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Mitigation and Remedy of Groundwater Arsenic Menace in India

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> Remediation Update from West Bengal <strong>and</strong> Bihar : Studies <strong>and</strong> Projects Initiated<strong>of</strong> vadose zone, <strong>and</strong> mobilization <strong>of</strong> arsenic <strong>in</strong> the freshwater zones. Ensur<strong>in</strong>g supply <strong>of</strong> potablewater alone, thus, seems to be <strong>in</strong>adequate to atta<strong>in</strong> susta<strong>in</strong>ability <strong>in</strong> terms <strong>of</strong> resolv<strong>in</strong>g the arsenicmenace. It is, therefore, necessary to consider a framework <strong>of</strong> problem-solv<strong>in</strong>g curriculum l<strong>in</strong>k<strong>in</strong>gone issue to another, one's favor<strong>in</strong>g <strong>and</strong> pos<strong>in</strong>g condition to another, <strong>and</strong> resolve thosesystematically <strong>in</strong> a judicious manner to achieve the target <strong>of</strong> human-l<strong>and</strong>-water resources management <strong>in</strong> the arsenic affected areas.4.1.2 F<strong>in</strong>d<strong>in</strong>gs <strong>of</strong> <strong>in</strong>itiated R & D studiesA number <strong>of</strong> research studies have been pursued to <strong>in</strong>vestigate extent, mobilizationprocess, geochemistry, hydro-geological properties <strong>and</strong> processes by different organizations.F<strong>in</strong>d<strong>in</strong>gs <strong>of</strong> various research studies have broadly been discussed <strong>in</strong> chapter-3. The CentralGround Water Board-Eastern Region (CGWB-ER), <strong>in</strong> addition to the above aspects, undertooktasks to identify potential arsenic safe zones aquifer. F<strong>in</strong>d<strong>in</strong>gs <strong>of</strong> CGWB-ER are given below:(i)(ii)(iii)(iv)(v)(vi)Arseniferous aquifers are ma<strong>in</strong>ly observed with<strong>in</strong> the shallow depth (with<strong>in</strong> 100 mbelow ground level), while the deeper aquifer (>100 m bgl) <strong>in</strong> the same area is foundfree from arsenic. The shallow <strong>and</strong> the deeper aquifers are separated by a thickimpervious clay layer <strong>and</strong> the thickness is above 10 m. The deeper aquifer is capable toyield 5 to 20 lps <strong>of</strong> water. It is further observed that when the deeper aquifer is pumpedcreat<strong>in</strong>g a drawdown <strong>of</strong> 6 m, there is not much impact on the overla<strong>in</strong> arseniccontam<strong>in</strong>ated zone.<strong>Groundwater</strong> <strong>in</strong> the arsenic affected area is characterized by high iron, calcium, magnesium, bicarbonate with low chloride, sulphate, fluoride <strong>and</strong> sodium.Geologically, the arsenic affected areas are the parts <strong>of</strong> the Ganga-Bhagirathi deltacompris<strong>in</strong>g succession <strong>of</strong> thick Quaternary sediments. The arseniferous tract is restricted<strong>in</strong> the upper delta pla<strong>in</strong> with<strong>in</strong> shallow depth, which is ma<strong>in</strong>ly built up <strong>of</strong> sedimentsdeposited by me<strong>and</strong>er<strong>in</strong>g streams <strong>and</strong> levees composed <strong>of</strong> s<strong>and</strong>s <strong>of</strong> various grades, silt,clay <strong>and</strong> their admixtures.The groundwater mostly occurs <strong>in</strong> thick zone <strong>of</strong> saturation with<strong>in</strong> the unconsolidatedalluvial sediments <strong>in</strong> the affected areas; <strong>and</strong> the aquifers are made up <strong>of</strong> s<strong>and</strong>s <strong>of</strong> various grades. <strong>Groundwater</strong> occurs generally under unconf<strong>in</strong>ed hydro-geologic conditions.The arsenic groundwater contam<strong>in</strong>ation is attributed to the geogenic orig<strong>in</strong>, <strong>and</strong> thesource <strong>of</strong> arsenic <strong>in</strong> localized patches is due to presence <strong>of</strong> Arsenopyrite <strong>in</strong> clay <strong>and</strong>s<strong>and</strong>. <strong>Arsenic</strong> concentration is more <strong>in</strong> clay than <strong>in</strong> s<strong>and</strong>.In arsenic affected areas, all tube wells harness<strong>in</strong>g shallow aquifers do not yield arseniccontam<strong>in</strong>ated water. Some are arsenic affected <strong>and</strong> some others are free from suchcontam<strong>in</strong>ation.60NIH & CGWB

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