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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 Documentother common <strong>in</strong>gredient do not produce toxicity Characteristic leachate beyond permissiblelimit. It was suggested that 25% (by volume) <strong>of</strong> cement can be replaced by the fly ash to stabilizearsenic-laden to the tune <strong>of</strong> 11% (by volume <strong>of</strong> cement-mortar. It <strong>in</strong>dicates that arsenic sludgecan also be used/managed effectively for our dem<strong>and</strong> management.C. Potentials <strong>of</strong> deeper aquifers <strong>and</strong> surface water as alternate source<strong>of</strong> dr<strong>in</strong>k<strong>in</strong>g water(i)Potential <strong>of</strong> surface water sourcesSupply <strong>of</strong> surface water from ponds, rivers etc. for dr<strong>in</strong>k<strong>in</strong>g purposes through pipenetwork system after suitable purification by conventional method <strong>of</strong> treatment viz. coagulation,flocculation, rapid s<strong>and</strong> filtration <strong>and</strong> dis<strong>in</strong>fections, as an alternate option, have been put <strong>in</strong>topractice <strong>in</strong> some places <strong>in</strong> West Bengal. Eight such surface water based schemes have beenoperationalized by the West Bengal Government <strong>in</strong> different places, cover<strong>in</strong>g population <strong>of</strong> 3.85million <strong>in</strong> 1266 mouzas. All the surface water based schemes are successfully runn<strong>in</strong>g to providepotable water supply to masses covered under the schemes. In Bihar also, a number <strong>of</strong> surfacewater based pipe water supply schemes with their <strong>in</strong>take from the Ganga River to meet dem<strong>and</strong><strong>of</strong> multi-village supply are under construction. Surface water based schemes are constra<strong>in</strong>ed bynumber <strong>of</strong> factors, namely; (i) technical feasibility, (ii) water availability, (iii) cost factors, etcSurface water sources are not omnipresent, <strong>and</strong>, therefore, cannot be located <strong>and</strong>extended everywhere. Moreover, water <strong>in</strong> some <strong>of</strong> the flow<strong>in</strong>g/ stationary bodies rema<strong>in</strong>s onlyfor a specific period <strong>of</strong> a year <strong>and</strong> cannot form the regular source for public water supplysystem. In addition to that, due to changes <strong>in</strong> the river discharges <strong>and</strong> its flow course, it is difficultto keep a susta<strong>in</strong>able <strong>in</strong>take po<strong>in</strong>t <strong>of</strong> water for the whole year. Most <strong>of</strong> the arsenic affected areas<strong>in</strong> the Ganges are along l<strong>in</strong>ear track <strong>of</strong> the river Ganga <strong>in</strong> U.P., Bihar, <strong>and</strong> Jharkh<strong>and</strong> state <strong>and</strong>along the river Bhagirathi <strong>in</strong> West Bengal, supply <strong>of</strong> potable water from the surface watersources, wherever feasible, can be the most promis<strong>in</strong>g alternative. In areas, where surfacewater supplies are available or can be made available by any water conservation method,surface water based scheme after suitable purification could be the suitable proposition forpotable water supply.(ii)Potentials <strong>of</strong> Deeper AquifersThe arsenic contam<strong>in</strong>ated zones <strong>in</strong> the Ganga-Brahmaputra fluvial pla<strong>in</strong>s mostly lie with<strong>in</strong>the shallow aquifer (100 m bgl) underneath the contam<strong>in</strong>atedshallow aquifer, <strong>in</strong> many places <strong>of</strong> Bengal Delta Pla<strong>in</strong>s, are normally seen arsenic free. Thedeeper aquifer is separated by a thick clay layer <strong>of</strong> appropriate composition from the shallowaquifer. From the isotopic studies carried out <strong>in</strong> West Bengal, it was observed that there was nohydraulic connection between the shallow <strong>and</strong> deep aquifers as they belong to different ageNIH & CGWB 183

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