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(PDF) Morphometric Study of Dhatarwadi River Basin Using RS and GIS Techniques | Priti Jayswal (SWE) - Academia.edu
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Place and Duration of Study: This study is a work done for the research work in Ph.D. degree at College of Agricultural Engineering and Technology, Junagadh Agricultural University, Junagadh," /> <title>(PDF) Morphometric Study of Dhatarwadi River Basin Using RS and GIS Techniques | Priti Jayswal (SWE) - Academia.edu</title> <link rel="canonical" href="https://www.academia.edu/56959055/Morphometric_Study_of_Dhatarwadi_River_Basin_Using_RS_and_GIS_Techniques" /> <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 = '10e3dae8ffd20c8f5a4f7002303d92ad374c73ee'; 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(1733263524000); window.Aedu.timeDifference = new Date().getTime() - 1733263524000; </script> <script type="application/ld+json">{"@context":"https://schema.org","@type":"ScholarlyArticle","abstract":"Aims: Morphometric study of Dhatarwadi river basin. Place and Duration of Study: This study is a work done for the research work in Ph.D. degree at College of Agricultural Engineering and Technology, Junagadh Agricultural University, Junagadh, Gujarat, India. Methodology: Morphometric analysis involved determination of linear, aerial and relief aspects of the Dhatarwadi river basin, which was carried out using 30 X 30 m SRTM DEM in ArcGIS 10.5 software using standard formulae. Results: The obtained results revealed that the Dhatarwadi river basin is 6th order drainage basin. The total number of 1327 streams were identified out of which 1st, 2nd, 3rd, 4th, 5th and 6th order streams are counted as 1036, 239, 42, 7, 2 and 1 number, respectively. The mean bifurcation ratio value is 4.31 for the study area which indicates that the geological structures are not distorting the drainage pattern. Stream length ratio varies between 0.14 and 2.14 indicates late youth geomorphic stage. 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"https://www.academia.edu/login?post_login_redirect_url=https%3A%2F%2Fwww.academia.edu%2F54249189%2FMorphometric_Study_of_Dhatarwadi_River_Basin_Using_RS_and_GIS_Techniques%3Fauto%3Ddownload"; window.loswp.translateUrl = "https://www.academia.edu/login?post_login_redirect_url=https%3A%2F%2Fwww.academia.edu%2F54249189%2FMorphometric_Study_of_Dhatarwadi_River_Basin_Using_RS_and_GIS_Techniques%3Fshow_translation%3Dtrue"; window.loswp.previewableAttachments = [{"id":70703659,"identifier":"Attachment_70703659","shouldShowBulkDownload":false}]; window.loswp.shouldDetectTimezone = true; window.loswp.shouldShowBulkDownload = true; window.loswp.showSignupCaptcha = false window.loswp.willEdgeCache = false; window.loswp.work = {"work":{"id":54249189,"created_at":"2021-09-30T03:50:08.113-07:00","from_world_paper_id":174961565,"updated_at":"2021-09-30T04:43:10.951-07:00","_data":{"abstract":"Aims: Morphometric study of Dhatarwadi river basin. Place and Duration of Study: This study is a work done for the research work in Ph.D. degree at College of Agricultural Engineering and Technology, Junagadh Agricultural University, Junagadh, Gujarat, India. Methodology: Morphometric analysis involved determination of linear, aerial and relief aspects of the Dhatarwadi river basin, which was carried out using 30 X 30 m SRTM DEM in ArcGIS 10.5 software using standard formulae. Results: The obtained results revealed that the Dhatarwadi river basin is 6th order drainage basin. The total number of 1327 streams were identified out of which 1st, 2nd, 3rd, 4th, 5th and 6th order streams are counted as 1036, 239, 42, 7, 2 and 1 number, respectively. The mean bifurcation ratio value is 4.31 for the study area which indicates that the geological structures are not distorting the drainage pattern. Stream length ratio varies between 0.14 and 2.14 indicates late youth geomorphic stage. The leng...","publisher":"Sciencedomain International","publication_name":"Current Journal of Applied Science and Technology"},"document_type":"paper","pre_hit_view_count_baseline":null,"quality":"high","language":"en","title":"Morphometric Study of Dhatarwadi River Basin Using RS and GIS Techniques","broadcastable":null,"draft":null,"has_indexable_attachment":true,"indexable":true}}["work"]; window.loswp.workCoauthors = [65512584]; 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":70703659,"attachmentType":"pdf"}"><div class="ds-work-cover--blank-cover"><div class="ds-work-cover--blank-cover--title">Morphometric Study of Dhatarwadi River Basin Using RS and GIS Techniques</div></div><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">Morphometric Study of Dhatarwadi River Basin Using RS and GIS Techniques</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="65512584" href="https://independent.academia.edu/PritiJayswalSWE"><img alt="Profile image of Priti Jayswal (SWE)" class="ds-work-card--author-avatar" src="https://0.academia-photos.com/65512584/50775911/38817247/s65_priti.jayswal_swe_.png" />Priti Jayswal (SWE)</a></div><div class="ds-work-card--detail"><p class="ds-work-card--detail ds2-5-body-sm">Current Journal of Applied Science and Technology</p></div><p class="ds-work-card--work-abstract ds-work-card--detail ds2-5-body-md">Aims: Morphometric study of Dhatarwadi river basin. Place and Duration of Study: This study is a work done for the research work in Ph.D. degree at College of Agricultural Engineering and Technology, Junagadh Agricultural University, Junagadh, Gujarat, India. Methodology: Morphometric analysis involved determination of linear, aerial and relief aspects of the Dhatarwadi river basin, which was carried out using 30 X 30 m SRTM DEM in ArcGIS 10.5 software using standard formulae. Results: The obtained results revealed that the Dhatarwadi river basin is 6th order drainage basin. The total number of 1327 streams were identified out of which 1st, 2nd, 3rd, 4th, 5th and 6th order streams are counted as 1036, 239, 42, 7, 2 and 1 number, respectively. The mean bifurcation ratio value is 4.31 for the study area which indicates that the geological structures are not distorting the drainage pattern. Stream length ratio varies between 0.14 and 2.14 indicates late youth geomorphic stage. The leng...</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":70703659,"attachmentType":"pdf","workUrl":"https://www.academia.edu/54249189/Morphometric_Study_of_Dhatarwadi_River_Basin_Using_RS_and_GIS_Techniques"}">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":70703659,"attachmentType":"pdf","workUrl":"https://www.academia.edu/54249189/Morphometric_Study_of_Dhatarwadi_River_Basin_Using_RS_and_GIS_Techniques"}"><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="70703659" data-landing_url="https://www.academia.edu/54249189/Morphometric_Study_of_Dhatarwadi_River_Basin_Using_RS_and_GIS_Techniques" 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="102733879" 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/102733879/Morphometric_Analysis_of_Dhadhar_River_Basin_Gujarat">Morphometric Analysis of Dhadhar River Basin, Gujarat</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="35300658" href="https://msubaroda.academia.edu/SANSKRITIMUJUMDAR">SANSKRITI MUJUMDAR</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Zenodo (CERN European Organization for Nuclear Research), 2015</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 Dhadhar River Basin, Gujarat","attachmentId":102924867,"attachmentType":"pdf","work_url":"https://www.academia.edu/102733879/Morphometric_Analysis_of_Dhadhar_River_Basin_Gujarat","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/102733879/Morphometric_Analysis_of_Dhadhar_River_Basin_Gujarat"><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="125209727" 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/125209727/A_Geo_Spatial_Based_Approach_for_Morphometric_Analysis_of_Sindphana_River_Basin_in_Shirur_Kasar_Taluka_M_S_India">A Geo-Spatial Based Approach for Morphometric Analysis of Sindphana River Basin in Shirur-Kasar Taluka, M.S., 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="191972391" href="https://independent.academia.edu/SandipSirsat1">Dr. Sandip K . Sirsat</a></div><p class="ds-related-work--metadata ds2-5-body-xs">International Journal of Geo-informatics and Geological Science, 2024</p><p class="ds-related-work--abstract ds2-5-body-sm">The present study based on morphometric analysis in the Sindphana River Basin was carried out for the delineation of areas for the natural water resources and long-term sustainability in Shirur-Kasar Taluka of Beed district, Maharashtra, India. The linear, areal, drainage and relief aspects were analyzed with the help of SRTM DEM data using Remote Sensing and GIS techniques. The total basin length is 44.24 km, and 1078 km 2 is the total basin area of the Sindphana River Basin in Shirur-Kasar Taluka. In the study area dendritic to sub-dendritic drainage patterns were observed with homogenous lithology and maximum seventh-order stream networks. The mean bifurcation ratio is 4.51 which suggests the basin is not structurally controlled. Water storage capacity in flat areas and runoff in steep areas are indicated by Rho values and mean stream length. The elongation and circulatory ratio values are 0.472 and 0.62, respectively, which suggests the river basin has an elongated shape and very fine drainage texture. The river basin area reveals that 2.26 km-1 drainage density value which suggests a moderate infiltration rate and is feasible for soil and water resource structures for further growth of groundwater. This study is beneficial for delineating the water resource areas for the conservation and management of the basin.</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 Geo-Spatial Based Approach for Morphometric Analysis of Sindphana River Basin in Shirur-Kasar Taluka, M.S., India","attachmentId":119293512,"attachmentType":"pdf","work_url":"https://www.academia.edu/125209727/A_Geo_Spatial_Based_Approach_for_Morphometric_Analysis_of_Sindphana_River_Basin_in_Shirur_Kasar_Taluka_M_S_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/125209727/A_Geo_Spatial_Based_Approach_for_Morphometric_Analysis_of_Sindphana_River_Basin_in_Shirur_Kasar_Taluka_M_S_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="2" data-entity-id="110931783" 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/110931783/Drainage_Basin_Characteristics_of_Dhund_River_Basin_Eastern_Rajasthan_India_Using_Remote_Sensing_and_GIS_Techniques">Drainage Basin Characteristics of Dhund River Basin, Eastern Rajasthan India, Using Remote Sensing and GIS Techniques</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="253295931" href="https://independent.academia.edu/SadiaMazahir">Sadia Mazahir</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Journal of Geographic Information System, 2022</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 Basin Characteristics of Dhund River Basin, Eastern Rajasthan India, Using Remote Sensing and GIS Techniques","attachmentId":108595697,"attachmentType":"pdf","work_url":"https://www.academia.edu/110931783/Drainage_Basin_Characteristics_of_Dhund_River_Basin_Eastern_Rajasthan_India_Using_Remote_Sensing_and_GIS_Techniques","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/110931783/Drainage_Basin_Characteristics_of_Dhund_River_Basin_Eastern_Rajasthan_India_Using_Remote_Sensing_and_GIS_Techniques"><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="44969530" 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/44969530/Study_of_linear_aspects_of_morphometric_parameters_in_parts_of_TAPI_river_basin_Madhya_Pradesh_India_using_remote_sensing_and_GIS_perspective">Study of linear aspects of morphometric parameters in parts of TAPI river basin, Madhya Pradesh, India using remote sensing and GIS perspective</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="10600685" href="https://barkatullahuniversity.academia.edu/SharaddeepVarshney">Dr. Sharaddeep Varshney</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Int J Geogr Geol Environ 2020;2(2):131-135., 2020</p><p class="ds-related-work--abstract ds2-5-body-sm">Remote Sensing technique is a method for basin study as the satellite images provide a synoptic view over a large area. 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Five types of drainage patterns were identified: dendritic, parallel, rectangular, trellis, and modified dendritic/trellis. Study conclude that remote sensing data (Carto DEM of 30 m spatial resolution) along with geoprocessing techniques proven to be a tool used for morphometric analysis and evolution of linear aspects of morphometric parameters. Bifurcation ratio of basin (1.54 to 5.32) showing that geologic structures moderately controlled the drainage pattern. Length of overland flow of the basin (0.209 Km) usually low and indicates that basin is showing high relief and slope.</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 linear aspects of morphometric parameters in parts of TAPI river basin, Madhya Pradesh, India using remote sensing and GIS perspective","attachmentId":65504498,"attachmentType":"pdf","work_url":"https://www.academia.edu/44969530/Study_of_linear_aspects_of_morphometric_parameters_in_parts_of_TAPI_river_basin_Madhya_Pradesh_India_using_remote_sensing_and_GIS_perspective","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/44969530/Study_of_linear_aspects_of_morphometric_parameters_in_parts_of_TAPI_river_basin_Madhya_Pradesh_India_using_remote_sensing_and_GIS_perspective"><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="30045118" 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/30045118/MORPHOMETRIC_ANALYSIS_OF_FOUR_SUB_USING_REMOTE_SENSING_AND_GIS_TECHNIQUES_MORPHOMETRIC_ANALYSIS_OF_FOUR_SUB_WATERSHEDS_IN_BAH_AREA_OF_AGRA_DISTRICT_USING_REMOTE_SENSING_AND_GIS_TECHNIQUES_About_the_Author_WATERSHEDS_IN_BAH_AREA_OF_AGRA_DISTRICT">MORPHOMETRIC ANALYSIS OF FOUR SUB USING REMOTE SENSING AND GIS TECHNIQUES MORPHOMETRIC ANALYSIS OF FOUR SUB-WATERSHEDS IN BAH AREA OF AGRA DISTRICT USING REMOTE SENSING AND GIS TECHNIQUES About the Author: WATERSHEDS IN BAH AREA OF AGRA 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="143954" href="https://jnu.academia.edu/sharadchandradwivedi">Sharad Chandra Dwivedi</a></div><p class="ds-related-work--abstract ds2-5-body-sm">Morphometric analysis of four sub-watersheds namely Pidhaura, Batesar, Balapur and Pariar forming parts of Yamuna River around Bah Tahsil of Agra district have been carried out using Geo-coded FCC of bands 2, 3 and 4 of IRS 1D, LISS-III, SOI toposheets number 54 J/5 and 54 J/9 and GIS softwares-ArcGIS, Arcview and 3Dem software for preparation of DEM. The present study shows terrain exhibits dendritic to sub-dendritic drainage pattern, stream order ranges from third to fourth order; drainage density varies slightly and has very coarse to coarse texture in Pidhaura and Balarpur sub-watersheds and fine drainage texture in Batesar and Pariar sub-watersheds. The other parameters determined and discussed include bifurcation ratio, elongation ratio, stream frequency, number, length of overland flow and relief aspects of the watersheds. The mean bifurcation ratio depicts that the basin falls under normal basin category. The elongation ratio shows that Balarpur sub-watershed mark elongation pattern whereas Pidhaura, Batesar and Pariar sub watersheds possess circular shape. The present study concludes that remote sensing techniques proved to be a competent tool in morphometric analysis of drainage basin and channel network. watersheds namely Pidhaura, Batesar, Balapur and Pariar forming parts of of Agra district have been coded FCC of bands 2, 3 and 4 of IRS-III, SOI toposheets number 54 J/5 and 54 J/9 and ArcGIS, Arcview and 3Dem software for preparation of DEM. The present study shows that the dendritic drainage pattern, stream order ranges from third to fourth order; drainage density varies slightly and has very coarse to coarse texture watersheds and fine drainage watersheds. The other parameters determined and discussed include bifurcation gation ratio, stream frequency, infiltration number, length of overland flow and relief aspects of the o depicts that the basin falls under normal basin category. The elongation watershed mark elongation pattern whereas Pidhaura, Batesar and Pariar sub-watersheds possess circular shape. The present study ensing techniques proved to be a competent tool in morphometric analysis of drainage basin</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 FOUR SUB USING REMOTE SENSING AND GIS TECHNIQUES MORPHOMETRIC ANALYSIS OF FOUR SUB-WATERSHEDS IN BAH AREA OF AGRA DISTRICT USING REMOTE SENSING AND GIS TECHNIQUES About the Author: WATERSHEDS IN BAH AREA OF AGRA DISTRICT","attachmentId":50497131,"attachmentType":"pdf","work_url":"https://www.academia.edu/30045118/MORPHOMETRIC_ANALYSIS_OF_FOUR_SUB_USING_REMOTE_SENSING_AND_GIS_TECHNIQUES_MORPHOMETRIC_ANALYSIS_OF_FOUR_SUB_WATERSHEDS_IN_BAH_AREA_OF_AGRA_DISTRICT_USING_REMOTE_SENSING_AND_GIS_TECHNIQUES_About_the_Author_WATERSHEDS_IN_BAH_AREA_OF_AGRA_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/30045118/MORPHOMETRIC_ANALYSIS_OF_FOUR_SUB_USING_REMOTE_SENSING_AND_GIS_TECHNIQUES_MORPHOMETRIC_ANALYSIS_OF_FOUR_SUB_WATERSHEDS_IN_BAH_AREA_OF_AGRA_DISTRICT_USING_REMOTE_SENSING_AND_GIS_TECHNIQUES_About_the_Author_WATERSHEDS_IN_BAH_AREA_OF_AGRA_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="5" data-entity-id="35523364" 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/35523364/APPLICATION_OF_RS_AND_GIS_TECHNIQUES_IN_THE_ANALYSIS_OF_MORPHOMETRIC_CHARACTERISTICS_OF_UPPER_BERACH_RIVER_BASIN_RAJASTHAN_STATE">APPLICATION OF RS AND GIS TECHNIQUES IN THE ANALYSIS OF MORPHOMETRIC CHARACTERISTICS OF UPPER BERACH RIVER BASIN, RAJASTHAN STATE</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--abstract ds2-5-body-sm">Natural resource conservation and its sustainable planning and development of a river basin can be done satisfactory by morphometric characteristics analysis. In the present study, Survey of India toposheets no. 45H/9, 45H/10, 45H/13, 45H/14, 45L/1 and 45L/2, were used to evaluate hydro morphometric characteristics (viz. Linear, aerial and relief) of Upper Berach river basin in GIS environment using the ARC GIS 10.1 software. Results reveals that the total area of river basin covers 1095.98 km2, which divided in two sub-basins, covers the area of 431.08 and 664.90 km 2 respectively. Dendritic to sub-dendritic drainage pattern with stream orders of sub-basins, are found with ranged from VI to VII orders. Sub-basin stream length ratios are changing haphazardly which is indicating differences in slope and topographic conditions. Mean bifurcation ratio values vary from 3.28 to 4.13. Drainage density shows variation from 1.77 to 1.84 km/km 2 in the whole river basin and sub-basins. The values of form factor and circularity ratio are varied from 0.15 to 0.23 and 0.24 to 0.47, in the whole river basin and sub-basins The ruggedness number of river basins, sub-basin-1 and sub-basin-2 are 0.83, 0.40 and 0.83.</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":"APPLICATION OF RS AND GIS TECHNIQUES IN THE ANALYSIS OF MORPHOMETRIC CHARACTERISTICS OF UPPER BERACH RIVER BASIN, RAJASTHAN STATE","attachmentId":55388603,"attachmentType":"pdf","work_url":"https://www.academia.edu/35523364/APPLICATION_OF_RS_AND_GIS_TECHNIQUES_IN_THE_ANALYSIS_OF_MORPHOMETRIC_CHARACTERISTICS_OF_UPPER_BERACH_RIVER_BASIN_RAJASTHAN_STATE","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/35523364/APPLICATION_OF_RS_AND_GIS_TECHNIQUES_IN_THE_ANALYSIS_OF_MORPHOMETRIC_CHARACTERISTICS_OF_UPPER_BERACH_RIVER_BASIN_RAJASTHAN_STATE"><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="66474928" 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/66474928/A_GIS_based_morphometric_analysis_of_Kandaihimmat_watershed_Hoshangabad_district_M_P_India">A GIS-based morphometric analysis of Kandaihimmat watershed, Hoshangabad district, M.P. 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="34178524" href="https://independent.academia.edu/subzarMalik">subzar Malik</a></div><p class="ds-related-work--metadata ds2-5-body-xs">2018</p><p class="ds-related-work--abstract ds2-5-body-sm">A GIS based morphometric analysis of Kandaihimmat Watershed, which is a part of Tawa river basin of Hoshangabad district, Madhya Pradesh India, was carried out in the study. Drainage map of the watershed was prepared from Survey of India Toposheets (SOI) No.55 F/14 on scale 1: 50,000. Drainage pattern of watershed exhibits dendritic to the sub-dendritic pattern. The stream order range from I to Vth order. Morphometric parameters viz; number and length of streams, drainage density, drainage frequency, bifurcation and texture ratio were calculated. The shape parameters also determined include form factor, circularity and elongation ratio and basin relief. High drainage density (2.67 km/km2) of the watershed is the signature of impermeable subsoil material, sparse vegetation and high relief. High texture ratio indicates high runoff and high erosion potential of the watershed. Bifurcation, elongation, circularity ratio and form factor indicate shape of the basin as elongated to nearly c...</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 GIS-based morphometric analysis of Kandaihimmat watershed, Hoshangabad district, M.P. India","attachmentId":77651910,"attachmentType":"pdf","work_url":"https://www.academia.edu/66474928/A_GIS_based_morphometric_analysis_of_Kandaihimmat_watershed_Hoshangabad_district_M_P_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/66474928/A_GIS_based_morphometric_analysis_of_Kandaihimmat_watershed_Hoshangabad_district_M_P_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="7" data-entity-id="124763828" 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/124763828/Morphometric_Analysis_of_Panzara_River_Basin_Watershed_Maharashtra_India_Using_Geospatial_Approach">Morphometric Analysis of Panzara River Basin Watershed, Maharashtra, India Using Geospatial 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="80025315" href="https://hnbgarhwal.academia.edu/FirozKhan">Firoz Khan</a></div><p class="ds-related-work--metadata ds2-5-body-xs">2024</p><p class="ds-related-work--abstract ds2-5-body-sm">This work aims to deal with the morphometric analysis of the Panzara River Basin (PRB) watershed, a tributary of the Tapi River in Maharashtra, India. In this study, Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) Digital Elevation Model (DEM) and Survey of India (SOI) toposheets have been used along with various parameters like linear, areal, and relief aspects in Geographical Information System (GIS) environment. Out of total 293 number of streams in the watershed, 226, 54, 12, and 1 are of first, second, third and fourth orders respectively. PRB watershed is of 4th order and less elongated in shape, having lower peak flows of longer duration with dendritic pattern and having coarse drainage texture. The bifurcation ratio lies between 6 and 7, indicating that geological structure doesn't have more influence on drainage patterns. The area forms a rugged topography having an elevation range from 123 to 1199 m above Mean Sea Level (MSL). Variables like Stream Frequency and Drainage Density shows impermeable surface of PRB watershed which causes higher water discharge volume and speed in the basin so that the probability is maximum for frequent floods. The results indicates that PRB is having high slope in SW part as compare to NE part and having very low gradient ratio. These variables also shows a temporal variation in the water flowing speed in the stream when the flood reaches its peak. The outcomes of this work can suggest and recommend a better mechanism for proper watershed management in the PRB.</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 Panzara River Basin Watershed, Maharashtra, India Using Geospatial Approach","attachmentId":118928598,"attachmentType":"pdf","work_url":"https://www.academia.edu/124763828/Morphometric_Analysis_of_Panzara_River_Basin_Watershed_Maharashtra_India_Using_Geospatial_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/124763828/Morphometric_Analysis_of_Panzara_River_Basin_Watershed_Maharashtra_India_Using_Geospatial_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="8" data-entity-id="34240305" 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/34240305/A_GIS_based_approach_in_drainage_morphometric_analysis_of_Kanhar_River_Basin_India">A GIS-based approach in drainage morphometric analysis of Kanhar River Basin, 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="49980113" href="https://independent.academia.edu/VarunMishra29">Varun Mishra</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Applied Water Science, 2014</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 GIS-based approach in drainage morphometric analysis of Kanhar River Basin, India","attachmentId":54154123,"attachmentType":"pdf","work_url":"https://www.academia.edu/34240305/A_GIS_based_approach_in_drainage_morphometric_analysis_of_Kanhar_River_Basin_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/34240305/A_GIS_based_approach_in_drainage_morphometric_analysis_of_Kanhar_River_Basin_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="86853142" 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/86853142/Quantitative_analysis_of_the_morphometric_characteristics_of_Arpa_River_Basin_ARB_Chhattisgarh_India">Quantitative analysis of the morphometric characteristics of Arpa River Basin (ARB), Chhattisgarh, 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="163590072" href="https://independent.academia.edu/JKOSHALE">JAI PRAKASH KOSHALE</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="237671534" href="https://independent.academia.edu/AnupamaMahato7">Anupama Mahato</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Indian Hydrobiology, 2022</p><p class="ds-related-work--abstract ds2-5-body-sm">Morphometric analysis is a quantitative measurement and mathematical analysis of a drainage basin in terms of the terrain feature and its flow patterns. The morphometric characterization of the drainage system is essential to study the detailed hydrological behavior of each river basin. In the present study, an attempt has been made to determine the morphometric characteristics of the Arpa River Basin (ARB), a watershed of Sheonath River that constitutes a part of the Mahanadi River Basin. The entire ARB has been divided into 6 major sub basins and various linear, areal and relief has been carried out to understand the spatial variations in morphometric parameters and evaluate the hydrological, topographical and geological properties. This study was performed using the hydrology tool in GIS environment. The ARB comprises of dendritic drainage pattern with the maximum number of flows found in first order. Circulatory ratio (0.12) depicts an elongated shape of Arpa River basin. The mean bifurcation ratio (5.71) confirms that the drainage pattern is not affected by its structural disturbances. The study will be helpful for management of water catchment areas, agricultural land use planning, sustainable water utilization by industrial facilities as well as for studies on hazard 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":"Quantitative analysis of the morphometric characteristics of Arpa River Basin (ARB), Chhattisgarh, India","attachmentId":91215401,"attachmentType":"pdf","work_url":"https://www.academia.edu/86853142/Quantitative_analysis_of_the_morphometric_characteristics_of_Arpa_River_Basin_ARB_Chhattisgarh_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/86853142/Quantitative_analysis_of_the_morphometric_characteristics_of_Arpa_River_Basin_ARB_Chhattisgarh_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":70703659,"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":70703659,"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_70703659" 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. You can download the paper by clicking the button above.</p></div></div></div></div><div class="ds-sidebar--container js-work-sidebar"><div class="ds-related-content--container"><h2 class="ds-related-content--heading">Related papers</h2><div class="ds-related-work--container js-related-work-sidebar-card" data-collection-position="0" data-entity-id="38137584" data-sort-order="default"><a class="ds-related-work--title js-related-work-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-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" 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Western Maharashtra, India using Geospatial Techniques</a><div class="ds-related-work--metadata"><a class="js-related-work-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="31493941" href="https://irjet.academia.edu/IRJET">IRJET Journal</a></div><p class="ds-related-work--metadata ds2-5-body-xs">IRJET, 2021</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":"IRJET- Geo-Morphometric Assessment of Nandani River Basin, Western Maharashtra, India using Geospatial Techniques","attachmentId":68914760,"attachmentType":"pdf","work_url":"https://www.academia.edu/51052519/IRJET_Geo_Morphometric_Assessment_of_Nandani_River_Basin_Western_Maharashtra_India_using_Geospatial_Techniques","alternativeTracking":true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span 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