2019
DOI: 10.1007/s12040-019-1104-y
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Assessment of aquifer zones and its protection via second-order geoelectric indices in parts of drought-prone region of Deccan Volcanic Province, Maharashtra, India

Abstract: , using electrical resistivity technique. The study was also aimed at alleviating the drinking water scarcity in these regions. A total of 118 vertical electrical sounding sites were occupied using Schlumberger electrode configuration and the data analysis revealed two to five layered curve types. The modelled layer resistivity and layer thickness at every station were used to calculate the Dar-Zarrouk parameters (i.e., longitudinal conductance S and transverse resistance T). The S values showed that 67% of th… Show more

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Cited by 12 publications
(4 citation statements)
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“…The anisotropy of rocks can be caused by their fracturing or metamorphism, as well as the presence of disseminated ore grains. Lower values of λ are associated with high aquifer potential zones, according to recent studies by Venkateswara et al (2022), Suneetha et al (2021), andShailaja et al (2019).…”
Section: Introductionmentioning
confidence: 74%
“…The anisotropy of rocks can be caused by their fracturing or metamorphism, as well as the presence of disseminated ore grains. Lower values of λ are associated with high aquifer potential zones, according to recent studies by Venkateswara et al (2022), Suneetha et al (2021), andShailaja et al (2019).…”
Section: Introductionmentioning
confidence: 74%
“…Accordingly, the overburden protective capacity was evaluated using the total longitudinal unit conductance (S). In the studied area lower S values generally indicate a relatively weak succession of fine grain size sediments overburden together with greater proximity to the emission center of the eruption and are given the highest priority in terms of aquifer protection studies as it implies the potential infiltration of contaminants into the aquifer [47].…”
Section: Longitudinal Conductancementioning
confidence: 96%
“…In the Deccan Volcanic Province (DVP) of Maharashtra, secondary porosity and permeability are developed due to weathering and fracturing of rocks (Deolankar, 1980;Rai et al, 2015) which are responsible for groundwater prospects. The unceasing shortage of drinkable water compounded by increasing drought and rising population demands to locate secondary groundwater sources over the hard rock terrains of the DVP of Maharashtra (Shailaja et al, 2019).…”
Section: Introductionmentioning
confidence: 99%