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Mitigation and Remedy of Groundwater Arsenic Menace in India

Mitigation and Remedy of Groundwater Arsenic Menace in India

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<strong>Mitigation</strong> <strong>and</strong> <strong>Remedy</strong> <strong>of</strong> <strong>Groundwater</strong> <strong>Arsenic</strong> <strong>Menace</strong> <strong>in</strong> <strong>India</strong> : A Vision Documentfrom 100-120m to 230-260m bgl. This is separated from the shallow contam<strong>in</strong>ated zoneby an aquitard, which has been found risk free from arsenic. If tapped through deep tubewells, deeper aquifer is estimated to have yield about 150-200 m3/hr <strong>of</strong> water. Thegeological map <strong>and</strong> lithological features <strong>of</strong> the arsenic affected areas are shown <strong>in</strong> Figs.4.6 <strong>and</strong> 4.7, respectively. The lithological features (Fig. 4.7) showed that top soils <strong>of</strong>thickness about 2-5 m comprise clay, s<strong>and</strong>y clay <strong>and</strong> silty clay followed by f<strong>in</strong>e to medium s<strong>and</strong> with occasional s<strong>and</strong> layers, hav<strong>in</strong>g disconnected lenses <strong>of</strong> coarse to verycoarse s<strong>and</strong> with occasional gravel beds. The geological units (Fig.4.6) <strong>of</strong> theseformations can be l<strong>in</strong>ked to Siwaliks, Rajmahal traps, <strong>and</strong> V<strong>in</strong>dhayans ranges.(ii)(iii)A jo<strong>in</strong>t study, by CGWB-MER, Patna <strong>and</strong> BARC, Mumbai, has been carried out to<strong>in</strong>vestigate hydrodynamic behavior <strong>of</strong> arsenic affected aquifers, age <strong>of</strong> arseniccontam<strong>in</strong>ated groundwater, its relationship with the age <strong>of</strong> aquifer water, <strong>and</strong> to studythe mechanism <strong>of</strong> arsenic mobilization. From the analysis <strong>of</strong> major chemical <strong>and</strong> environmental isotopes like Tritium, O 16/O 18<strong>and</strong> radio carbon, it was found that the shallowaquifers, <strong>in</strong>fluenced by arsenic contam<strong>in</strong>ation, are replenished by ra<strong>in</strong>fall recharge, <strong>and</strong>,therefore, shallow aquifers with young groundwater is contam<strong>in</strong>ated (< 40 years). Deeperaquifers, which posses' water <strong>of</strong> much older age (> 3000 years), are arsenic-free. This<strong>in</strong>dicates that deeper aquifers are not <strong>in</strong>fluenced by direct vertical percolation <strong>of</strong> overla<strong>in</strong> strata. A positive correlation between arsenic <strong>and</strong> iron, <strong>and</strong> a concentrateddistribution <strong>of</strong> arsenic <strong>in</strong> bicarbonate rich water, are also observed.In addition to the above studies, several other studies have also been <strong>in</strong>itiated by variousorganizations. GSI-Patna has <strong>in</strong>itiated a study, cover<strong>in</strong>g 2400 sq. km <strong>in</strong> Bhojpur, Buxar<strong>and</strong> Patna districts <strong>and</strong> 1200 sq km area <strong>in</strong> Saran <strong>and</strong> Vaishali districts, to exam<strong>in</strong>edistribution <strong>and</strong> physiochemical behavior <strong>of</strong> arsenic <strong>in</strong> soil-water <strong>and</strong> m<strong>in</strong>eral phases.Deptt. <strong>of</strong> Environment <strong>and</strong> Water Management, A N College, Patna, is study<strong>in</strong>g effects<strong>of</strong> arsenic <strong>in</strong> food cha<strong>in</strong> consider<strong>in</strong>g crop plants, like; wheat, maize, <strong>and</strong> rice irrigated bygroundwater arsenic contam<strong>in</strong>ated water.In short, the outcomes <strong>of</strong> the studies carried out so far are as follows:(a)(b)(c)(d)<strong>Groundwater</strong> arsenic contam<strong>in</strong>ation is conf<strong>in</strong>ed to Newer alluvial belt along the riverGanga,<strong>Arsenic</strong> contam<strong>in</strong>ation is mostly <strong>in</strong> shallow aquifer (

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