity; higher contents of labile organic matter carbon, microbial biomass nitrogen, and available phosphorus; and higher microbial activity.","publisher":"Pleiades Publishing Ltd","publication_date":{"day":null,"month":null,"year":2019,"errors":{}},"publication_name":"Russian Journal of Ecology"},"translated_abstract":"Abstract—The study of the effect of mycorrhiza symbiosis on the transformation of carbon and nitrogen compounds in soils is important in view of the necessity to predict variations in the cycles of nutrients under changing environmental conditions. It has been shown that the ericaceous dwarf shrub Vaccinium vitis-idaea characterized by ericoid mycorrhiza, which releases oxidative and hydrolytic enzymes into the soil, has an effect on the properties of mountain-meadow soil in the alpine phytocenosis. In the presence of V. vitis-idaea, the soil is characterized by increased acidity; higher contents of labile organic matter carbon, microbial biomass nitrogen, and available phosphorus; and higher microbial activity.","internal_url":"https://www.academia.edu/78568963/The_Effect_of_Vaccinium_vitis_idaea_on_Properties_of_Mountain_Meadow_Soil_under_Alpine_Lichen_Heath","translated_internal_url":"","created_at":"2022-05-05T22:52:42.991-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Effect_of_Vaccinium_vitis_idaea_on_Properties_of_Mountain_Meadow_Soil_under_Alpine_Lichen_Heath","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. Menyailo","url":"https://independent.academia.edu/OMenyailo"},"attachments":[],"research_interests":[{"id":523,"name":"Chemistry","url":"https://www.academia.edu/Documents/in/Chemistry"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"}],"urls":[{"id":20256412,"url":"http://link.springer.com/content/pdf/10.1134/S1067413619040118.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="78568962"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/78568962/Determination_of_carbon_and_nitrogen_in_microbial_biomass_of_southern_Taiga_soils_by_different_methods"><img alt="Research paper thumbnail of Determination of carbon and nitrogen in microbial biomass of southern-Taiga soils by different methods" class="work-thumbnail" src="https://attachments.academia-assets.com/85572108/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/78568962/Determination_of_carbon_and_nitrogen_in_microbial_biomass_of_southern_Taiga_soils_by_different_methods">Determination of carbon and nitrogen in microbial biomass of southern-Taiga soils by different methods</a></div><div class="wp-workCard_item"><span>Eurasian Soil Science</span><span>, 2016</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="44b0c7f4f58345467daf4dfaa69c311b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":85572108,"asset_id":78568962,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/85572108/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="78568962"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="78568962"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 78568962; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=78568962]").text(description); $(".js-view-count[data-work-id=78568962]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 78568962; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='78568962']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 78568962, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "44b0c7f4f58345467daf4dfaa69c311b" } } $('.js-work-strip[data-work-id=78568962]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":78568962,"title":"Determination of carbon and nitrogen in microbial biomass of southern-Taiga soils by different methods","translated_title":"","metadata":{"publisher":"Pleiades Publishing Ltd","grobid_abstract":"The results of methods for determining microbial biomass carbon vary in reproducibility among soils. The fumigation-extraction and substrate-induced respiration methods give similar results for Albic Luvisol and Gleyic Fluvisol, while the results of the rehydration method are reliably higher. In Histic Fluvisol, relatively similar results are obtained using the fumigation-extraction and rehydration methods, and the substrate-induced respiration method gives almost halved results. The seasonal dynamics of microbial biomass carbon also varies depending on the method used. The highest difference is typical for the warm period, when the concentrations found by the extraction and substrate-induced methods poorly agree between two out of three soils studied. The concentration of microbial biomass nitrogen is less sensitive to the analytical method: the differences between the results of the fumigation-extraction and rehydration methods are statistically insignificant in the all soils. To reveal stable relationships between the results of determining microbial carbon and the soil properties and analytical method, a large diversity of soils should be studied. This will allow for proposing of conversion factors for the recalculation of the obtained values to the concentrations of carbon and nitrogen in microbial biomass for different soils (or soil groups) and, hence, the more correct comparison of the results obtained by different methods.","publication_date":{"day":null,"month":null,"year":2016,"errors":{}},"publication_name":"Eurasian Soil Science","grobid_abstract_attachment_id":85572108},"translated_abstract":null,"internal_url":"https://www.academia.edu/78568962/Determination_of_carbon_and_nitrogen_in_microbial_biomass_of_southern_Taiga_soils_by_different_methods","translated_internal_url":"","created_at":"2022-05-05T22:52:42.825-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":85572108,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/85572108/thumbnails/1.jpg","file_name":"10.1134s1064229316060053.pdf","download_url":"https://www.academia.edu/attachments/85572108/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Determination_of_carbon_and_nitrogen_in.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/85572108/10.1134s1064229316060053-libre.pdf?1651817168=\u0026response-content-disposition=attachment%3B+filename%3DDetermination_of_carbon_and_nitrogen_in.pdf\u0026Expires=1733220925\u0026Signature=dlFW9EhLRH4ysqFM9G8qvrhRXp84bLQ~cA6qmPbj7oHB61bjJG~By8~1DzPlila8tDnL--G43KkK7QECOauox9uk24vhWx~5yT4wN-MlGsdhyuCTq8nGHguFGQ-9dT8zOYAON2xGRWIZR3yN1cRvwVmkJulfTYE~VrkQ0KQ54LnZON0fpopLOuN4FdIB41Koi1npIwpN3HxbqrdXIgqkWl5D6P18kwVq8v5xppSAW2z7GrdudFNAQXnNi2SJJNHWAy32FeC8nw9WOiBPLuvMxIqEM2NBWVSD4BJ4ejLZ4ab9gKMjgpc6ft6hfdMzwrBG3rlRIsboLIP8QZFkmPeZrQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Determination_of_carbon_and_nitrogen_in_microbial_biomass_of_southern_Taiga_soils_by_different_methods","translated_slug":"","page_count":11,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="78568932"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/78568932/Interactive_effects_of_tree_species_and_soil_moisture_on_methane_consumption"><img alt="Research paper thumbnail of Interactive effects of tree species and soil moisture on methane consumption" class="work-thumbnail" src="https://attachments.academia-assets.com/85572069/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/78568932/Interactive_effects_of_tree_species_and_soil_moisture_on_methane_consumption">Interactive effects of tree species and soil moisture on methane consumption</a></div><div class="wp-workCard_item"><span>Soil Biology and Biochemistry</span><span>, 2003</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e0a3f3ba4c052b50d66c033dd49c1b92" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":85572069,"asset_id":78568932,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/85572069/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="78568932"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="78568932"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 78568932; 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Menyailo</a></span></div><div class="wp-workCard_item"><span>Soil Biology and Biochemistry</span><span>, 2006</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f60a4b46ab2fecca2950d0a7ba1f5b3a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":46033085,"asset_id":12640386,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/46033085/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="12640386"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="12640386"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 12640386; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=12640386]").text(description); $(".js-view-count[data-work-id=12640386]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 12640386; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='12640386']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 12640386, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "f60a4b46ab2fecca2950d0a7ba1f5b3a" } } $('.js-work-strip[data-work-id=12640386]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":12640386,"title":"13C and 15N natural abundance of the soil microbial biomass","translated_title":"","metadata":{"grobid_abstract":"Stable isotope analysis is a powerful tool in the study of soil organic matter formation. It is often observed that more decomposed soil organic matter is 13 C, and especially 15 N-enriched relative to fresh litter and recent organic matter. We investigated whether this shift in isotope composition relates to the isotope composition of the microbial biomass, an important source for soil organic matter. We developed a new approach to determine the natural abundance C and N isotope composition of the microbial biomass across a broad range of soil types, vegetation, and climates. We found consistently that the soil microbial biomass was 15 N-enriched relative to the total (3.2 %) and extractable N pools (3.7 %), and 13 C-enriched relative to the extractable C pool (2.5 %). The microbial biomass was also 13 C-enriched relative to total C for soils that exhibited a C3-plant signature (1.6 %), but 13 C-depleted for soils with a C4 signature (À1.1 %). The latter was probably associated with an increase of annual C3 forbs in C4 grasslands after an extreme drought. These findings are in agreement with the proposed contribution of microbial products to the stabilized soil organic matter and may help explain the shift in isotope composition during soil organic matter formation. r","publication_date":{"day":null,"month":null,"year":2006,"errors":{}},"publication_name":"Soil Biology and Biochemistry","grobid_abstract_attachment_id":46033085},"translated_abstract":null,"internal_url":"https://www.academia.edu/12640386/13C_and_15N_natural_abundance_of_the_soil_microbial_biomass","translated_internal_url":"","created_at":"2015-05-27T21:28:12.007-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":31619589,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":20739543,"work_id":12640386,"tagging_user_id":31619589,"tagged_user_id":41398316,"co_author_invite_id":null,"email":"m***o@hotmail.com","display_order":0,"name":"O. 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Abundance","url":"https://www.academia.edu/Documents/in/Natural_Abundance"},{"id":1188997,"name":"C","url":"https://www.academia.edu/Documents/in/C"},{"id":2302453,"name":"Soil microbial biomass","url":"https://www.academia.edu/Documents/in/Soil_microbial_biomass"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20540320"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20540320/Effect_of_afforestation_on_N2O_formation_and_consumption_by_ecosystems"><img alt="Research paper thumbnail of Effect of afforestation on N2O formation and consumption by ecosystems" class="work-thumbnail" src="https://attachments.academia-assets.com/41426932/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20540320/Effect_of_afforestation_on_N2O_formation_and_consumption_by_ecosystems">Effect of afforestation on N2O formation and consumption by ecosystems</a></div><div class="wp-workCard_item"><span>Doklady Biological Sciences</span><span>, 2006</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3642a2d1170ab6b8a9f40908dfb17533" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41426932,"asset_id":20540320,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41426932/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20540320"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20540320"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20540320; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=20540320]").text(description); $(".js-view-count[data-work-id=20540320]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget 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It is assumed that carbon accumulation during the formation of forest ecosystems exceeds its emission from soil in the form of ëé 2 . However, the effect of afforestation on the formation and emission of other greenhouse gases ( CH 4 and N 2 O ) has not been considered. Nitrous oxide ( N 2 O ) is one of the most important greenhouse gases and, in addition, makes a contribution to the destruction of the ozone layer . Soil is the main source of N 2 O , it accounts about 60% of its total annual emission into the atmosphere. Denitrification is the main process of N 2 O formation in soil . At the last stage of denitrification, N 2 O may be reduced to molecular nitrogen ( N 2 ). Therefore, the total emission of N 2 O from the soil to the atmosphere is determined by the ratio between the rates of N 2 O formation in the course of denitrification and N 2 O consumption in the same process . 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20540318"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20540318/Denitrification_Potential_and_CO_2_Emission_in_the_Northern_Forest_Soils_of_the_Yenisei_Meridian_the_Siberian_IGBP_Transect_"><img alt="Research paper thumbnail of Denitrification Potential and CO 2 Emission in the Northern Forest Soils of the Yenisei Meridian (the Siberian IGBP Transect)" class="work-thumbnail" src="https://attachments.academia-assets.com/41426933/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20540318/Denitrification_Potential_and_CO_2_Emission_in_the_Northern_Forest_Soils_of_the_Yenisei_Meridian_the_Siberian_IGBP_Transect_">Denitrification Potential and CO 2 Emission in the Northern Forest Soils of the Yenisei Meridian (the Siberian IGBP Transect)</a></div><div class="wp-workCard_item"><span>Biology Bulletin</span><span>, 2003</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="0512486d13abf552600354f38d3e0aea" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41426933,"asset_id":20540318,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41426933/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20540318"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20540318"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20540318; 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Multiple regression models that describe 57% of the variation in denitrification and 97% of the variation in the organic carbon mineralization were developed. It was found that the simulation of potential denitrification activity is a more difficult problem than the simulation of C mineralization. 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Broadleaf species (aspen and birch) proved to have lower rates of N2O consumption compared to coniferous species. The factors influencing production and consumption of N2O were also evaluated. The replacement of coniferous forests with broadleaf trees will double the N2O/N2 ratio in the denitrification end-products. Doubled N2O emission from Siberian forest soils to the atmosphere can be expected due to changes in tree species composition of forest ecosystems even without considering changes in water and temperature regimes in soil.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f6b487526cd6ac09fdfea1be5c4b7071" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":43654256,"asset_id":20540317,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/43654256/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20540317"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20540317"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20540317; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=20540317]").text(description); $(".js-view-count[data-work-id=20540317]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 20540317; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='20540317']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 20540317, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "f6b487526cd6ac09fdfea1be5c4b7071" } } $('.js-work-strip[data-work-id=20540317]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":20540317,"title":"Effect of Siberian tree species on N2O production and consumption","translated_title":"","metadata":{"abstract":"The effect of six Siberian tree species on two stages of denitrification-N2O production and consumption-was studied. Broadleaf species (aspen and birch) proved to have lower rates of N2O consumption compared to coniferous species. The factors influencing production and consumption of N2O were also evaluated. The replacement of coniferous forests with broadleaf trees will double the N2O/N2 ratio in the denitrification end-products. Doubled N2O emission from Siberian forest soils to the atmosphere can be expected due to changes in tree species composition of forest ecosystems even without considering changes in water and temperature regimes in soil.","publication_date":{"day":null,"month":null,"year":2006,"errors":{}},"publication_name":"Biology Bulletin"},"translated_abstract":"The effect of six Siberian tree species on two stages of denitrification-N2O production and consumption-was studied. Broadleaf species (aspen and birch) proved to have lower rates of N2O consumption compared to coniferous species. The factors influencing production and consumption of N2O were also evaluated. The replacement of coniferous forests with broadleaf trees will double the N2O/N2 ratio in the denitrification end-products. Doubled N2O emission from Siberian forest soils to the atmosphere can be expected due to changes in tree species composition of forest ecosystems even without considering changes in water and temperature regimes in soil.","internal_url":"https://www.academia.edu/20540317/Effect_of_Siberian_tree_species_on_N2O_production_and_consumption","translated_internal_url":"","created_at":"2016-01-22T06:17:37.786-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":43654256,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/43654256/thumbnails/1.jpg","file_name":"Izv._RAN_2006.pdf","download_url":"https://www.academia.edu/attachments/43654256/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Effect_of_Siberian_tree_species_on_N2O_p.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/43654256/Izv._RAN_2006-libre.pdf?1457787203=\u0026response-content-disposition=attachment%3B+filename%3DEffect_of_Siberian_tree_species_on_N2O_p.pdf\u0026Expires=1733220925\u0026Signature=B2EiUifz3hGSQ96t0WkP0tyhST5-98R6ogM6Qa-GORirhvwS4fuuOmYRIhA6ZcA3jE1FYo3DpIHlBg4dHi15hbzDsMAmEI8pKvcE8Lwu1Yg0aS3EPkiwV98sH2mbdUg68XsTCeR~UvLn4h7SthvniTOg5ZHPgLiCAinYc0Gx4nlZ4fobisosxH6NO9B48YGmbiaV8q8SbQKQVnu2Ap5NfQibvBVISyZ~YsH839xWjpKfbYYuNPVwr16VpJkN3PrV81G0AjWd~YVQedhrEvNIsDlBnzT0I8MybP8rIA4QHR6Ekq07haKOVPZXDMnVPSWOwNX-cyYkIN~YvgLO~blvqA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Effect_of_Siberian_tree_species_on_N2O_production_and_consumption","translated_slug":"","page_count":6,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20540316"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20540316/The_effect_of_Siberian_tree_species_on_the_mineralization_rate_of_soil_organic_matter"><img alt="Research paper thumbnail of The effect of Siberian tree species on the mineralization rate of soil organic matter" class="work-thumbnail" src="https://attachments.academia-assets.com/41426930/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20540316/The_effect_of_Siberian_tree_species_on_the_mineralization_rate_of_soil_organic_matter">The effect of Siberian tree species on the mineralization rate of soil organic matter</a></div><div class="wp-workCard_item"><span>Eurasian Soil Science</span><span>, 2009</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="688bb9abd29c0905c430d92f3a1f4a4b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41426930,"asset_id":20540316,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41426930/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20540316"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20540316"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20540316; 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The nitrogen mineralization and nitrification were the most affected by the different tree species. The rate of the CO 2 formation was similar in the soils under the different tree species. The factors affecting the variation of the data characterizing the microbiological processes were revealed. The nitrogen mineralization and nitrification correlated with the contents of the soil carbon, nitrogen, and and the soil acidity, while the carbon mineralization correlated only with the concentration and the C/N ratio.","publication_date":{"day":null,"month":null,"year":2009,"errors":{}},"publication_name":"Eurasian Soil Science","grobid_abstract_attachment_id":41426930},"translated_abstract":null,"internal_url":"https://www.academia.edu/20540316/The_effect_of_Siberian_tree_species_on_the_mineralization_rate_of_soil_organic_matter","translated_internal_url":"","created_at":"2016-01-22T06:17:37.644-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":41426930,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/41426930/thumbnails/1.jpg","file_name":"The_effect_of_Siberian_tree_species_on_t20160122-13154-87esdm.pdf","download_url":"https://www.academia.edu/attachments/41426930/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_effect_of_Siberian_tree_species_on_t.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/41426930/The_effect_of_Siberian_tree_species_on_t20160122-13154-87esdm-libre.pdf?1453472977=\u0026response-content-disposition=attachment%3B+filename%3DThe_effect_of_Siberian_tree_species_on_t.pdf\u0026Expires=1733220925\u0026Signature=TFvGiYaWbiTR7r5P9kyRMXASktH56J2brl63EOLeazLh5Qm-0QBL7rcpVr6Eze0S~SO3udqSgt0nKDygQX2FvfZKkZMSW7IJaJuQGwj383FkBiXyC2qNyU1ow7IcYDZCezeg4IqeIFnbSU4SHsvqBUprx3Rs8BC7LJdLeDO4EzLf2hBWPlFbkY2UwjpGYmgrrxqG4N4OZRK4dAfpS77zmSdRYXj3lAiNeyp6UHx48rlxa9jAicN3~ZHW8hDi7VrZ523C9B7QL5YMjKGrXBmlXSe5eFKSbXp-AIVaJ255nGj3VvbDPyi7L~CCDHIQQQsyCMtFVvLiG8IELfsH87iC9A__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_effect_of_Siberian_tree_species_on_the_mineralization_rate_of_soil_organic_matter","translated_slug":"","page_count":7,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20540315"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20540315/The_influence_of_tree_species_on_the_biomass_of_denitrifying_bacteria_in_gray_forest_soils"><img alt="Research paper thumbnail of The influence of tree species on the biomass of denitrifying bacteria in gray forest soils" class="work-thumbnail" src="https://attachments.academia-assets.com/41426929/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20540315/The_influence_of_tree_species_on_the_biomass_of_denitrifying_bacteria_in_gray_forest_soils">The influence of tree species on the biomass of denitrifying bacteria in gray forest soils</a></div><div class="wp-workCard_item"><span>Eurasian Soil Science</span><span>, 2007</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2dc5ab1cd7b48a8b20a49ac4a27a7d4d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41426929,"asset_id":20540315,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41426929/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20540315"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20540315"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20540315; 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The biomass was the highest in the soil of the layland. The lowest (19.4 µ g C/g of soil) biomass of heterotrophic microorganisms was found in the soil under the birch trees, and the highest one (41.7 and 32.0 µ g C/g), under the pine and spruce ones. The biomass of denitrifying microorganisms was lower by thirty times than that of the heterotrophic ones. In the soils under the pine and spruce trees (8.4 and 9.2 µ g C/g, respectively), the biomass of the denitrifying microorganisms was the lowest; under the birch and larch trees, it was the highest (16.7 and 13.7 µ g C/g).","publication_date":{"day":null,"month":null,"year":2007,"errors":{}},"publication_name":"Eurasian Soil Science","grobid_abstract_attachment_id":41426929},"translated_abstract":null,"internal_url":"https://www.academia.edu/20540315/The_influence_of_tree_species_on_the_biomass_of_denitrifying_bacteria_in_gray_forest_soils","translated_internal_url":"","created_at":"2016-01-22T06:17:37.512-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":41426929,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/41426929/thumbnails/1.jpg","file_name":"The_influence_of_tree_species_on_the_bio20160122-13160-l8hukl.pdf","download_url":"https://www.academia.edu/attachments/41426929/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_influence_of_tree_species_on_the_bio.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/41426929/The_influence_of_tree_species_on_the_bio20160122-13160-l8hukl-libre.pdf?1453472977=\u0026response-content-disposition=attachment%3B+filename%3DThe_influence_of_tree_species_on_the_bio.pdf\u0026Expires=1733220925\u0026Signature=fTDPj~Fnyeq6MeNJY6x33~zhrMpfwlul7vFclCKjPapip4pHv7Xhyzcywa8Qgqc6C57ZX19UIjXgafRmyAcC0r5gFmC6-jngIR46puahC4CGJTUOgW49R93u~01~qDJSRRuFsojOTA-vcReXv3ddkMEdzJHuSPNazUKuWvlp9bePywWzv1Nk~Qthm1HVPHsvWsyRcxWRDP22w8d-aX6i42DZmXQ7FXlvwP22SehrHNJy8MvhgmnADSWvjpiJqvxfr1DxjU5udkF~CzNVrKeVoYflLT9VUpYHffXdHszIEn-TYXA3Q8dpag38h3mxT35iMIi1OduaGlYU8-MED0svcw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_influence_of_tree_species_on_the_biomass_of_denitrifying_bacteria_in_gray_forest_soils","translated_slug":"","page_count":6,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="4395985" id="papers"><div class="js-work-strip profile--work_container" data-work-id="108964575"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/108964575/Single_tree_effects_on_denitrification_and_soil_microbial_biomass_in_agroforestry_systems_and_natural_forests_of_the_Amazon_region"><img alt="Research paper thumbnail of Single tree-effects on denitrification and soil microbial biomass in agroforestry systems and natural forests of the Amazon region" class="work-thumbnail" src="https://attachments.academia-assets.com/107218579/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/108964575/Single_tree_effects_on_denitrification_and_soil_microbial_biomass_in_agroforestry_systems_and_natural_forests_of_the_Amazon_region">Single tree-effects on denitrification and soil microbial biomass in agroforestry systems and natural forests of the Amazon region</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The aim of this study was to find the effect of tree species (Theobroma grandiflorum - cupuacu, B...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The aim of this study was to find the effect of tree species (Theobroma grandiflorum - cupuacu, Bixa orellana - urucum, Vismia spp, Carapa guianensis - andiroba, Ceiba pentandra - sumauma) used in agroforestry system in Amazonian region and natural forests on the total biomass of heterotrophic microorganisms (BH), in Manaus-AM (Brasil).</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c65abdddc890c945e3421c261314e377" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":107218579,"asset_id":108964575,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/107218579/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108964575"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108964575"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108964575; 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This study ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Soil CO2 emission is one of the most important components of the global carbon cycle. This study analyzes the seasonal dynamics of soil emission for various land cover types in the middle taiga subzone of central Siberia during five growing seasons. It is shown that, throughout a vast area covered by pine forests and their derivatives formed on sandy soils, seasonal CO2 emission values are determined primarily by the moisture conditions and only secondarily by the temperature regime and ecosystem type. The effect of the forest type is manifested only under the most favorable moisture conditions. A new approach is proposed: divide the growing season into dry and moist periods depending on the threshold soil moisture for areas with different vegetation types.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108964574"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108964574"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108964574; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108964574]").text(description); $(".js-view-count[data-work-id=108964574]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108964574; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108964574']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 108964574, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=108964574]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108964574,"title":"The Impact of Climatic Factors on CО2 Emissions from Soils of Middle-Taiga Forests in Central Siberia: Emission as a Function of Soil Temperature and Moisture","translated_title":"","metadata":{"abstract":"Soil CO2 emission is one of the most important components of the global carbon cycle. This study analyzes the seasonal dynamics of soil emission for various land cover types in the middle taiga subzone of central Siberia during five growing seasons. It is shown that, throughout a vast area covered by pine forests and their derivatives formed on sandy soils, seasonal CO2 emission values are determined primarily by the moisture conditions and only secondarily by the temperature regime and ecosystem type. The effect of the forest type is manifested only under the most favorable moisture conditions. A new approach is proposed: divide the growing season into dry and moist periods depending on the threshold soil moisture for areas with different vegetation types.","publisher":"Pleiades Publishing Ltd","publication_date":{"day":null,"month":null,"year":2020,"errors":{}},"publication_name":"Russian Journal of Ecology"},"translated_abstract":"Soil CO2 emission is one of the most important components of the global carbon cycle. This study analyzes the seasonal dynamics of soil emission for various land cover types in the middle taiga subzone of central Siberia during five growing seasons. It is shown that, throughout a vast area covered by pine forests and their derivatives formed on sandy soils, seasonal CO2 emission values are determined primarily by the moisture conditions and only secondarily by the temperature regime and ecosystem type. The effect of the forest type is manifested only under the most favorable moisture conditions. A new approach is proposed: divide the growing season into dry and moist periods depending on the threshold soil moisture for areas with different vegetation types.","internal_url":"https://www.academia.edu/108964574/The_Impact_of_Climatic_Factors_on_C%D0%9E2_Emissions_from_Soils_of_Middle_Taiga_Forests_in_Central_Siberia_Emission_as_a_Function_of_Soil_Temperature_and_Moisture","translated_internal_url":"","created_at":"2023-11-07T10:41:00.371-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Impact_of_Climatic_Factors_on_CО2_Emissions_from_Soils_of_Middle_Taiga_Forests_in_Central_Siberia_Emission_as_a_Function_of_Soil_Temperature_and_Moisture","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. Menyailo","url":"https://independent.academia.edu/OMenyailo"},"attachments":[],"research_interests":[{"id":402,"name":"Environmental Science","url":"https://www.academia.edu/Documents/in/Environmental_Science"},{"id":9846,"name":"Ecology","url":"https://www.academia.edu/Documents/in/Ecology"},{"id":14719,"name":"Carbon Cycle","url":"https://www.academia.edu/Documents/in/Carbon_Cycle"},{"id":83037,"name":"Soil moisture","url":"https://www.academia.edu/Documents/in/Soil_moisture"},{"id":133176,"name":"Moisture","url":"https://www.academia.edu/Documents/in/Moisture"},{"id":278441,"name":"Soil Temperature","url":"https://www.academia.edu/Documents/in/Soil_Temperature"},{"id":373754,"name":"Ecosystem","url":"https://www.academia.edu/Documents/in/Ecosystem"},{"id":845678,"name":"Water Content","url":"https://www.academia.edu/Documents/in/Water_Content"},{"id":1222799,"name":"Soil Water","url":"https://www.academia.edu/Documents/in/Soil_Water"},{"id":1648025,"name":"Taiga","url":"https://www.academia.edu/Documents/in/Taiga"},{"id":2904182,"name":"Middle Taiga","url":"https://www.academia.edu/Documents/in/Middle_Taiga"}],"urls":[{"id":35254849,"url":"http://link.springer.com/content/pdf/10.1134/S1067413620010063.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="108964573"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/108964573/13C_and_15N_natural_abundance_of_the_soil_microbial_biomass"><img alt="Research paper thumbnail of 13C and 15N natural abundance of the soil microbial biomass" class="work-thumbnail" src="https://attachments.academia-assets.com/107218584/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/108964573/13C_and_15N_natural_abundance_of_the_soil_microbial_biomass">13C and 15N natural abundance of the soil microbial biomass</a></div><div class="wp-workCard_item"><span>Soil Biology and Biochemistry</span><span>, 2006</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="7289ea94c52452d21d922bd956d62fd4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":107218584,"asset_id":108964573,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/107218584/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108964573"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108964573"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108964573; 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It is often observed that more decomposed soil organic matter is 13 C, and especially 15 N-enriched relative to fresh litter and recent organic matter. We investigated whether this shift in isotope composition relates to the isotope composition of the microbial biomass, an important source for soil organic matter. We developed a new approach to determine the natural abundance C and N isotope composition of the microbial biomass across a broad range of soil types, vegetation, and climates. We found consistently that the soil microbial biomass was 15 N-enriched relative to the total (3.2 %) and extractable N pools (3.7 %), and 13 C-enriched relative to the extractable C pool (2.5 %). The microbial biomass was also 13 C-enriched relative to total C for soils that exhibited a C3-plant signature (1.6 %), but 13 C-depleted for soils with a C4 signature (À1.1 %). The latter was probably associated with an increase of annual C3 forbs in C4 grasslands after an extreme drought. These findings are in agreement with the proposed contribution of microbial products to the stabilized soil organic matter and may help explain the shift in isotope composition during soil organic matter formation.","publication_date":{"day":null,"month":null,"year":2006,"errors":{}},"publication_name":"Soil Biology and Biochemistry","grobid_abstract_attachment_id":107218584},"translated_abstract":null,"internal_url":"https://www.academia.edu/108964573/13C_and_15N_natural_abundance_of_the_soil_microbial_biomass","translated_internal_url":"","created_at":"2023-11-07T10:40:59.108-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":107218584,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/107218584/thumbnails/1.jpg","file_name":"0912f50b9a620c4b87000000.pdf","download_url":"https://www.academia.edu/attachments/107218584/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"13C_and_15N_natural_abundance_of_the_soi.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/107218584/0912f50b9a620c4b87000000-libre.pdf?1699382709=\u0026response-content-disposition=attachment%3B+filename%3D13C_and_15N_natural_abundance_of_the_soi.pdf\u0026Expires=1733220925\u0026Signature=F060xSCAI58SiCDFx67GnvYqgqdM8a5LTdNerhWIWXmuQAL00NxHAeO2GbOO8ou0YVPLygGltd3wWb5laf5KbE9O15a7Wn9sCDiuhcnKN42Noez5THJlWF1Wr45zoKWpy1I6ch6C67Joh2byiiRPNOP-8NNXhsj6yIS9D4CPWDh9d-0svZCnaPceGMSM-xLPCDDjHGrsYQLQJEmtbXIrlgbkjm0h8DTyElU6GcF1BtyqsKta3hhxVMsJYVx5baABoWj285NEnKZ~SsLb~JSur9a5QM16GRtPHwwAcrA37~xoOkNbtwnzHO2ALMl8UpGMZcEMDYdnlfiMeFyg4YU~iw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"13C_and_15N_natural_abundance_of_the_soil_microbial_biomass","translated_slug":"","page_count":10,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="108964572"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/108964572/Age_Dependent_Changes_in_Soil_Respiration_and_Associated_Parameters_in_Siberian_Permafrost_Larch_Stands_Affected_by_Wildfire"><img alt="Research paper thumbnail of Age-Dependent Changes in Soil Respiration and Associated Parameters in Siberian Permafrost Larch Stands Affected by Wildfire" class="work-thumbnail" src="https://attachments.academia-assets.com/107218572/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/108964572/Age_Dependent_Changes_in_Soil_Respiration_and_Associated_Parameters_in_Siberian_Permafrost_Larch_Stands_Affected_by_Wildfire">Age-Dependent Changes in Soil Respiration and Associated Parameters in Siberian Permafrost Larch Stands Affected by Wildfire</a></div><div class="wp-workCard_item"><span>Forests</span><span>, 2021</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The observed high spatial variation in soil respiration (SR) and associated parameters emphasized...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The observed high spatial variation in soil respiration (SR) and associated parameters emphasized the importance of SR heterogeneity at high latitudes and the involvement of many factors in its regulation, especially within fire-affected areas. The problem of estimating CO2 emissions during post-fire recovery in high-latitude ecosystems addresses the mutual influence of wildfires and climate change on the C cycle. Despite its importance, especially in permafrost regions because of their vulnerability, the mutual influence of these factors on CO2 dynamics has rarely been studied. Thus, we aimed to understand the dynamics of soil respiration (SR) in wildfire-affected larch recovery successions. We analyzed 16-year data (1995–2010) on SR and associated soil, biological, and environmental parameters obtained during several field studies in larch stands of different ages (0–276 years) in the Krasnoyarsk region (Russia). We observed a high variation in SR and related parameters among the ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="591626014d28112e4a3267d219a876b4" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":107218572,"asset_id":108964572,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/107218572/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="108964572"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="108964572"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 108964572; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=108964572]").text(description); $(".js-view-count[data-work-id=108964572]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 108964572; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='108964572']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 108964572, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "591626014d28112e4a3267d219a876b4" } } $('.js-work-strip[data-work-id=108964572]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":108964572,"title":"Age-Dependent Changes in Soil Respiration and Associated Parameters in Siberian Permafrost Larch Stands Affected by Wildfire","translated_title":"","metadata":{"abstract":"The observed high spatial variation in soil respiration (SR) and associated parameters emphasized the importance of SR heterogeneity at high latitudes and the involvement of many factors in its regulation, especially within fire-affected areas. The problem of estimating CO2 emissions during post-fire recovery in high-latitude ecosystems addresses the mutual influence of wildfires and climate change on the C cycle. Despite its importance, especially in permafrost regions because of their vulnerability, the mutual influence of these factors on CO2 dynamics has rarely been studied. Thus, we aimed to understand the dynamics of soil respiration (SR) in wildfire-affected larch recovery successions. We analyzed 16-year data (1995–2010) on SR and associated soil, biological, and environmental parameters obtained during several field studies in larch stands of different ages (0–276 years) in the Krasnoyarsk region (Russia). We observed a high variation in SR and related parameters among the ...","publisher":"MDPI AG","publication_date":{"day":null,"month":null,"year":2021,"errors":{}},"publication_name":"Forests"},"translated_abstract":"The observed high spatial variation in soil respiration (SR) and associated parameters emphasized the importance of SR heterogeneity at high latitudes and the involvement of many factors in its regulation, especially within fire-affected areas. The problem of estimating CO2 emissions during post-fire recovery in high-latitude ecosystems addresses the mutual influence of wildfires and climate change on the C cycle. Despite its importance, especially in permafrost regions because of their vulnerability, the mutual influence of these factors on CO2 dynamics has rarely been studied. Thus, we aimed to understand the dynamics of soil respiration (SR) in wildfire-affected larch recovery successions. We analyzed 16-year data (1995–2010) on SR and associated soil, biological, and environmental parameters obtained during several field studies in larch stands of different ages (0–276 years) in the Krasnoyarsk region (Russia). 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Tree species effects on soil sources of N2O" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/95813351/A_new_method_of_quantifying_contributions_from_nitrification_and_denitrification_Tree_species_effects_on_soil_sources_of_N2O">A new method of quantifying contributions from nitrification and denitrification. Tree species effects on soil sources of N2O</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Soil microorganisms produce N2O through denitrification and nitrification. Here we propose the ne...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Soil microorganisms produce N2O through denitrification and nitrification. Here we propose the new method to accurately distinguish contributions of nitrification or denitrification to the N2O production. This method is based on the application of the NH4NO3 (substrate for both processes) with low level of oxygen isotopes enrichment (ca. 1.6 atom excess, %). During nitrification, the first atom of oxygen in nitrous oxide derives from atmospheric O2 and the second from H2O, while in denitrification, all oxygen atoms of the formed N2O originate from oxygen of NO3-. Thus applying enriched 18O-NO3- and measuring 18O-N2O thereafter it is possible to distinguish the two processes. We used the Siberian afforestation experiment with six dominant in Siberia tree species grown artificially for about 30 y on initially homogeneous soil. The soil samples from all species were incubated at the two moisture levels to test whether the isotopic signatures of oxygen in N2O will be more enriched at hi...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="95813351"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="95813351"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 95813351; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=95813351]").text(description); $(".js-view-count[data-work-id=95813351]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 95813351; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='95813351']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 95813351, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=95813351]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":95813351,"title":"A new method of quantifying contributions from nitrification and denitrification. 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The soil samples from all species were incubated at the two moisture levels to test whether the isotopic signatures of oxygen in N2O will be more enriched at hi..."},"translated_abstract":"Soil microorganisms produce N2O through denitrification and nitrification. Here we propose the new method to accurately distinguish contributions of nitrification or denitrification to the N2O production. This method is based on the application of the NH4NO3 (substrate for both processes) with low level of oxygen isotopes enrichment (ca. 1.6 atom excess, %). During nitrification, the first atom of oxygen in nitrous oxide derives from atmospheric O2 and the second from H2O, while in denitrification, all oxygen atoms of the formed N2O originate from oxygen of NO3-. Thus applying enriched 18O-NO3- and measuring 18O-N2O thereafter it is possible to distinguish the two processes. We used the Siberian afforestation experiment with six dominant in Siberia tree species grown artificially for about 30 y on initially homogeneous soil. The soil samples from all species were incubated at the two moisture levels to test whether the isotopic signatures of oxygen in N2O will be more enriched at hi...","internal_url":"https://www.academia.edu/95813351/A_new_method_of_quantifying_contributions_from_nitrification_and_denitrification_Tree_species_effects_on_soil_sources_of_N2O","translated_internal_url":"","created_at":"2023-01-27T12:05:23.850-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"A_new_method_of_quantifying_contributions_from_nitrification_and_denitrification_Tree_species_effects_on_soil_sources_of_N2O","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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It is shown that N transformation in meadow-alpine soils (Leptic Umbrisols) of the northwestern Caucasus (Teberda Reserve, Karachay-Cherkess Republic) leads to well-expressed differences in isotopic signatures of different N compounds: δ15N of extractable organic matter &gt; δ15Ntotal &gt; δ15N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NH}}_{{\text{4}}}^{ + }$$\end{document} &gt; δ15N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NO}}_{{\text{3}}}^{ - }.$$\end{document} The range of δ15N in this sequence reaches 25‰. Differences in δ15N within the same pool of N in soils of different alpine ecosystems, as well as seasonal dynamics of δ15N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NH}}_{{\text{4}}}^{ + },$$\end{document} are much less pronounced (the range of δ15N is 2–4‰). The values of δ15Ntotal and δ15N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NH}}_{{\text{4}}}^{ + }$$\end{document} positively correlate with N mineralization and nitrification and demonstrate the accumulation of heavy N isotope in soils of the alpine ecosystems with more active N transformation processes. Obviously, nitrification is the key process controlling the isotopic signature of N–\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${\text{NH}}_{{\text{4}}}^{ + }.$$\end{document} The role of N mineralization in the fractionation of N isotopes is less obvious, and 15N accumulation in the extractable organic matter can be related to the significant content of “heavy” microbial N in extractable organic N pool.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="78568964"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="78568964"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 78568964; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=78568964]").text(description); $(".js-view-count[data-work-id=78568964]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 78568964; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='78568964']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 78568964, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=78568964]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":78568964,"title":"Isotopic Composition of Nitrogen and Transformation of Nitrogen Compounds in Meadow-Alpine Soils","translated_title":"","metadata":{"abstract":"Isotopic composition of nitrogen in soils can be an informative indicator of N transformation processes and sources of N nutrition of plants, but data on δ15N of labile N compounds are scarce. 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It is shown that N transformation in meadow-alpine soils (Leptic Umbrisols) of the northwestern Caucasus (Teberda Reserve, Karachay-Cherkess Republic) leads to well-expressed differences in isotopic signatures of different N compounds: δ15N of extractable organic matter \u0026gt; δ15Ntotal \u0026gt; δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + }$$\\end{document} \u0026gt; δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NO}}_{{\\text{3}}}^{ - }.$$\\end{document} The range of δ15N in this sequence reaches 25‰. Differences in δ15N within the same pool of N in soils of different alpine ecosystems, as well as seasonal dynamics of δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + },$$\\end{document} are much less pronounced (the range of δ15N is 2–4‰). The values of δ15Ntotal and δ15N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + }$$\\end{document} positively correlate with N mineralization and nitrification and demonstrate the accumulation of heavy N isotope in soils of the alpine ecosystems with more active N transformation processes. Obviously, nitrification is the key process controlling the isotopic signature of N–\\documentclass[12pt]{minimal} \\usepackage{amsmath} \\usepackage{wasysym} \\usepackage{amsfonts} \\usepackage{amssymb} \\usepackage{amsbsy} \\usepackage{mathrsfs} \\usepackage{upgreek} \\setlength{\\oddsidemargin}{-69pt} \\begin{document}$${\\text{NH}}_{{\\text{4}}}^{ + }.$$\\end{document} The role of N mineralization in the fractionation of N isotopes is less obvious, and 15N accumulation in the extractable organic matter can be related to the significant content of “heavy” microbial N in extractable organic N pool.","internal_url":"https://www.academia.edu/78568964/Isotopic_Composition_of_Nitrogen_and_Transformation_of_Nitrogen_Compounds_in_Meadow_Alpine_Soils","translated_internal_url":"","created_at":"2022-05-05T22:52:43.203-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Isotopic_Composition_of_Nitrogen_and_Transformation_of_Nitrogen_Compounds_in_Meadow_Alpine_Soils","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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It has been shown that the ericaceous dwarf shrub Vaccinium vitis-idaea characterized by ericoid mycorrhiza, which releases oxidative and hydrolytic enzymes into the soil, has an effect on the properties of mountain-meadow soil in the alpine phytocenosis. In the presence of V. vitis-idaea, the soil is characterized by increased acidity; higher contents of labile organic matter carbon, microbial biomass nitrogen, and available phosphorus; and higher microbial activity.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="78568963"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="78568963"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 78568963; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=78568963]").text(description); $(".js-view-count[data-work-id=78568963]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 78568963; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='78568963']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 78568963, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=78568963]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":78568963,"title":"The Effect of Vaccinium vitis-idaea on Properties of Mountain-Meadow Soil under Alpine Lichen Heath","translated_title":"","metadata":{"abstract":"Abstract—The study of the effect of mycorrhiza symbiosis on the transformation of carbon and nitrogen compounds in soils is important in view of the necessity to predict variations in the cycles of nutrients under changing environmental conditions. It has been shown that the ericaceous dwarf shrub Vaccinium vitis-idaea characterized by ericoid mycorrhiza, which releases oxidative and hydrolytic enzymes into the soil, has an effect on the properties of mountain-meadow soil in the alpine phytocenosis. In the presence of V. vitis-idaea, the soil is characterized by increased acidity; higher contents of labile organic matter carbon, microbial biomass nitrogen, and available phosphorus; and higher microbial activity.","publisher":"Pleiades Publishing Ltd","publication_date":{"day":null,"month":null,"year":2019,"errors":{}},"publication_name":"Russian Journal of Ecology"},"translated_abstract":"Abstract—The study of the effect of mycorrhiza symbiosis on the transformation of carbon and nitrogen compounds in soils is important in view of the necessity to predict variations in the cycles of nutrients under changing environmental conditions. It has been shown that the ericaceous dwarf shrub Vaccinium vitis-idaea characterized by ericoid mycorrhiza, which releases oxidative and hydrolytic enzymes into the soil, has an effect on the properties of mountain-meadow soil in the alpine phytocenosis. In the presence of V. vitis-idaea, the soil is characterized by increased acidity; higher contents of labile organic matter carbon, microbial biomass nitrogen, and available phosphorus; and higher microbial activity.","internal_url":"https://www.academia.edu/78568963/The_Effect_of_Vaccinium_vitis_idaea_on_Properties_of_Mountain_Meadow_Soil_under_Alpine_Lichen_Heath","translated_internal_url":"","created_at":"2022-05-05T22:52:42.991-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"The_Effect_of_Vaccinium_vitis_idaea_on_Properties_of_Mountain_Meadow_Soil_under_Alpine_Lichen_Heath","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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The fumigation-extraction and substrate-induced respiration methods give similar results for Albic Luvisol and Gleyic Fluvisol, while the results of the rehydration method are reliably higher. In Histic Fluvisol, relatively similar results are obtained using the fumigation-extraction and rehydration methods, and the substrate-induced respiration method gives almost halved results. The seasonal dynamics of microbial biomass carbon also varies depending on the method used. The highest difference is typical for the warm period, when the concentrations found by the extraction and substrate-induced methods poorly agree between two out of three soils studied. The concentration of microbial biomass nitrogen is less sensitive to the analytical method: the differences between the results of the fumigation-extraction and rehydration methods are statistically insignificant in the all soils. To reveal stable relationships between the results of determining microbial carbon and the soil properties and analytical method, a large diversity of soils should be studied. This will allow for proposing of conversion factors for the recalculation of the obtained values to the concentrations of carbon and nitrogen in microbial biomass for different soils (or soil groups) and, hence, the more correct comparison of the results obtained by different methods.","publication_date":{"day":null,"month":null,"year":2016,"errors":{}},"publication_name":"Eurasian Soil Science","grobid_abstract_attachment_id":85572108},"translated_abstract":null,"internal_url":"https://www.academia.edu/78568962/Determination_of_carbon_and_nitrogen_in_microbial_biomass_of_southern_Taiga_soils_by_different_methods","translated_internal_url":"","created_at":"2022-05-05T22:52:42.825-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":85572108,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/85572108/thumbnails/1.jpg","file_name":"10.1134s1064229316060053.pdf","download_url":"https://www.academia.edu/attachments/85572108/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Determination_of_carbon_and_nitrogen_in.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/85572108/10.1134s1064229316060053-libre.pdf?1651817168=\u0026response-content-disposition=attachment%3B+filename%3DDetermination_of_carbon_and_nitrogen_in.pdf\u0026Expires=1733220925\u0026Signature=dlFW9EhLRH4ysqFM9G8qvrhRXp84bLQ~cA6qmPbj7oHB61bjJG~By8~1DzPlila8tDnL--G43KkK7QECOauox9uk24vhWx~5yT4wN-MlGsdhyuCTq8nGHguFGQ-9dT8zOYAON2xGRWIZR3yN1cRvwVmkJulfTYE~VrkQ0KQ54LnZON0fpopLOuN4FdIB41Koi1npIwpN3HxbqrdXIgqkWl5D6P18kwVq8v5xppSAW2z7GrdudFNAQXnNi2SJJNHWAy32FeC8nw9WOiBPLuvMxIqEM2NBWVSD4BJ4ejLZ4ab9gKMjgpc6ft6hfdMzwrBG3rlRIsboLIP8QZFkmPeZrQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Determination_of_carbon_and_nitrogen_in_microbial_biomass_of_southern_Taiga_soils_by_different_methods","translated_slug":"","page_count":11,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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Menyailo</a></span></div><div class="wp-workCard_item"><span>Soil Biology and Biochemistry</span><span>, 2006</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f60a4b46ab2fecca2950d0a7ba1f5b3a" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":46033085,"asset_id":12640386,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/46033085/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="12640386"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="12640386"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 12640386; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=12640386]").text(description); $(".js-view-count[data-work-id=12640386]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 12640386; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='12640386']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 12640386, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "f60a4b46ab2fecca2950d0a7ba1f5b3a" } } $('.js-work-strip[data-work-id=12640386]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":12640386,"title":"13C and 15N natural abundance of the soil microbial biomass","translated_title":"","metadata":{"grobid_abstract":"Stable isotope analysis is a powerful tool in the study of soil organic matter formation. It is often observed that more decomposed soil organic matter is 13 C, and especially 15 N-enriched relative to fresh litter and recent organic matter. We investigated whether this shift in isotope composition relates to the isotope composition of the microbial biomass, an important source for soil organic matter. We developed a new approach to determine the natural abundance C and N isotope composition of the microbial biomass across a broad range of soil types, vegetation, and climates. We found consistently that the soil microbial biomass was 15 N-enriched relative to the total (3.2 %) and extractable N pools (3.7 %), and 13 C-enriched relative to the extractable C pool (2.5 %). The microbial biomass was also 13 C-enriched relative to total C for soils that exhibited a C3-plant signature (1.6 %), but 13 C-depleted for soils with a C4 signature (À1.1 %). The latter was probably associated with an increase of annual C3 forbs in C4 grasslands after an extreme drought. These findings are in agreement with the proposed contribution of microbial products to the stabilized soil organic matter and may help explain the shift in isotope composition during soil organic matter formation. r","publication_date":{"day":null,"month":null,"year":2006,"errors":{}},"publication_name":"Soil Biology and Biochemistry","grobid_abstract_attachment_id":46033085},"translated_abstract":null,"internal_url":"https://www.academia.edu/12640386/13C_and_15N_natural_abundance_of_the_soil_microbial_biomass","translated_internal_url":"","created_at":"2015-05-27T21:28:12.007-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":31619589,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[{"id":20739543,"work_id":12640386,"tagging_user_id":31619589,"tagged_user_id":41398316,"co_author_invite_id":null,"email":"m***o@hotmail.com","display_order":0,"name":"O. 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wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20540320/Effect_of_afforestation_on_N2O_formation_and_consumption_by_ecosystems">Effect of afforestation on N2O formation and consumption by ecosystems</a></div><div class="wp-workCard_item"><span>Doklady Biological Sciences</span><span>, 2006</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3642a2d1170ab6b8a9f40908dfb17533" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41426932,"asset_id":20540320,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41426932/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa 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It is assumed that carbon accumulation during the formation of forest ecosystems exceeds its emission from soil in the form of ëé 2 . However, the effect of afforestation on the formation and emission of other greenhouse gases ( CH 4 and N 2 O ) has not been considered. Nitrous oxide ( N 2 O ) is one of the most important greenhouse gases and, in addition, makes a contribution to the destruction of the ozone layer . Soil is the main source of N 2 O , it accounts about 60% of its total annual emission into the atmosphere. Denitrification is the main process of N 2 O formation in soil . At the last stage of denitrification, N 2 O may be reduced to molecular nitrogen ( N 2 ). Therefore, the total emission of N 2 O from the soil to the atmosphere is determined by the ratio between the rates of N 2 O formation in the course of denitrification and N 2 O consumption in the same process . The higher the ratio between the rates of two stages of denitrification ( N 2 O formation to N 2 O consumption) in the soil, the higher the N 2 O emission.","publication_date":{"day":null,"month":null,"year":2006,"errors":{}},"publication_name":"Doklady Biological Sciences","grobid_abstract_attachment_id":41426932},"translated_abstract":null,"internal_url":"https://www.academia.edu/20540320/Effect_of_afforestation_on_N2O_formation_and_consumption_by_ecosystems","translated_internal_url":"","created_at":"2016-01-22T06:17:38.299-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":41426932,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/41426932/thumbnails/1.jpg","file_name":"Effect_of_afforestation_on_N2O_formation20160122-22091-118m8ps.pdf","download_url":"https://www.academia.edu/attachments/41426932/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Effect_of_afforestation_on_N2O_formation.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/41426932/Effect_of_afforestation_on_N2O_formation20160122-22091-118m8ps-libre.pdf?1453472976=\u0026response-content-disposition=attachment%3B+filename%3DEffect_of_afforestation_on_N2O_formation.pdf\u0026Expires=1733220925\u0026Signature=LN6KcrDsANHQB8v8cSzWmXF-nvSFdN8d~B4q7qIac1EOOgOfOH4Ph77~hXVagMbKK5WBU11j3P-N9qMo2mxnUc1MnzBQEgBXdEcbxqX7nfCYIBG2S4tkoc2wv~6J9g0iTuLE0mUFU-v8es0sxUYV9Hdny67-ntbcnxJTDeVTQR9KwZi8AqZXVvFUTzcpdLxnJ7Kk8mpGbwZWUPLmkLj5kAWiGeSdgmMbxixXCRtSV8SSLqA-0NK2trweJ-2yyxtDauaZ0B13Hw6aqDxJySCmw9t1Vz5x9Cp1sElJbYmcliuhuple0VX4VbtDyNk3lkl1Uvnv15gshnaPjsk2VD1jew__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Effect_of_afforestation_on_N2O_formation_and_consumption_by_ecosystems","translated_slug":"","page_count":3,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20540319"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20540319/The_effect_of_afforestation_on_mineralization_of_soil_organic_matter"><img alt="Research paper thumbnail of The effect of afforestation on mineralization of soil organic matter" class="work-thumbnail" src="https://attachments.academia-assets.com/41948230/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20540319/The_effect_of_afforestation_on_mineralization_of_soil_organic_matter">The effect of afforestation on mineralization of soil organic matter</a></div><div class="wp-workCard_item"><span>Russian Journal of Ecology</span><span>, 2008</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="29ed28797f947317ff160423828f95b1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41948230,"asset_id":20540319,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41948230/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20540319"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20540319"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20540319; 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The results show that this effect concerns mainly net nitrogen mineralization and net nitrification, while carbon mineralization ( CO 2 formation) does not depend on the type of ecosystem. It is proposed to use the rates of net nitrogen mineralization and nitrification as the most sensitive indicators of changes in an ecosystem.","publication_date":{"day":null,"month":null,"year":2008,"errors":{}},"publication_name":"Russian Journal of Ecology","grobid_abstract_attachment_id":41948230},"translated_abstract":null,"internal_url":"https://www.academia.edu/20540319/The_effect_of_afforestation_on_mineralization_of_soil_organic_matter","translated_internal_url":"","created_at":"2016-01-22T06:17:38.174-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":41948230,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/41948230/thumbnails/1.jpg","file_name":"s1067413608010049.pdf20160203-21626-1f3jqkg","download_url":"https://www.academia.edu/attachments/41948230/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"The_effect_of_afforestation_on_mineraliz.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/41948230/s1067413608010049-libre.pdf20160203-21626-1f3jqkg?1454506385=\u0026response-content-disposition=attachment%3B+filename%3DThe_effect_of_afforestation_on_mineraliz.pdf\u0026Expires=1733220925\u0026Signature=MItAaAvfVCR4A4kQ9YLNxYaPUj4JJ1JoXOz8GMft4kQYOWFw8iEKwL4N4za92vhmNsDPT2BpofoIWKihmof-vnOUk7RUj1so-r2wSdSfHSDz6Q--XClb-22B~MGAKorVaAB5i7cws-6EdxcjGGufShmhNDlHgm3xSjA96f9z-GYlXnUfYah0iHJOmSbp5MCBaEtfXVcyom3oq5UYLZUrG~qfHTmeGTHsLZfIl5dQUy8lVKwY1I1NVD3yk7pzt88QBVpTNRKvn5eoqSgHVJ9N-silsHKZ~eWwMjgNcL6mQKlRMN9P8vpu6jMxWY8KdX3y~zhVM-lUEVIFT6cgJnfx-A__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"The_effect_of_afforestation_on_mineralization_of_soil_organic_matter","translated_slug":"","page_count":5,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20540318"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20540318/Denitrification_Potential_and_CO_2_Emission_in_the_Northern_Forest_Soils_of_the_Yenisei_Meridian_the_Siberian_IGBP_Transect_"><img alt="Research paper thumbnail of Denitrification Potential and CO 2 Emission in the Northern Forest Soils of the Yenisei Meridian (the Siberian IGBP Transect)" class="work-thumbnail" src="https://attachments.academia-assets.com/41426933/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20540318/Denitrification_Potential_and_CO_2_Emission_in_the_Northern_Forest_Soils_of_the_Yenisei_Meridian_the_Siberian_IGBP_Transect_">Denitrification Potential and CO 2 Emission in the Northern Forest Soils of the Yenisei Meridian (the Siberian IGBP Transect)</a></div><div class="wp-workCard_item"><span>Biology Bulletin</span><span>, 2003</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="0512486d13abf552600354f38d3e0aea" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41426933,"asset_id":20540318,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41426933/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20540318"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20540318"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20540318; 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Application of the orthogonal regression method proved that the fluxes of CO 2 and N 2 O depend on the content of exchangeable cations in the soil (12-17% of the variability); the effect of soil acidity and the organic matter content is shown to be more significant (74-75% of the variability).","publication_date":{"day":null,"month":null,"year":2003,"errors":{}},"publication_name":"Biology Bulletin","grobid_abstract_attachment_id":41426933},"translated_abstract":null,"internal_url":"https://www.academia.edu/20540318/Denitrification_Potential_and_CO_2_Emission_in_the_Northern_Forest_Soils_of_the_Yenisei_Meridian_the_Siberian_IGBP_Transect_","translated_internal_url":"","created_at":"2016-01-22T06:17:37.944-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":41426933,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/41426933/thumbnails/1.jpg","file_name":"Denitrification_Potential_and_CO2_Emissi20160122-30626-1k7vem5.pdf","download_url":"https://www.academia.edu/attachments/41426933/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Denitrification_Potential_and_CO_2_Emiss.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/41426933/Denitrification_Potential_and_CO2_Emissi20160122-30626-1k7vem5-libre.pdf?1453472977=\u0026response-content-disposition=attachment%3B+filename%3DDenitrification_Potential_and_CO_2_Emiss.pdf\u0026Expires=1733220925\u0026Signature=WaQGkFshmT7JxHIHSctdWQ21cr-fwNyWoTdW91ScDi~LLruQ-HseJm9366rQYMs3cTbwK~j1mTi3BRPdmIcxvrTRKi5LBzhywxWdma0Svf~a3ISre0DuvQPUgFrLDZxTVaSOKz~DUChqXZDFSrCOW91ZpNROcxA9XRpRQNjAoqb5zrHkkHUagOXdPp4aln2R~yC6zKjFxrJKxTO~w~VmWb0IynvP3V8sTusEvcGz5w8EqC92gC4LBGwfJiy5uJdg62LoGARJq9hZu~QGdoRv4BAkOhcVLJ8CuB~wipCGgrS0qtOphDPFbuCKLU4I1KK3jJo-w9-39cKsaa4EGWRBbA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Denitrification_Potential_and_CO_2_Emission_in_the_Northern_Forest_Soils_of_the_Yenisei_Meridian_the_Siberian_IGBP_Transect_","translated_slug":"","page_count":8,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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Broadleaf species (aspen and birch) proved to have lower rates of N2O consumption compared to coniferous species. The factors influencing production and consumption of N2O were also evaluated. The replacement of coniferous forests with broadleaf trees will double the N2O/N2 ratio in the denitrification end-products. Doubled N2O emission from Siberian forest soils to the atmosphere can be expected due to changes in tree species composition of forest ecosystems even without considering changes in water and temperature regimes in soil.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f6b487526cd6ac09fdfea1be5c4b7071" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":43654256,"asset_id":20540317,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/43654256/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20540317"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20540317"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20540317; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=20540317]").text(description); $(".js-view-count[data-work-id=20540317]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 20540317; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='20540317']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 20540317, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "f6b487526cd6ac09fdfea1be5c4b7071" } } $('.js-work-strip[data-work-id=20540317]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":20540317,"title":"Effect of Siberian tree species on N2O production and consumption","translated_title":"","metadata":{"abstract":"The effect of six Siberian tree species on two stages of denitrification-N2O production and consumption-was studied. Broadleaf species (aspen and birch) proved to have lower rates of N2O consumption compared to coniferous species. The factors influencing production and consumption of N2O were also evaluated. The replacement of coniferous forests with broadleaf trees will double the N2O/N2 ratio in the denitrification end-products. Doubled N2O emission from Siberian forest soils to the atmosphere can be expected due to changes in tree species composition of forest ecosystems even without considering changes in water and temperature regimes in soil.","publication_date":{"day":null,"month":null,"year":2006,"errors":{}},"publication_name":"Biology Bulletin"},"translated_abstract":"The effect of six Siberian tree species on two stages of denitrification-N2O production and consumption-was studied. Broadleaf species (aspen and birch) proved to have lower rates of N2O consumption compared to coniferous species. The factors influencing production and consumption of N2O were also evaluated. The replacement of coniferous forests with broadleaf trees will double the N2O/N2 ratio in the denitrification end-products. Doubled N2O emission from Siberian forest soils to the atmosphere can be expected due to changes in tree species composition of forest ecosystems even without considering changes in water and temperature regimes in soil.","internal_url":"https://www.academia.edu/20540317/Effect_of_Siberian_tree_species_on_N2O_production_and_consumption","translated_internal_url":"","created_at":"2016-01-22T06:17:37.786-08:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":41398316,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":43654256,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/43654256/thumbnails/1.jpg","file_name":"Izv._RAN_2006.pdf","download_url":"https://www.academia.edu/attachments/43654256/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Effect_of_Siberian_tree_species_on_N2O_p.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/43654256/Izv._RAN_2006-libre.pdf?1457787203=\u0026response-content-disposition=attachment%3B+filename%3DEffect_of_Siberian_tree_species_on_N2O_p.pdf\u0026Expires=1733220925\u0026Signature=B2EiUifz3hGSQ96t0WkP0tyhST5-98R6ogM6Qa-GORirhvwS4fuuOmYRIhA6ZcA3jE1FYo3DpIHlBg4dHi15hbzDsMAmEI8pKvcE8Lwu1Yg0aS3EPkiwV98sH2mbdUg68XsTCeR~UvLn4h7SthvniTOg5ZHPgLiCAinYc0Gx4nlZ4fobisosxH6NO9B48YGmbiaV8q8SbQKQVnu2Ap5NfQibvBVISyZ~YsH839xWjpKfbYYuNPVwr16VpJkN3PrV81G0AjWd~YVQedhrEvNIsDlBnzT0I8MybP8rIA4QHR6Ekq07haKOVPZXDMnVPSWOwNX-cyYkIN~YvgLO~blvqA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Effect_of_Siberian_tree_species_on_N2O_production_and_consumption","translated_slug":"","page_count":6,"language":"en","content_type":"Work","owner":{"id":41398316,"first_name":"O.","middle_initials":null,"last_name":"Menyailo","page_name":"OMenyailo","domain_name":"independent","created_at":"2016-01-13T02:29:24.406-08:00","display_name":"O. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20540315"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20540315/The_influence_of_tree_species_on_the_biomass_of_denitrifying_bacteria_in_gray_forest_soils"><img alt="Research paper thumbnail of The influence of tree species on the biomass of denitrifying bacteria in gray forest soils" class="work-thumbnail" src="https://attachments.academia-assets.com/41426929/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20540315/The_influence_of_tree_species_on_the_biomass_of_denitrifying_bacteria_in_gray_forest_soils">The influence of tree species on the biomass of denitrifying bacteria in gray forest soils</a></div><div class="wp-workCard_item"><span>Eurasian Soil Science</span><span>, 2007</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="2dc5ab1cd7b48a8b20a49ac4a27a7d4d" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41426929,"asset_id":20540315,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41426929/download_file?st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&st=MTczMzIxNzMyNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20540315"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20540315"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20540315; 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The biomass was the highest in the soil of the layland. The lowest (19.4 µ g C/g of soil) biomass of heterotrophic microorganisms was found in the soil under the birch trees, and the highest one (41.7 and 32.0 µ g C/g), under the pine and spruce ones. The biomass of denitrifying microorganisms was lower by thirty times than that of the heterotrophic ones. 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