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Watershed is the basic land unit for" /> <title>(PDF) IRJET- Quantitative Morphometric Analysis of Adhala basin, Ahmednagar Maharashtra Using Arc-GIS Tool | IRJET Journal - Academia.edu</title> <link rel="canonical" href="https://www.academia.edu/44181819/IRJET_Quantitative_Morphometric_Analysis_of_Adhala_basin_Ahmednagar_Maharashtra_Using_Arc_GIS_Tool" /> <script async src="https://www.googletagmanager.com/gtag/js?id=G-5VKX33P2DS"></script> <script> window.dataLayer = window.dataLayer || []; function gtag(){dataLayer.push(arguments);} gtag('js', new Date()); gtag('config', 'G-5VKX33P2DS', { cookie_domain: 'academia.edu', send_page_view: false, }); gtag('event', 'page_view', { 'controller': "single_work", 'action': "show", 'controller_action': 'single_work#show', 'logged_in': 'false', 'edge': 'unknown', // Send nil if there is no A/B test bucket, in case some records get logged // with missing data - that way we can distinguish between the two cases. // ab_test_bucket should be of the form <ab_test_name>:<bucket> 'ab_test_bucket': null, }) </script> <script> var $controller_name = 'single_work'; var $action_name = "show"; var $rails_env = 'production'; var $app_rev = 'f165b2130d5c50c25416d834a9f1c4074341d4b5'; var $domain = 'academia.edu'; var $app_host = "academia.edu"; var $asset_host = "academia-assets.com"; var $start_time = new Date().getTime(); var $recaptcha_key = "6LdxlRMTAAAAADnu_zyLhLg0YF9uACwz78shpjJB"; var $recaptcha_invisible_key = "6Lf3KHUUAAAAACggoMpmGJdQDtiyrjVlvGJ6BbAj"; var $disableClientRecordHit = false; </script> <script> window.require = { config: function() { return function() {} } } </script> <script> window.Aedu = window.Aedu || {}; window.Aedu.hit_data = null; window.Aedu.serverRenderTime = new Date(1733263979000); window.Aedu.timeDifference = new Date().getTime() - 1733263979000; </script> <script type="application/ld+json">{"@context":"https://schema.org","@type":"ScholarlyArticle","abstract":"Advancement of technology in natural resource planning has brought new hopes for sustainable development. Sustainable development can be achieved by the micro level planning and management at watershed scale. Watershed is the basic land unit for water resource management and support for human as well as other living beings and is vulnerable to unfavorable weather events and climatic conditions. In present study, the morphometric characteristic of Adhala river basin was done. The Adhala river basin is one of the major tributaries of Pravara river which rises in the North of Akole at Deothan in Ahmednagar district of Maharashtra. It extends between 19°32ʹ40ʺ N to 19°43ʹ02ʺ N latitudes and 74°10ʹ15ʺE to 74°48ʹ18ʺ E longitudes and encompasses an area of 216.17 km2. DEM data were used to calculate the flow accumulation, stream networks, morphometric characteristics and also delineation of watershed using ArcGIS watershed delineator tools. The more emphasis is given to evaluate all the morphometric parameters which are basically categorized in three aspects viz; linear, areal and relief. Strahler\u0026amp;#39;s stream ordering techniques \u0026amp;amp; analysis were followed. The results of the morphometric study showed that the trunk stream order was found to be of 6th order having 3145 numbers of streams in the basin, also total length of the streams was found to be 985.20 km. Lengths of streams indicate flatter gradient of the basin. Bifurcation ratio indicates elongated shape of the basin. Drainage density of Adhala basin was 4.54 km/km2 indicating high drainage densities, circularity ratio was 0.17 and indicated moderate to high relief. Infiltration number was 65.97 indicating low infiltration capacity and very high surface runoff. Relief aspect showed that absolute relief was 552 m and relief ratio was 0.02 indicating overall low relief due to highly elongated basin. The geoprocessing techniques employed in this study will assist in planning \u0026amp;amp; decision making in watershed development.","author":[{"@context":"https://schema.org","@type":"Person","name":"IRJET Journal"}],"contributor":[],"dateCreated":"2020-09-28","dateModified":"2020-09-28","datePublished":"2020-01-01","headline":"IRJET- Quantitative Morphometric Analysis of Adhala basin, Ahmednagar Maharashtra Using Arc-GIS Tool","image":"https://attachments.academia-assets.com/64542162/thumbnails/1.jpg","inLanguage":"en","keywords":["Mechanical Engineering"],"publication":"IRJET","publisher":{"@context":"https://schema.org","@type":"Organization","name":null},"sourceOrganization":[{"@context":"https://schema.org","@type":"EducationalOrganization","name":"irjet"}],"thumbnailUrl":"https://attachments.academia-assets.com/64542162/thumbnails/1.jpg","url":"https://www.academia.edu/44181819/IRJET_Quantitative_Morphometric_Analysis_of_Adhala_basin_Ahmednagar_Maharashtra_Using_Arc_GIS_Tool"}</script><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/single_work_page/loswp-102fa537001ba4d8dcd921ad9bd56c474abc201906ea4843e7e7efe9dfbf561d.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/body-8d679e925718b5e8e4b18e9a4fab37f7eaa99e43386459376559080ac8f2856a.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/button-3cea6e0ad4715ed965c49bfb15dedfc632787b32ff6d8c3a474182b231146ab7.css" /><link rel="stylesheet" media="all" 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[{"id":64542162,"identifier":"Attachment_64542162","shouldShowBulkDownload":false}]; window.loswp.shouldDetectTimezone = true; window.loswp.shouldShowBulkDownload = true; window.loswp.showSignupCaptcha = false window.loswp.willEdgeCache = false; window.loswp.work = {"work":{"id":44181819,"created_at":"2020-09-28T05:51:17.098-07:00","from_world_paper_id":null,"updated_at":"2021-01-17T16:13:50.997-08:00","_data":{"abstract":"Advancement of technology in natural resource planning has brought new hopes for sustainable development. Sustainable development can be achieved by the micro level planning and management at watershed scale. Watershed is the basic land unit for water resource management and support for human as well as other living beings and is vulnerable to unfavorable weather events and climatic conditions. In present study, the morphometric characteristic of Adhala river basin was done. The Adhala river basin is one of the major tributaries of Pravara river which rises in the North of Akole at Deothan in Ahmednagar district of Maharashtra. It extends between 19°32ʹ40ʺ N to 19°43ʹ02ʺ N latitudes and 74°10ʹ15ʺE to 74°48ʹ18ʺ E longitudes and encompasses an area of 216.17 km2. DEM data were used to calculate the flow accumulation, stream networks, morphometric characteristics and also delineation of watershed using ArcGIS watershed delineator tools. The more emphasis is given to evaluate all the morphometric parameters which are basically categorized in three aspects viz; linear, areal and relief. Strahler's stream ordering techniques \u0026 analysis were followed. The results of the morphometric study showed that the trunk stream order was found to be of 6th order having 3145 numbers of streams in the basin, also total length of the streams was found to be 985.20 km. Lengths of streams indicate flatter gradient of the basin. Bifurcation ratio indicates elongated shape of the basin. Drainage density of Adhala basin was 4.54 km/km2 indicating high drainage densities, circularity ratio was 0.17 and indicated moderate to high relief. Infiltration number was 65.97 indicating low infiltration capacity and very high surface runoff. Relief aspect showed that absolute relief was 552 m and relief ratio was 0.02 indicating overall low relief due to highly elongated basin. The geoprocessing techniques employed in this study will assist in planning \u0026 decision making in watershed development.","publication_date":"2020,,","publication_name":"IRJET"},"document_type":"paper","pre_hit_view_count_baseline":null,"quality":"high","language":"en","title":"IRJET- Quantitative Morphometric Analysis of Adhala basin, Ahmednagar Maharashtra Using Arc-GIS Tool","broadcastable":true,"draft":null,"has_indexable_attachment":true,"indexable":true}}["work"]; window.loswp.workCoauthors = [31493941]; window.loswp.locale = "en"; window.loswp.countryCode = "SG"; window.loswp.cwvAbTestBucket = ""; window.loswp.designVariant = "ds_vanilla"; window.loswp.fullPageMobileSutdModalVariant = "full_page_mobile_sutd_modal"; window.loswp.useOptimizedScribd4genScript = false; window.loswp.appleClientId = 'edu.academia.applesignon';</script><script defer="" src="https://accounts.google.com/gsi/client"></script><div class="ds-loswp-container"><div class="ds-work-card--grid-container"><div class="ds-work-card--container js-loswp-work-card"><div class="ds-work-card--cover"><div class="ds-work-cover--wrapper"><div class="ds-work-cover--container"><button class="ds-work-cover--clickable js-swp-download-button" data-signup-modal="{"location":"swp-splash-paper-cover","attachmentId":64542162,"attachmentType":"pdf"}"><img alt="First page of “IRJET- Quantitative Morphometric Analysis of Adhala basin, Ahmednagar Maharashtra Using Arc-GIS Tool”" class="ds-work-cover--cover-thumbnail" src="https://0.academia-photos.com/attachment_thumbnails/64542162/mini_magick20200928-830-n61lwv.png?1601298962" /><img alt="PDF Icon" class="ds-work-cover--file-icon" src="//a.academia-assets.com/assets/single_work_splash/adobe.icon-574afd46eb6b03a77a153a647fb47e30546f9215c0ee6a25df597a779717f9ef.svg" /><div class="ds-work-cover--hover-container"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span><p>Download Free PDF</p></div><div class="ds-work-cover--ribbon-container">Download Free PDF</div><div class="ds-work-cover--ribbon-triangle"></div></button></div></div></div><div class="ds-work-card--work-information"><h1 class="ds-work-card--work-title">IRJET- Quantitative Morphometric Analysis of Adhala basin, Ahmednagar Maharashtra Using Arc-GIS Tool</h1><div class="ds-work-card--work-authors ds-work-card--detail"><a class="ds-work-card--author js-wsj-grid-card-author ds2-5-body-md ds2-5-body-link" data-author-id="31493941" href="https://irjet.academia.edu/IRJET"><img alt="Profile image of IRJET Journal" class="ds-work-card--author-avatar" src="https://0.academia-photos.com/31493941/9304077/11813823/s65_irjet.journal.jpg" />IRJET Journal</a></div><div class="ds-work-card--detail"><p class="ds-work-card--detail ds2-5-body-sm">2020, IRJET</p><div class="ds-work-card--work-metadata"><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">visibility</span><p class="ds2-5-body-sm" id="work-metadata-view-count">…</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">description</span><p class="ds2-5-body-sm">13 pages</p></div><div class="ds-work-card--work-metadata__stat"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">link</span><p class="ds2-5-body-sm">1 file</p></div></div><script>(async () => { const workId = 44181819; 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} }; // If the DOM is still loading, wait for it to be ready before updating the view count. if (document.readyState === "loading") { document.addEventListener('DOMContentLoaded', () => { updateViewCount(viewCount); }); // Otherwise, just update it immediately. } else { updateViewCount(viewCount); } })();</script></div><p class="ds-work-card--work-abstract ds-work-card--detail ds2-5-body-md">Advancement of technology in natural resource planning has brought new hopes for sustainable development. Sustainable development can be achieved by the micro level planning and management at watershed scale. Watershed is the basic land unit for water resource management and support for human as well as other living beings and is vulnerable to unfavorable weather events and climatic conditions. In present study, the morphometric characteristic of Adhala river basin was done. The Adhala river basin is one of the major tributaries of Pravara river which rises in the North of Akole at Deothan in Ahmednagar district of Maharashtra. It extends between 19°32ʹ40ʺ N to 19°43ʹ02ʺ N latitudes and 74°10ʹ15ʺE to 74°48ʹ18ʺ E longitudes and encompasses an area of 216.17 km2. DEM data were used to calculate the flow accumulation, stream networks, morphometric characteristics and also delineation of watershed using ArcGIS watershed delineator tools. The more emphasis is given to evaluate all the morphometric parameters which are basically categorized in three aspects viz; linear, areal and relief. Strahler's stream ordering techniques & analysis were followed. The results of the morphometric study showed that the trunk stream order was found to be of 6th order having 3145 numbers of streams in the basin, also total length of the streams was found to be 985.20 km. Lengths of streams indicate flatter gradient of the basin. Bifurcation ratio indicates elongated shape of the basin. Drainage density of Adhala basin was 4.54 km/km2 indicating high drainage densities, circularity ratio was 0.17 and indicated moderate to high relief. Infiltration number was 65.97 indicating low infiltration capacity and very high surface runoff. Relief aspect showed that absolute relief was 552 m and relief ratio was 0.02 indicating overall low relief due to highly elongated basin. The geoprocessing techniques employed in this study will assist in planning & decision making in watershed development.</p><div class="ds-work-card--button-container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{"location":"continue-reading-button--work-card","attachmentId":64542162,"attachmentType":"pdf","workUrl":"https://www.academia.edu/44181819/IRJET_Quantitative_Morphometric_Analysis_of_Adhala_basin_Ahmednagar_Maharashtra_Using_Arc_GIS_Tool"}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{"location":"download-pdf-button--work-card","attachmentId":64542162,"attachmentType":"pdf","workUrl":"https://www.academia.edu/44181819/IRJET_Quantitative_Morphometric_Analysis_of_Adhala_basin_Ahmednagar_Maharashtra_Using_Arc_GIS_Tool"}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div></div></div></div><div data-auto_select="false" data-client_id="331998490334-rsn3chp12mbkiqhl6e7lu2q0mlbu0f1b" data-doc_id="64542162" data-landing_url="https://www.academia.edu/44181819/IRJET_Quantitative_Morphometric_Analysis_of_Adhala_basin_Ahmednagar_Maharashtra_Using_Arc_GIS_Tool" data-login_uri="https://www.academia.edu/registrations/google_one_tap" data-moment_callback="onGoogleOneTapEvent" id="g_id_onload"></div><div class="ds-top-related-works--grid-container"><div class="ds-related-content--container ds-top-related-works--container"><h2 class="ds-related-content--heading">Related papers</h2><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="0" data-entity-id="102522533" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/102522533/Quantitative_Analysis_of_Drainage_System_is_an_Important_Aspect_of_Prioritisation_of_Watersheds">Quantitative Analysis of Drainage System is an Important Aspect of Prioritisation of Watersheds</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="271635899" href="https://independent.academia.edu/sourabhsingh238">sourabh singh</a></div><p class="ds-related-work--metadata ds2-5-body-xs">2013</p><p class="ds-related-work--abstract ds2-5-body-sm">The quantitative analysis of drainage system is an important aspect of prioritisation of watersheds. Using watershed as a basic unit in morphometric analysis is the most logical choice because all hydrologic and geomorphic processes occur within the watershed. In the present study, an attempt has been made to study the quantitative geomorphological analysis of micro watersheds of Ghataprabha river sub-basin in Karnataka, India. The study region lies between 16° 12’ 16’’ N to 16° 30’ 1’’ N latitude and 74° 45’ 18’’ E to 75° 44’ 58’’ E longitude of northern Karnataka. The twelve micro watersheds of sub basins (KSNU032 and KSNU033) have been prioritized using GIS by determining the areal, linear, and relief parameters based on morphometric analysis on the basis of Survey of India Toposheets at 1:50,000 scale, CARTOSAT-1 DEM data, and RESOURCESAT-2 LISS-III data. Each morphometric characteristic is considered as a single parameter and knowledge based weightage has been assigned. The com...</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Quantitative Analysis of Drainage System is an Important Aspect of Prioritisation of Watersheds","attachmentId":102770659,"attachmentType":"pdf","work_url":"https://www.academia.edu/102522533/Quantitative_Analysis_of_Drainage_System_is_an_Important_Aspect_of_Prioritisation_of_Watersheds","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/102522533/Quantitative_Analysis_of_Drainage_System_is_an_Important_Aspect_of_Prioritisation_of_Watersheds"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="1" data-entity-id="65612420" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/65612420/Morphometric_Analysis_of_Patapur_Micro_watershed_in_North_Eastern_Dry_Zone_of_Karnataka_Using_Geographical_Information_System_A_Case_Study">Morphometric Analysis of Patapur Micro-watershed in North-Eastern Dry Zone of Karnataka Using Geographical Information System: A Case Study</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="6446750" href="https://independent.academia.edu/PremanandDashavant">Premanand Dashavant</a></div><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Morphometric Analysis of Patapur Micro-watershed in North-Eastern Dry Zone of Karnataka Using Geographical Information System: A Case Study","attachmentId":77133089,"attachmentType":"pdf","work_url":"https://www.academia.edu/65612420/Morphometric_Analysis_of_Patapur_Micro_watershed_in_North_Eastern_Dry_Zone_of_Karnataka_Using_Geographical_Information_System_A_Case_Study","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/65612420/Morphometric_Analysis_of_Patapur_Micro_watershed_in_North_Eastern_Dry_Zone_of_Karnataka_Using_Geographical_Information_System_A_Case_Study"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="2" data-entity-id="43761876" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/43761876/Watershed_Management_of_the_Western_Region_of_Akkalkot_Taluka_Dhubdhubi_Basin_Solapur_District_Maharashtra">Watershed Management of the Western Region of Akkalkot Taluka, Dhubdhubi Basin, Solapur District, Maharashtra</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="165910677" href="https://independent.academia.edu/VijayMKolhe">Vijay M Kolhe</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="31258981" href="https://kedarunipune.academia.edu/NanasahebSathe">Nanasaheb J Sathe</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Journal of Engineering Sciences (JES), 2020</p><p class="ds-related-work--abstract ds2-5-body-sm">Morphometric analysis includes various parameters in preparation of drainage networks maps ordering the various streams, measurements of catchment area, perimeter, relative relief, and relief ratio, channels, drainage density, drainage frequency, bifurcation ratio, texture ratio, circulatory ratio of the western region watershed of Akkalkot Taluka i.e. Dhubdhubi basin. The Morphometric studies helps to understand the nature of the drainage properties of watershed, which in turn gives a valid reasoning for the soil transportation and its conservation. Geographic Information System (GIS) and Remote Sensing is the most efficient tools in delineation of drainage patterns and water resources planning worldwide. The hydrological investigations provides the information for planning, delineating, evaluation, exploitation and management of groundwater resources. The main sources is the rainfall that plays a vital role in fluctuation of water table. Depending upon the hydrogeological characters of the subsurface, the rate of recharge after the rainfall event decides the groundwater levels and there is always a time gap, which is defined as lap time to attain the maximum water level and subsequently there is a time gap for attaining lowest water level which is also a function of Geology and differences in the heads provide the flow of water from higher potential to lower potential. This flow of water brings down the water levels increasing the gap between the surface and the water table which is designated as the vadose zone. This also delineates the area feasible and non-feasible for artificial recharge. Present study is an attempt to evaluate the nature of the drainage basins and its relationship with characters of the terrains and for deriving means to conserve and manage the resources and overcoming the water management system.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Watershed Management of the Western Region of Akkalkot Taluka, Dhubdhubi Basin, Solapur District, Maharashtra","attachmentId":98306501,"attachmentType":"pdf","work_url":"https://www.academia.edu/43761876/Watershed_Management_of_the_Western_Region_of_Akkalkot_Taluka_Dhubdhubi_Basin_Solapur_District_Maharashtra","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/43761876/Watershed_Management_of_the_Western_Region_of_Akkalkot_Taluka_Dhubdhubi_Basin_Solapur_District_Maharashtra"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="3" data-entity-id="15401189" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/15401189/Drainage_Morphometry_Evaluation_for_Kodavanar_sub_basin_to_Understand_the_Interrelationships_in_Morphological_Systems_and_in_Process_Response_Systems">Drainage Morphometry Evaluation for Kodavanar sub basin to Understand the Interrelationships in Morphological Systems and in Process-Response Systems</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1870354" href="https://tnou.academia.edu/DrAMuthukrishnanAchari">Dr. A. Muthukrishnan Achari</a></div><p class="ds-related-work--abstract ds2-5-body-sm">The utility of the drainage geomorphometric characteristics for the investigations relating to geomorphology and hydrology has been amply demonstrated by a number of studies to conducted various geospatial technology. The present study area is Dindigul district and its suburbs have been frequented by heavy rains during the monsoon seasons. The river Kodavanar which is frequently in spate during the monsoon seasons and flows through the western part of the Dindigul and its suburbs has a large catchment area, extending to the neighbouring Karur and Madurai Districts on the north east. The aim is to assess the morphometric characteristics of the Kodavanar sub basin of Amaravathy basin of Tamil Nadu. The objectives is to accomplish the aim are: to analyse the linear, areal and relief aspects and to bring out the form and processes of the study area. In order to understand the drainage characteristics in various parts of the Kodavanar sub basin, the basin has been divided into 5 watersheds namely, Kodavanar-Umiyar, Anaiviludan Odai, Pudukulam kombaiar, Todikombu and Periyakombai watersheds. Strahler‟s method of stream ordering which is the most commonly used method of stream ordering has been followed for the present study. For all the 5 watersheds separately, the linear, and areal and relief aspects have been discussed. The linear aspects considered for the study include stream order, stream number, stream length, bifurcation ratio and length ratio. The areal aspects include basin area, form factor, circulatory ratio, elongation ratio, drainage density, stream frequency, length of overland flow and the relief aspects considered for the present study are basin relief and ruggedness number.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Drainage Morphometry Evaluation for Kodavanar sub basin to Understand the Interrelationships in Morphological Systems and in Process-Response Systems","attachmentId":38670010,"attachmentType":"pdf","work_url":"https://www.academia.edu/15401189/Drainage_Morphometry_Evaluation_for_Kodavanar_sub_basin_to_Understand_the_Interrelationships_in_Morphological_Systems_and_in_Process_Response_Systems","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/15401189/Drainage_Morphometry_Evaluation_for_Kodavanar_sub_basin_to_Understand_the_Interrelationships_in_Morphological_Systems_and_in_Process_Response_Systems"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="4" data-entity-id="12712078" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/12712078/Influence_of_Lineaments_on_drainage_morphometry_using_Geoinformatics_a_case_study_of_Nethravathi_Watershed">Influence of Lineaments on drainage morphometry using Geoinformatics: a case study of Nethravathi Watershed</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="28950357" href="https://cuk-in.academia.edu/BharathkumarL">Bharathkumar L</a></div><p class="ds-related-work--abstract ds2-5-body-sm">An attempt has been made to study the influence of Lineaments on drainage morphometry of Nethravathi Watershed of Dakshina Kannada district. A lineament is s linear feature in a landscape which represents the underlying geological structure. Lineaments play an important role in water movement and storage. Usually drainage network follows elevation of terrain. A linear drainage network will either controlled by geological structures or steep slope. Typically it represents the fault zones, series of folds, fracture zones, shear zones and igneous intrusions like dykes. Lineaments were extracted from Bhuvan website in the form of WMS layer and processed in ArcGIS 9.3 software. Drainage networks for the sub watershed are extracted from Cartosat 1 Dem data derived from Bhuvan portal. Morphometric calculations were carried out using ArcGIS 9.3 to evaluate aerial, linear and relief features of morphometric parameters. Compare to conventional method of drainage analysis, Remote sensing and GIS can provide appropriate data with good coverage. The analysis clearly shows following successive results. IX sub-basin have high elongation ratio (Re), basin relief (Bh), Ruggedness number (Rn) and time of concentration (Tc). The erosion and peak discharges were high in these basins. It is necessary to construct the check dams and earth dams to reduce peak discharge along the main channel. The study is predominantly useful in field of watershed management and artificial recharge structure to solve the crisis on water issues.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Influence of Lineaments on drainage morphometry using Geoinformatics: a case study of Nethravathi Watershed","attachmentId":37791151,"attachmentType":"pdf","work_url":"https://www.academia.edu/12712078/Influence_of_Lineaments_on_drainage_morphometry_using_Geoinformatics_a_case_study_of_Nethravathi_Watershed","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/12712078/Influence_of_Lineaments_on_drainage_morphometry_using_Geoinformatics_a_case_study_of_Nethravathi_Watershed"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="5" data-entity-id="40152147" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/40152147/A_QUANTITATIVE_ANALYSIS_OF_WATERSHED_MORPHOLOGY_USING_GEO_SPATIAL_APPROACH">A QUANTITATIVE ANALYSIS OF WATERSHED MORPHOLOGY USING GEO-SPATIAL APPROACH</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="3775225" href="https://independent.academia.edu/TJPRCPublication">TJPRC Publication</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Transstellar Journals, 2019</p><p class="ds-related-work--abstract ds2-5-body-sm">A study was conducted from Kumulur watershed, Trichy district, Tamil Nadu located at latitude and longitude of10°56'41.50"N-10°55'57.85"N&78°50'4.34"E-78°50'4.58"E, respectively with an areal extent of 848694 sq. m. The spatial data of Digital Elevation Model (DEM) of 4-meter resolution and satellite imagery(Google Earth) were used for the extraction of the watershed characteristics through morphometric analysis. The hydrological module of ArcGIS software was used to analyze the geospatial data. The watershed was therein delineated and the various parameters for the morphometric analysis viz., stream order (U), stream number (N u), stream length (L u), mean stream length (L sm), stream length ratio (R L), bifurcation ratio (R b), drainage density (D d), drainage texture (T), stream frequency (F s), form factor (F f), elongation ratio (R e), circularity ratio (R c), relief (R) and relief ratio (R r)were calculated using the software. The basin morphometry shows the numerical analysis and mathematical quantification of different aspects of the watershed. The morphometric analysis includes aspects such as linear, areal & relief. The area and perimeter of the basin was calculated as 848694 sq. m. and 4923.06 m respectively. The total number of streams were found to be 213 and the total stream length of the watershed was calculated as 12833.6240 mof all the 4 stream orders forming a dendritic type of drainage pattern. The maximum length of the stream for the entire basin was observed to be 315.532 m. The bifurcation ratio of the basin varied from 1.543 to 5.000; the elongation ratio and the circularity ratio of the drainage basin were calculated as 0.5967 and 0.4398 respectively. The highest and lowest elevation of the watershed were observed to be 102.021 and 68.786 m which delivered the relief as 33.235 m and the relief ratio as 0.019.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"A QUANTITATIVE ANALYSIS OF WATERSHED MORPHOLOGY USING GEO-SPATIAL APPROACH","attachmentId":60370826,"attachmentType":"pdf","work_url":"https://www.academia.edu/40152147/A_QUANTITATIVE_ANALYSIS_OF_WATERSHED_MORPHOLOGY_USING_GEO_SPATIAL_APPROACH","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/40152147/A_QUANTITATIVE_ANALYSIS_OF_WATERSHED_MORPHOLOGY_USING_GEO_SPATIAL_APPROACH"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="6" data-entity-id="28331870" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/28331870/Morphometric_Analysis_of_a_Phulambri_River_Drainage_Basin_Gp8_Watershed_Aurangabad_District_Maharashtra_using_Geographical_Information_System">Morphometric Analysis of a Phulambri River Drainage Basin (Gp8 Watershed), Aurangabad District (Maharashtra) using Geographical Information System</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="53127938" href="https://independent.academia.edu/SonarMohan">Mohan Sonar</a></div><p class="ds-related-work--abstract ds2-5-body-sm">Geographical information system (GIS) has emerged as a professional tool in demarcation of drainage pattern and ground water potential and its planning. GIS and image processing techniques can be utilized for the identification of morphological characteristics and investigating properties of basin. The morphometric parameters of basin can deal with linear, areal and relief features. The present study deals mainly with the geometry, more importance being given on the evaluation of morphometric parameters such as stream order (Nu), stream length (Lu), bifurcation ratio (Rb), drainage density (D), stream frequency (Fs), texture ratio (T), elongation ratio (Re), circularity ratio (Rc), and form factor ratio (Rf) etc. Study area is Phulambri river basin located in Aurangabad district of Maharashtra state in India. The GIS based Morphometric analysis of this drainage basin revealed that the Girja-Purna is 6th order drainage basin and drainage pattern mainly in dendritic type thereby indicates homogeneity in texture and lack of structural control. Total number of streams is 1616, in which 895 are first order, 391 are second order, 196 are third order and 97 are fourth order streams and 36 of the fifth order and 1 of the sixth order. The length of stream segment is maximum for first order stream and decreases as the stream order increases. The drainage density (Dd) of study area is 0.030 km/km 2 .</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Morphometric Analysis of a Phulambri River Drainage Basin (Gp8 Watershed), Aurangabad District (Maharashtra) using Geographical Information System","attachmentId":48664840,"attachmentType":"pdf","work_url":"https://www.academia.edu/28331870/Morphometric_Analysis_of_a_Phulambri_River_Drainage_Basin_Gp8_Watershed_Aurangabad_District_Maharashtra_using_Geographical_Information_System","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/28331870/Morphometric_Analysis_of_a_Phulambri_River_Drainage_Basin_Gp8_Watershed_Aurangabad_District_Maharashtra_using_Geographical_Information_System"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="7" data-entity-id="40436369" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/40436369/Morphometric_Analysis_of_Vincharna_River_Watershed_Ahemadnagar_District">Morphometric Analysis of Vincharna River Watershed, Ahemadnagar District.</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="114990540" href="https://svims-pune.academia.edu/LalitThakare">Lalit Thakare</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Maharashtra Bhugolshastra Sanshodhan Patrika, 2018</p><p class="ds-related-work--abstract ds2-5-body-sm">In this paper, an attempt has been made to study the detailed morphometric characteristics of Vincharna watershed, tributary of the Sina river basin in Ahmednagar district, Maharashtra. The drainage patterns are dendritic and parallel, covering 390 sq. km. Morphometric analysis was done to determine the drainage characteristics of Vincharna watershed using topographic maps, ASTER and SRTM DEM (30 m Resolution). For detailed study, ASTER and SRTM data was used for preparing Digital Elevation Model (DEM). The relief data was derived from SOI toposheets and GIS-RS techniques were used to evaluate Linear, Areal and Relief aspects of morphometric parameters. Watershed boundary, flow accumulation, flow direction, flow length, stream ordering were prepared using Hydrology Tool; and contour, Slope, Aspect, Hillshade have been prepared using Surface Tool in ArcGIS-10 software. Different thematic maps like Stream Network, Slope, Relief, Aspect and Hillshade were prepared by using ArcGIS software. Based on all morphometric parameters achieved, it can be concluded that the development in erosive processes of the area by the river has been progressed beyond the maturity which indicates the lithology had an influence on the drainage development. These studies are very useful for planning rainwater harvesting and watershed management.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Morphometric Analysis of Vincharna River Watershed, Ahemadnagar District.","attachmentId":60694636,"attachmentType":"pdf","work_url":"https://www.academia.edu/40436369/Morphometric_Analysis_of_Vincharna_River_Watershed_Ahemadnagar_District","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/40436369/Morphometric_Analysis_of_Vincharna_River_Watershed_Ahemadnagar_District"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="8" data-entity-id="31928313" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/31928313/Morphometric_Analysis_and_Prioritization_of_Sub_Watersheds_of_Brahmani_and_Baitarni_Basins_Using_Remote_Sensing_and_GIS_Keonjhar_And_Sundargarh_Districts_Odisha_India">Morphometric Analysis and Prioritization of Sub-Watersheds of Brahmani and Baitarni Basins Using Remote Sensing and GIS, Keonjhar And Sundargarh Districts, Odisha, India</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="59085876" href="https://nitk.academia.edu/DrRajuAedla">EditorIJEE RajuAedla</a></div><p class="ds-related-work--abstract ds2-5-body-sm">In this study, morphometric analysis and prioritization of 12 sub-watersheds of Brahmani and Baitarni Basins, which are located in Keonjhar and Sundargarh Districts of Odisha State, India is carried out using Remote Sensing and GIS techniques. The morphometric parameters considered for analysis are stream order, stream length, bifurcation ratio, drainage density, stream frequency, texture ratio, form factor, circulatory ratio, elongation ratio, relief ratio, length of overland flow and basin shape. A total number of 1654 streams were identified of which 1223 are first order streams, 320 are 2 nd order, 77 are 3 rd order, 20 are 4 th order, 6 are 5 th order, 4 are 6 th order and 4 are of 7 th order. The streams up to seventh order can be seen in BAISWD6, BAISWD7, BAISWD8, and BAISWD11. Drainage patterns of stream network from the basin have been observed as mainly dendritic type which indicates the homogeneity in texture and lack of structural control.The drainage pattern is dendritic and the highest order stream is of 7 th order. The bifurcation ratio (Rbm) varies from 2.99 to 5.91 and all sub-watersheds fall under normal basin category. The drainage density (Dd) of the study area is varying between 2.05 and 2.89 km/km 2 indicating low density with highly permeable subsoil, thick vegetation cover, low relief and course drainage texture. Elongation ratio of all the watersheds varies between 0.65 to 0.70 respectively and indicating that it is elongated. Circulatory Ratio (Rc) ranges from 0.38 to 0.68 indicating that all the sub-watersheds except BAISWD6 are more or less circular and are characterized by high to moderate relief and drainage system is structurally controlled. The sub-watershed BAISWD6 having the Rc value of 0.38 indicating that it is elongated. The relief ratio of all sub-watersheds varies between the values of 23.56 to 47.59m, which indicates that the basin has strong relief and steep slope. The compound parameter values of 12 sub-watersheds of study area were calculated and prioritization rating was carried out. Sub-watershed BAISWD9 with a compound parameter value of 5.6 receives the highest priority indicates the greater degree of erosion in the particular sub-watershed and it becomes potential area for applying soil conservative measure.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"Morphometric Analysis and Prioritization of Sub-Watersheds of Brahmani and Baitarni Basins Using Remote Sensing and GIS, Keonjhar And Sundargarh Districts, Odisha, India","attachmentId":52207595,"attachmentType":"pdf","work_url":"https://www.academia.edu/31928313/Morphometric_Analysis_and_Prioritization_of_Sub_Watersheds_of_Brahmani_and_Baitarni_Basins_Using_Remote_Sensing_and_GIS_Keonjhar_And_Sundargarh_Districts_Odisha_India","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/31928313/Morphometric_Analysis_and_Prioritization_of_Sub_Watersheds_of_Brahmani_and_Baitarni_Basins_Using_Remote_Sensing_and_GIS_Keonjhar_And_Sundargarh_Districts_Odisha_India"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="9" data-entity-id="38137584" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/38137584/STUDY_OF_DRAINAGE_SYSTEM_AND_ITS_HYDROLOGICAL_IMPLICATIONS_USING_GEO_SPATIAL_TECHNIQUES_A_MORPHOMETRIC_ANALYSIS_IN_MOHAL_KHAD_WATERSHED_OF_KULLU_DISTRICT_HIMACHAL_PRADESH_INDIA">STUDY OF DRAINAGE SYSTEM AND ITS HYDROLOGICAL IMPLICATIONS USING GEO-SPATIAL TECHNIQUES: A MORPHOMETRIC ANALYSIS IN MOHAL KHAD WATERSHED OF KULLU DISTRICT, HIMACHAL PRADESH, INDIA.</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="39246530" href="https://independent.academia.edu/JournalIJAR">IJAR Indexing</a></div><p class="ds-related-work--metadata ds2-5-body-xs">International Journal of Advanced Research (IJAR), 2018</p><p class="ds-related-work--abstract ds2-5-body-sm">Understanding the behavior of surface drainage network is one of the important prerequisite condition for effective planning and management of water resources within the watershed. Morphometric analysis of a watershed is a crucial step in watershed development and management to understand and interpret the dynamics of drainage system of the watershed and is useful for interpretation of silent features of drainage network. A morphometric analysis was carried out to evaluate the drainage characteristics of Mohalkhad watershed which covers an area about 54 km2 in Kullu district of Himachal Pradesh in Indian Himalayan Region (IHR). Geospatial technique/tool such as Remote Sensing (RS) and GIS was used to evaluate the linear, areal and relief aspects of morphometric parameters. RS and GIS technique is very helpful over the conventional methods that are too laborious and cumbersome. To carry out this study, Survey of India (SOI) toposheet of 1:50,000 scale and ASTER DEM (30 m resolution) data were used and analysis was carried out in ArcGIS 10.5 software. Total 21 morphometric parameters of Mohalkhad watershed were evaluated considering the linear, areal and relief aspects. The significance of each morphometric parameter with the hydrological behavior of the watershed is discussed in this study. This exercise provide detailed insight into drainage system of the Mohalkhad watershed, which is useful for the development and management of water conservation measures in the area.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{"location":"wsj-grid-card-download-pdf-modal","work_title":"STUDY OF DRAINAGE SYSTEM AND ITS HYDROLOGICAL IMPLICATIONS USING GEO-SPATIAL TECHNIQUES: A MORPHOMETRIC ANALYSIS IN MOHAL KHAD WATERSHED OF KULLU DISTRICT, HIMACHAL PRADESH, INDIA.","attachmentId":58168706,"attachmentType":"pdf","work_url":"https://www.academia.edu/38137584/STUDY_OF_DRAINAGE_SYSTEM_AND_ITS_HYDROLOGICAL_IMPLICATIONS_USING_GEO_SPATIAL_TECHNIQUES_A_MORPHOMETRIC_ANALYSIS_IN_MOHAL_KHAD_WATERSHED_OF_KULLU_DISTRICT_HIMACHAL_PRADESH_INDIA","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/38137584/STUDY_OF_DRAINAGE_SYSTEM_AND_ITS_HYDROLOGICAL_IMPLICATIONS_USING_GEO_SPATIAL_TECHNIQUES_A_MORPHOMETRIC_ANALYSIS_IN_MOHAL_KHAD_WATERSHED_OF_KULLU_DISTRICT_HIMACHAL_PRADESH_INDIA"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div></div></div><div class="ds-sticky-ctas--wrapper js-loswp-sticky-ctas hidden"><div class="ds-sticky-ctas--grid-container"><div class="ds-sticky-ctas--container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{"location":"continue-reading-button--sticky-ctas","attachmentId":64542162,"attachmentType":"pdf","workUrl":null}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{"location":"download-pdf-button--sticky-ctas","attachmentId":64542162,"attachmentType":"pdf","workUrl":null}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div></div></div><div class="ds-below-fold--grid-container"><div class="ds-work--container js-loswp-embedded-document"><div class="attachment_preview" data-attachment="Attachment_64542162" style="display: none"><div class="js-scribd-document-container"><div class="scribd--document-loading js-scribd-document-loader" style="display: block;"><img alt="Loading..." src="//a.academia-assets.com/images/loaders/paper-load.gif" /><p>Loading Preview</p></div></div><div style="text-align: center;"><div class="scribd--no-preview-alert js-preview-unavailable"><p>Sorry, preview is currently unavailable. 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