2016
DOI: 10.1007/s40808-016-0192-9
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Groundwater recharge potential zones mapping in upper Manimuktha Sub basin Vellar river Tamil Nadu India using GIS and remote sensing techniques

Abstract: An attempt has been made to assess the groundwater recharge potential zones in Upper Manimuktha sub basin, Vellar river, Tamil Nadu. Groundwater recharge denotes to the entry of water from the unsaturated zone into the saturated zone below the water table surface, together with the associated movement away from the water table within the saturated zone. This study mainly focus the many factors that control the occurrence and movement of groundwater in a hardrock region including topography, Geology, lineament,… Show more

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Cited by 80 publications
(39 citation statements)
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“…A number of studies on various aspects of groundwater exploration and assessment using RS and GIS techniques have been performed (e.g., Bilal and Ammar 2002;Kumar et al 2007;Al Saud 2010;Adiat et al 2012;Konkul et al 2014;Samson and Elangovan 2015;Deepa et al 2016). It was observed in numerous situations that the reliability of results is not consistent.…”
Section: Introductionmentioning
confidence: 99%
“…A number of studies on various aspects of groundwater exploration and assessment using RS and GIS techniques have been performed (e.g., Bilal and Ammar 2002;Kumar et al 2007;Al Saud 2010;Adiat et al 2012;Konkul et al 2014;Samson and Elangovan 2015;Deepa et al 2016). It was observed in numerous situations that the reliability of results is not consistent.…”
Section: Introductionmentioning
confidence: 99%
“…For the determination of preferential zones for infiltration/recharge, we calculated qualitative maps of the recharge potential (compare to Muir and Johnson, 1979;Shaban et al, 2006;Deepa et al, 2016) in ArcGIS 10.3 by a weighted linear combination of surface-subsurface properties that influence water infiltration and percolation. The input raster data sets and the respective weight factors were chosen based on expert knowledge and the best fit to measured soil hydraulic conductivities: aquifer storey overburden thickness (40 %), type of bedrock (limestone-dominated vs. marlstonedominated strata; 15 %), soil classes (15 %), fracture/karst zones (10 %), vegetation and type of land management (10 %), soil thickness (5 %) and slope angle classes (5 %).…”
Section: Groundwater Recharge Potential Mapmentioning
confidence: 99%
“…The geological feature can also influence water infiltra-120 tion if the rock formations are porous or include faults (Deepa et al 2016). For this reason, when SW is disposed of above susceptible geological formations, instability of the containment systems and the waste mass may occur resulting in potential contamination of the surrounding surface and sub surface soils and water.…”
Section: Geologymentioning
confidence: 99%