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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 Documentamounts <strong>of</strong> toxic sludge, which needs further treatment before disposal <strong>in</strong>to the environment, <strong>and</strong>(ii) they lack <strong>in</strong> proper operation <strong>and</strong> ma<strong>in</strong>tenance policy guidel<strong>in</strong>es. In addition to those, thetreatment devices, <strong>in</strong> many cases, are not economically viable <strong>and</strong> socially acceptable. Theavailable arsenic removal technologies require ref<strong>in</strong>ement to make them suitable <strong>and</strong> susta<strong>in</strong>ablefor their large scale effective uses. Surface waters are free from arsenic contam<strong>in</strong>ation.Although usages <strong>of</strong> surface water sources with m<strong>in</strong>or treatment through organized piped watersupply system seems to be very expensive, it has been proved to be a feasible solution to supplypotable water <strong>in</strong> many places <strong>in</strong> West Bengal, where surface water availability is assured.Moreover, <strong>in</strong>vestigations have revealed that deeper aquifers underneath the contam<strong>in</strong>atedshallow aquifers are free from arsenic contam<strong>in</strong>ation. The deeper aquifers, which are risk freefrom future threat <strong>of</strong> contam<strong>in</strong>ation from the overla<strong>in</strong> aquifer, can provide a susta<strong>in</strong>able source<strong>of</strong> potential groundwater withdrawal. <strong>Groundwater</strong> arsenic contam<strong>in</strong>ation zones <strong>in</strong> most <strong>of</strong> thearsenic affected areas are <strong>in</strong> localized patches. Areas around the arsenic affected patches arefree from arsenic contam<strong>in</strong>ation. Because <strong>of</strong> hydrogeological features <strong>and</strong> fluvial characteristics<strong>of</strong> the groundwater doma<strong>in</strong>, <strong>in</strong> many cases all those freshwater zones are free from threat <strong>of</strong><strong>in</strong>trud<strong>in</strong>g contam<strong>in</strong>ants from the nearby <strong>in</strong>fected zones. Possibility <strong>of</strong> tapp<strong>in</strong>g all those shallowfreshwater zones can be explored. The top most layers <strong>of</strong> the shallow aquifers are rechargedannually by monsoon ra<strong>in</strong>fall. This recharge water rema<strong>in</strong>s free from arsenic for quite a longtime till they are mixed up by natural processes or by any external <strong>in</strong>tervention. Most <strong>of</strong> thearsenic affected areas <strong>in</strong> the Gangetic flood pla<strong>in</strong>s are along l<strong>in</strong>ear track <strong>of</strong> river courses. Riverwater is free from arsenic <strong>and</strong> the river banks possess unique properties <strong>of</strong> filtration, storage <strong>and</strong>transmission <strong>of</strong> water. Explor<strong>in</strong>g possibility <strong>of</strong> tapp<strong>in</strong>g top fresh water zones by radial collectorwells <strong>and</strong> river banks storage by <strong>in</strong>take wells can be one <strong>of</strong> suitable propositions to <strong>in</strong>vestigate.Over <strong>and</strong> above, as such no comprehensive maps del<strong>in</strong>eat<strong>in</strong>g arsenic vulnerable zones <strong>and</strong>potential freshwater zones <strong>of</strong> the arsenic vulnerable areas are available.Recogniz<strong>in</strong>g the above needs <strong>and</strong> their importance, follow<strong>in</strong>g three categorizes <strong>of</strong> R &D programmes are proposed to pursue simultaneously to achieve the goal aga<strong>in</strong>st groundwaterarsenic menace; these are: (i) Laboratory scale R & D programmes, (ii) Field level R & Dprogrammes, <strong>and</strong> (iii) evolv<strong>in</strong>g strategies to translate the techniques <strong>and</strong> technologies to thebenefit <strong>of</strong> the society. The laboratory scale R & Ds should aim at develop<strong>in</strong>g eco-friendly <strong>and</strong>economically viable arsenic removal treatment techniques, species identification <strong>and</strong>knowledgebase generation; while the field level R & D programmes should aim at develop<strong>in</strong>gappropriate methodologies for decontam<strong>in</strong>ation <strong>of</strong> aquifer from arsenic by improvis<strong>in</strong>gunderst<strong>and</strong><strong>in</strong>g <strong>of</strong> geo-chemical behavior, processes <strong>and</strong> mechanisms <strong>of</strong> mobilization, sourceidentification, monitor<strong>in</strong>g <strong>and</strong> mapp<strong>in</strong>g, management <strong>of</strong> aquifer. The third type <strong>of</strong> R & Ds couldaim at develop<strong>in</strong>g strategies as to how techniques <strong>and</strong> technologies can be translated to thesociety for their acceptability <strong>and</strong> susta<strong>in</strong>ability.The detailed outl<strong>in</strong><strong>in</strong>g <strong>of</strong> the three categories <strong>of</strong> R & D activities are illustrated <strong>in</strong> subsequentsection:NIH & CGWB 141

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