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Tejaswi Lakkundi | Karnatak University, Dharwad - Academia.edu
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class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/1917595/Geo_electrical_approach_for_groundwater_prospecting_in_Deccan_Trap_terrain_around_Mudalgi_village_Gokak_taluk_Belgaum_district_Karnataka">Geo-electrical approach for groundwater prospecting in Deccan Trap terrain around Mudalgi village, Gokak taluk, Belgaum district, Karnataka</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="dd672f0e233d412f428f4acb53869c64" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":27454720,"asset_id":1917595,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/27454720/download_file?st=MTczMjc3NDQzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa 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})(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "dd672f0e233d412f428f4acb53869c64" } } $('.js-work-strip[data-work-id=1917595]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":1917595,"title":"Geo-electrical approach for groundwater prospecting in Deccan Trap terrain around Mudalgi village, Gokak taluk, Belgaum district, Karnataka","translated_title":"","metadata":{"more_info":"ISSN 0974-5904","journal_name":"International Journal of Earth Sciences and Engineering","grobid_abstract":"Geo-electrical approach plays a vital role in groundwater prospecting and proved to be most successful. The hard rock terrain of the Deccan basalt is not always easy for targeting groundwater. An attempt has been made to decipher groundwater potential zones in the semi-arid basaltic terrain around Mudalgi village. The area falls under Ghataprabha command area and is irrigated by a network of canals for almost eight months from June to January. For the remaining period, crops are maintained by dug wells of large diameter extending to a depth to 10 -25m, dug cum bore wells and bore wells. Sugarcane and Maize are the primary commercial crops. The area comprises of cretaceoustertiary Deccan basalts with intertrappeans and red bole beds of varying thicknesses. In the basalts, weathering, fractures, fissures and joints facilitate groundwater accumulation and movement. 25 VES were conducted employing the schlumberger array with 150m maximum AB/2 separation using IGIS resistivity meter to delineate potential zones of groundwater occurrences. Five VES were carried out in the vicinity of successful bore wells to know different layer parameters such as the number of sub-surface layers, their resistivities and thickness, depth of water-bearing zones and depth of bedrock. This data has been used as a reference for interpreting the VES curves obtained in the area. The resistivity measurements were carefully interpreted by using curve matching technique and a computer program \"RESIST\" to recommend suitable locations for drilling. The VES curves are of A, H, K, and KH type and are 3-4 layers of varying resistivity and thickness. The yield of bore wells varies from 500 -2500 gph. Only in few cases wherein jointed massive basalt is encountered at depths, high yield of \u003e 3000 gph is obtained. The layer parameters obtained through interpretation of VES curves corroborates with the lithology of the area in most 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wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/1916527/Spatial_analysis_of_fluoride_concentration_in_groundwaters_of_Shivani_watershed_area_Karnataka_state_South_India_through_geospatial_information_system">Spatial analysis of fluoride concentration in groundwaters of Shivani watershed area, Karnataka state, South India, through geospatial information system</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Hydrogeochemical investigations with emphasis on groundwater fluoride concentrations were carried...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Hydrogeochemical investigations with emphasis on groundwater fluoride concentrations were carried out in the Shivani watershed area, Karnataka, South India. This drought-prone watershed is characterised by poor groundwater potential and is composed of different lithounits like gneisses, migmatites, tonalites, mafics–ultramafics, conglomerates and quartzites. Analysis of spatial variation of groundwater fluoride concentration through the use of GIS technology software platforms like ArcView 3.2a and MapInfo Professional 8.5 has enabled the identification of low-fluoride and high-fluoride areas within the watershed. Geochemical data indicates that 38% of groundwater samples have excessive fluoride concentration which poses a health risk to the population of the area. Correlation studies indicate that higher groundwater alkalinity activates leaching of fluoride resulting in elevated concentrations of fluoride. No other significant geochemical interrelationship could be identified between fluoride and rest of the physico-chemical parameters owing to the lack of any significant correlation coefficients. This holds good in the case of both low-fluoride (<1.5 mg/L) and high-fluoride (>1.5 mg/L) groundwaters of the watershed. However, differential or non-uniform type (positive or negative) of coefficient of correlation is observed between fluoride at different levels and other physico-chemical parameters. Among the different lithounits of the study area, gneisses house comparatively more number of high-fluoride groundwaters. Fluoride-bearing minerals biotite, hornblende and apatite are the probable natural sources of groundwater fluoride.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="64eaa8285c53b7a275cce415db925822" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":30254105,"asset_id":1916527,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/30254105/download_file?st=MTczMjc3NDQzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="1916527"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="1916527"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 1916527; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=1916527]").text(description); $(".js-view-count[data-work-id=1916527]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 1916527; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='1916527']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 1916527, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "64eaa8285c53b7a275cce415db925822" } } $('.js-work-strip[data-work-id=1916527]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":1916527,"title":"Spatial analysis of fluoride concentration in groundwaters of Shivani watershed area, Karnataka state, South India, through geospatial information system","translated_title":"","metadata":{"abstract":"Hydrogeochemical investigations with emphasis on groundwater fluoride concentrations were carried out in the Shivani watershed area, Karnataka, South India. 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This holds good in the case of both low-fluoride (\u003c1.5 mg/L) and high-fluoride (\u003e1.5 mg/L) groundwaters of the watershed. However, differential or non-uniform type (positive or negative) of coefficient of correlation is observed between fluoride at different levels and other physico-chemical parameters. Among the different lithounits of the study area, gneisses house comparatively more number of high-fluoride groundwaters. Fluoride-bearing minerals biotite, hornblende and apatite are the probable natural sources of groundwater fluoride.","publisher":"Springer","journal_name":"Environmental Earth Sciences","publication_date":{"day":1,"month":1,"year":2012,"errors":{}}},"translated_abstract":"Hydrogeochemical investigations with emphasis on groundwater fluoride concentrations were carried out in the Shivani watershed area, Karnataka, South India. This drought-prone watershed is characterised by poor groundwater potential and is composed of different lithounits like gneisses, migmatites, tonalites, mafics–ultramafics, conglomerates and quartzites. Analysis of spatial variation of groundwater fluoride concentration through the use of GIS technology software platforms like ArcView 3.2a and MapInfo Professional 8.5 has enabled the identification of low-fluoride and high-fluoride areas within the watershed. Geochemical data indicates that 38% of groundwater samples have excessive fluoride concentration which poses a health risk to the population of the area. Correlation studies indicate that higher groundwater alkalinity activates leaching of fluoride resulting in elevated concentrations of fluoride. No other significant geochemical interrelationship could be identified between fluoride and rest of the physico-chemical parameters owing to the lack of any significant correlation coefficients. This holds good in the case of both low-fluoride (\u003c1.5 mg/L) and high-fluoride (\u003e1.5 mg/L) groundwaters of the watershed. However, differential or non-uniform type (positive or negative) of coefficient of correlation is observed between fluoride at different levels and other physico-chemical parameters. Among the different lithounits of the study area, gneisses house comparatively more number of high-fluoride groundwaters. 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Absracts by Tejaswi Lakkundi</h3></div><div class="js-work-strip profile--work_container" data-work-id="1916522"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/1916522/Excessive_Fluoride_in_Groundwaters_of_River_Sindhanur_Catchment_South_India_A_Case_Study_from_a_Hard_Rock_Sub_Basin_with_Contrasting_Features"><img alt="Research paper thumbnail of Excessive Fluoride in Groundwaters of River Sindhanur Catchment, South India: A Case Study from a Hard-Rock Sub-Basin with Contrasting Features" class="work-thumbnail" src="https://attachments.academia-assets.com/27425851/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/1916522/Excessive_Fluoride_in_Groundwaters_of_River_Sindhanur_Catchment_South_India_A_Case_Study_from_a_Hard_Rock_Sub_Basin_with_Contrasting_Features">Excessive Fluoride in Groundwaters of River Sindhanur Catchment, South India: A Case Study from a Hard-Rock Sub-Basin with Contrasting Features</a></div><div class="wp-workCard_item"><span>IAHS-AISH publication</span><span>, Jan 1, 2010</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3770f9b9bcc1ba2d74db6e4c99aac2f1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":27425851,"asset_id":1916522,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/27425851/download_file?st=MTczMjc3NDQzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action 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Drinking Water ...","url":"https://www.academia.edu/Documents/in/Environmental_and_Economic_Impact_of_Fluoride_in_Drinking_Water_.."},{"id":511726,"name":"Ground Water Pollution","url":"https://www.academia.edu/Documents/in/Ground_Water_Pollution"},{"id":705183,"name":"Fluoride Toxicity","url":"https://www.academia.edu/Documents/in/Fluoride_Toxicity"},{"id":808868,"name":"Fluoride in Groundwater","url":"https://www.academia.edu/Documents/in/Fluoride_in_Groundwater"},{"id":992286,"name":"Ground and Surface Water Quality and Hydrology","url":"https://www.academia.edu/Documents/in/Ground_and_Surface_Water_Quality_and_Hydrology"}],"urls":[{"id":332587,"url":"http://iahs.info/conferences/2010Kovacs_Abstracts/KovacsX_Lakkundi.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="profile--tab_heading_container js-section-heading" data-section="Abstracts" id="Abstracts"><h3 class="profile--tab_heading_container">Abstracts by Tejaswi Lakkundi</h3></div><div class="js-work-strip profile--work_container" data-work-id="4374627"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4374627/Geochemical_appraisal_of_fluoride_contamination_of_groundwaters_of_river_Sindhanur_sub_basin_Koppal_and_Raichur_districts_Karnataka"><img alt="Research paper thumbnail of Geochemical appraisal of fluoride contamination of groundwaters of river Sindhanur sub-basin, Koppal and Raichur districts, Karnataka " class="work-thumbnail" src="https://attachments.academia-assets.com/31811979/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/4374627/Geochemical_appraisal_of_fluoride_contamination_of_groundwaters_of_river_Sindhanur_sub_basin_Koppal_and_Raichur_districts_Karnataka">Geochemical appraisal of fluoride contamination of groundwaters of river Sindhanur sub-basin, Koppal and Raichur districts, Karnataka </a></div><div class="wp-workCard_item"><span>33 International Geological Congress</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="db64ef0eb612f847d748271b4f666eea" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":31811979,"asset_id":4374627,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/31811979/download_file?st=MTczMjc3NDQzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner 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window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "db64ef0eb612f847d748271b4f666eea" } } $('.js-work-strip[data-work-id=4374627]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":4374627,"title":"Geochemical appraisal of fluoride contamination of groundwaters of river Sindhanur sub-basin, Koppal and Raichur districts, Karnataka ","translated_title":"","metadata":{"location":"Oslo, Norway","publisher":"33 International Geological Congress","grobid_abstract":"River Sindhanur sub-basin lies in the hard rock terrain of Raichur and Koppal districts of northern Karnataka. Archaean peninsular gneisses in the central part and Proterozoic basic metamorphosed volcanics of the Hutti and Hungund schist belts lying on both sides of the gneisses are the primary lithounits. Grey and pink granites are next in order of abundance. The sub-basin covers an area of 1171 sq.km. The area is arid and frequently drought prone with a maximum temperature of 43-45 degree Celsius in the summers. Eastern part of the study area is heavily irrigated by the Tungabhadra left bank main canal and its distributaries. Paddy is the main crop grown. The quality of groundwaters varies considerably within short distances. Groundwaters from the gneissic and irrigated area are characterized by elevated levels of fluoride. Fluoride levels range from a minimum of 0.34mg/l to 9.59mg/l and more than 55 percent of the area is affected by fluoride hazard, including many areas with metavolcanics, which may be attributed to groundwater migration from fluoride rich groundwaters of gneissic areas. The fluoride content in groundwaters show moderate to weakly negative correlation with calcium, sulphate, chloride, magnesium, total hardness, total dissolved solids and electrical conductivity whereas, the correlation is moderate to strongly positive with pH, carbonates and bicarbonates. Sodium and potassium show weak to moderately negative correlation with fluoride. Geochemical studies have indicated that the chemistry of groundwaters is mainly controlled by evaporation and rock interaction and more than 50 percent of the collected samples are unfit for irrigation. Consumption of fluoride rich groundwaters has resulted in fluorosis related diseases in the humans. Probable sources and causes for elevated fluoride levels in the groundwaters are discussed in this paper.","publication_name":"33 International Geological 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profile--work_container" data-work-id="3643462"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/3643462/Groundwater_Exploration_Traditional_and_Scientific_Methods"><img alt="Research paper thumbnail of Groundwater Exploration: Traditional and Scientific Methods" class="work-thumbnail" src="https://attachments.academia-assets.com/31337307/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/3643462/Groundwater_Exploration_Traditional_and_Scientific_Methods">Groundwater Exploration: Traditional and Scientific Methods</a></div><div class="wp-workCard_item"><span>Suvarna Karnataka Maale 20- Ratna Garbha Vasundhara</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="cc88dda5a3e6c7026605bd954d303a3e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":31337307,"asset_id":3643462,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/31337307/download_file?st=MTczMjc3NDQzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="3643462"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="3643462"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3643462; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3643462]").text(description); $(".js-view-count[data-work-id=3643462]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 3643462; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='3643462']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); 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</script> <div class="profile--tab_heading_container js-section-heading" data-section="Conference Presentations" id="Conference Presentations"><h3 class="profile--tab_heading_container">Conference Presentations by Tejaswi Lakkundi</h3></div><div class="js-work-strip profile--work_container" data-work-id="10226065"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/10226065/Impact_of_Agriculture_on_Groundwater_Around_Mahalingpur_Area_Mudhol_Taluka_Bagalkot_District_Karnataka"><img alt="Research paper thumbnail of Impact of Agriculture on Groundwater Around Mahalingpur Area, Mudhol Taluka, Bagalkot District, Karnataka" class="work-thumbnail" src="https://attachments.academia-assets.com/36320393/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" 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The hard rock terrain of the Deccan basalt is not always easy for targeting groundwater. An attempt has been made to decipher groundwater potential zones in the semi-arid basaltic terrain around Mudalgi village. The area falls under Ghataprabha command area and is irrigated by a network of canals for almost eight months from June to January. For the remaining period, crops are maintained by dug wells of large diameter extending to a depth to 10 -25m, dug cum bore wells and bore wells. Sugarcane and Maize are the primary commercial crops. The area comprises of cretaceoustertiary Deccan basalts with intertrappeans and red bole beds of varying thicknesses. In the basalts, weathering, fractures, fissures and joints facilitate groundwater accumulation and movement. 25 VES were conducted employing the schlumberger array with 150m maximum AB/2 separation using IGIS resistivity meter to delineate potential zones of groundwater occurrences. Five VES were carried out in the vicinity of successful bore wells to know different layer parameters such as the number of sub-surface layers, their resistivities and thickness, depth of water-bearing zones and depth of bedrock. This data has been used as a reference for interpreting the VES curves obtained in the area. The resistivity measurements were carefully interpreted by using curve matching technique and a computer program \"RESIST\" to recommend suitable locations for drilling. The VES curves are of A, H, K, and KH type and are 3-4 layers of varying resistivity and thickness. The yield of bore wells varies from 500 -2500 gph. Only in few cases wherein jointed massive basalt is encountered at depths, high yield of \u003e 3000 gph is obtained. The layer parameters obtained through interpretation of VES curves corroborates with the lithology of the area in most 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wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/1916527/Spatial_analysis_of_fluoride_concentration_in_groundwaters_of_Shivani_watershed_area_Karnataka_state_South_India_through_geospatial_information_system">Spatial analysis of fluoride concentration in groundwaters of Shivani watershed area, Karnataka state, South India, through geospatial information system</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Hydrogeochemical investigations with emphasis on groundwater fluoride concentrations were carried...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Hydrogeochemical investigations with emphasis on groundwater fluoride concentrations were carried out in the Shivani watershed area, Karnataka, South India. This drought-prone watershed is characterised by poor groundwater potential and is composed of different lithounits like gneisses, migmatites, tonalites, mafics–ultramafics, conglomerates and quartzites. Analysis of spatial variation of groundwater fluoride concentration through the use of GIS technology software platforms like ArcView 3.2a and MapInfo Professional 8.5 has enabled the identification of low-fluoride and high-fluoride areas within the watershed. Geochemical data indicates that 38% of groundwater samples have excessive fluoride concentration which poses a health risk to the population of the area. Correlation studies indicate that higher groundwater alkalinity activates leaching of fluoride resulting in elevated concentrations of fluoride. No other significant geochemical interrelationship could be identified between fluoride and rest of the physico-chemical parameters owing to the lack of any significant correlation coefficients. This holds good in the case of both low-fluoride (<1.5 mg/L) and high-fluoride (>1.5 mg/L) groundwaters of the watershed. However, differential or non-uniform type (positive or negative) of coefficient of correlation is observed between fluoride at different levels and other physico-chemical parameters. Among the different lithounits of the study area, gneisses house comparatively more number of high-fluoride groundwaters. Fluoride-bearing minerals biotite, hornblende and apatite are the probable natural sources of groundwater fluoride.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="64eaa8285c53b7a275cce415db925822" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":30254105,"asset_id":1916527,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/30254105/download_file?st=MTczMjc3NDQzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="1916527"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="1916527"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 1916527; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=1916527]").text(description); $(".js-view-count[data-work-id=1916527]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 1916527; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='1916527']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 1916527, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "64eaa8285c53b7a275cce415db925822" } } $('.js-work-strip[data-work-id=1916527]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":1916527,"title":"Spatial analysis of fluoride concentration in groundwaters of Shivani watershed area, Karnataka state, South India, through geospatial information system","translated_title":"","metadata":{"abstract":"Hydrogeochemical investigations with emphasis on groundwater fluoride concentrations were carried out in the Shivani watershed area, Karnataka, South India. This drought-prone watershed is characterised by poor groundwater potential and is composed of different lithounits like gneisses, migmatites, tonalites, mafics–ultramafics, conglomerates and quartzites. Analysis of spatial variation of groundwater fluoride concentration through the use of GIS technology software platforms like ArcView 3.2a and MapInfo Professional 8.5 has enabled the identification of low-fluoride and high-fluoride areas within the watershed. Geochemical data indicates that 38% of groundwater samples have excessive fluoride concentration which poses a health risk to the population of the area. Correlation studies indicate that higher groundwater alkalinity activates leaching of fluoride resulting in elevated concentrations of fluoride. No other significant geochemical interrelationship could be identified between fluoride and rest of the physico-chemical parameters owing to the lack of any significant correlation coefficients. This holds good in the case of both low-fluoride (\u003c1.5 mg/L) and high-fluoride (\u003e1.5 mg/L) groundwaters of the watershed. However, differential or non-uniform type (positive or negative) of coefficient of correlation is observed between fluoride at different levels and other physico-chemical parameters. Among the different lithounits of the study area, gneisses house comparatively more number of high-fluoride groundwaters. Fluoride-bearing minerals biotite, hornblende and apatite are the probable natural sources of groundwater fluoride.","publisher":"Springer","journal_name":"Environmental Earth Sciences","publication_date":{"day":1,"month":1,"year":2012,"errors":{}}},"translated_abstract":"Hydrogeochemical investigations with emphasis on groundwater fluoride concentrations were carried out in the Shivani watershed area, Karnataka, South India. This drought-prone watershed is characterised by poor groundwater potential and is composed of different lithounits like gneisses, migmatites, tonalites, mafics–ultramafics, conglomerates and quartzites. Analysis of spatial variation of groundwater fluoride concentration through the use of GIS technology software platforms like ArcView 3.2a and MapInfo Professional 8.5 has enabled the identification of low-fluoride and high-fluoride areas within the watershed. Geochemical data indicates that 38% of groundwater samples have excessive fluoride concentration which poses a health risk to the population of the area. Correlation studies indicate that higher groundwater alkalinity activates leaching of fluoride resulting in elevated concentrations of fluoride. No other significant geochemical interrelationship could be identified between fluoride and rest of the physico-chemical parameters owing to the lack of any significant correlation coefficients. This holds good in the case of both low-fluoride (\u003c1.5 mg/L) and high-fluoride (\u003e1.5 mg/L) groundwaters of the watershed. However, differential or non-uniform type (positive or negative) of coefficient of correlation is observed between fluoride at different levels and other physico-chemical parameters. Among the different lithounits of the study area, gneisses house comparatively more number of high-fluoride groundwaters. Fluoride-bearing minerals biotite, hornblende and apatite are the probable natural sources of groundwater fluoride.","internal_url":"https://www.academia.edu/1916527/Spatial_analysis_of_fluoride_concentration_in_groundwaters_of_Shivani_watershed_area_Karnataka_state_South_India_through_geospatial_information_system","translated_internal_url":"","created_at":"2012-09-07T04:52:17.830-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":2456695,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":30254105,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/30254105/thumbnails/1.jpg","file_name":"Springer_Publication_Abstract___Author_Proof.pdf","download_url":"https://www.academia.edu/attachments/30254105/download_file?st=MTczMjc3NDQzNSw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Spatial_analysis_of_fluoride_concentrati.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/30254105/Springer_Publication_Abstract___Author_Proof-libre.pdf?1390882069=\u0026response-content-disposition=attachment%3B+filename%3DSpatial_analysis_of_fluoride_concentrati.pdf\u0026Expires=1732745279\u0026Signature=Gd9h0IF9Rzm8aFP-cVJYlczTUKK1~9UDa1-t83e7YylnPwTyFI2L4m-6~4k2QQkPTe5Ij~5N9Eif48PVtt6dmkvj5rR-oFaQuQ~A-GuJ~0rc5s5ujAZz9q3WDglc3RLhqeVw~Cp~Pm0hDxogcNIMuaKbj0v-iPIUcN56gQwDhzIw8y8OVHbs-pUUxJOnSTN0E0gadzrX2AMatIBpT4MG4mIv~of1AFj-S776dfyYUyysy3IqVFY8SrLPNJoa5Ae0-bb~Q4ox0rYnO547jSpOJu71YF7IRwvGAgvCh1qLMCqLJeDOYWMiuMas5ghlIUNRV~S-J-V66fgevvxkqO7rXQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Spatial_analysis_of_fluoride_concentration_in_groundwaters_of_Shivani_watershed_area_Karnataka_state_South_India_through_geospatial_information_system","translated_slug":"","page_count":11,"language":"en","content_type":"Work","owner":{"id":2456695,"first_name":"Tejaswi","middle_initials":null,"last_name":"Lakkundi","page_name":"TejaswaiL","domain_name":"kud-in","created_at":"2012-09-07T04:35:56.963-07:00","display_name":"Tejaswi 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data-work-id="1916522"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/1916522/Excessive_Fluoride_in_Groundwaters_of_River_Sindhanur_Catchment_South_India_A_Case_Study_from_a_Hard_Rock_Sub_Basin_with_Contrasting_Features"><img alt="Research paper thumbnail of Excessive Fluoride in Groundwaters of River Sindhanur Catchment, South India: A Case Study from a Hard-Rock Sub-Basin with Contrasting Features" class="work-thumbnail" src="https://attachments.academia-assets.com/27425851/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/1916522/Excessive_Fluoride_in_Groundwaters_of_River_Sindhanur_Catchment_South_India_A_Case_Study_from_a_Hard_Rock_Sub_Basin_with_Contrasting_Features">Excessive Fluoride in Groundwaters of River Sindhanur Catchment, South India: A Case Study from a Hard-Rock Sub-Basin with Contrasting Features</a></div><div class="wp-workCard_item"><span>IAHS-AISH publication</span><span>, Jan 1, 2010</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3770f9b9bcc1ba2d74db6e4c99aac2f1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":27425851,"asset_id":1916522,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/27425851/download_file?st=MTczMjc3NDQzNSw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action 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id="abstracts"><div class="js-work-strip profile--work_container" data-work-id="4374627"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/4374627/Geochemical_appraisal_of_fluoride_contamination_of_groundwaters_of_river_Sindhanur_sub_basin_Koppal_and_Raichur_districts_Karnataka"><img alt="Research paper thumbnail of Geochemical appraisal of fluoride contamination of groundwaters of river Sindhanur sub-basin, Koppal and Raichur districts, Karnataka " class="work-thumbnail" src="https://attachments.academia-assets.com/31811979/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" 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Archaean peninsular gneisses in the central part and Proterozoic basic metamorphosed volcanics of the Hutti and Hungund schist belts lying on both sides of the gneisses are the primary lithounits. Grey and pink granites are next in order of abundance. The sub-basin covers an area of 1171 sq.km. The area is arid and frequently drought prone with a maximum temperature of 43-45 degree Celsius in the summers. Eastern part of the study area is heavily irrigated by the Tungabhadra left bank main canal and its distributaries. Paddy is the main crop grown. The quality of groundwaters varies considerably within short distances. Groundwaters from the gneissic and irrigated area are characterized by elevated levels of fluoride. Fluoride levels range from a minimum of 0.34mg/l to 9.59mg/l and more than 55 percent of the area is affected by fluoride hazard, including many areas with metavolcanics, which may be attributed to groundwater migration from fluoride rich groundwaters of gneissic areas. The fluoride content in groundwaters show moderate to weakly negative correlation with calcium, sulphate, chloride, magnesium, total hardness, total dissolved solids and electrical conductivity whereas, the correlation is moderate to strongly positive with pH, carbonates and bicarbonates. Sodium and potassium show weak to moderately negative correlation with fluoride. Geochemical studies have indicated that the chemistry of groundwaters is mainly controlled by evaporation and rock interaction and more than 50 percent of the collected samples are unfit for irrigation. Consumption of fluoride rich groundwaters has resulted in fluorosis related diseases in the humans. Probable sources and causes for elevated fluoride levels in the groundwaters are discussed in this paper.","publication_name":"33 International Geological 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