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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 Document(i)(ii)(iii)(iv)(v)Sk<strong>in</strong> itch<strong>in</strong>g to sun rays, Burn<strong>in</strong>g <strong>and</strong> water<strong>in</strong>g <strong>of</strong> eyes, Weight loss, Loss <strong>of</strong> appetite,Weakness, Lethargy <strong>and</strong> easily fatigued limited the physical activities <strong>and</strong> work<strong>in</strong>gcapacities.Chronic respiratory compla<strong>in</strong>ts were also common. Chronic cough with or withoutexpectoration was evident <strong>in</strong> more than 50%. As reported by the villagers, the uniquesound <strong>of</strong> "cough <strong>of</strong> arsenicosis" was reported from adjacent village homes at night tocreate an unusual atmosphere. The cough may be pa<strong>in</strong>ful <strong>and</strong> sputum may conta<strong>in</strong> bloodto be misdiagnosed as pulmonary tuberculosis. In late stages, shortness <strong>of</strong> breath mightpredom<strong>in</strong>ate.Gastro<strong>in</strong>test<strong>in</strong>al symptoms <strong>of</strong> anorexia, nausea, dyspepsia, altered taste, pa<strong>in</strong> <strong>in</strong> abdomen, enlarged liver <strong>and</strong> spleen, <strong>and</strong> ascites (collection <strong>of</strong> fluid <strong>in</strong> abdomen) were alsoobserved <strong>in</strong> 50% patients.Moderate to severe anemia was evident <strong>in</strong> some cases.Conjunctival congestion, Leg edema was less common.2.3.3.1 West BengalTable 2.2 shows an overview <strong>of</strong> arsenic contam<strong>in</strong>ation status <strong>in</strong> West Bengal up to2008 (Chakraborti, 2008a). Out <strong>of</strong> 140150 samples analyzed for arsenic, 48.1% had foundarsenic above 10 µg/L <strong>and</strong> 23.8% above 50 µg/L. Importantly, 3.3% <strong>of</strong> the analyzed tube-wellshad arsenic concentrations above 300µg/L, the concentration predict<strong>in</strong>g overt arsenical sk<strong>in</strong>lesions. A total <strong>of</strong> 187 (0.13%) h<strong>and</strong> tube-wells were reported highly contam<strong>in</strong>ated (> 1000 µg/L). The maximum arsenic concentration (3700 µg/L) was found <strong>in</strong> Ramnagar village <strong>of</strong> GPRamnagar II, Baruipur block, <strong>in</strong> South 24-Parganas district. This tubewell was a private one.Figure 2.5 depicts groundwater arsenic contam<strong>in</strong>ation status <strong>of</strong> all 9 districts <strong>of</strong> West Bengal.Table 2.3 represents the survey report by SOES for all the 19 districts (<strong>in</strong>clud<strong>in</strong>g Kolkata)<strong>in</strong> West Bengal. Based on the arsenic concentrations found <strong>in</strong> the 19 districts <strong>of</strong> West Bengal theseverities have been classified <strong>in</strong>to three categories: Severely affected (>300 µg/L), mildlyaffected (between 10 <strong>and</strong> 50 µg/L, <strong>and</strong> unaffected (< 10 µg/L). N<strong>in</strong>e districts (Malda, Murshidabad,Nadia, North 24-Parganas, South 24-Parganas, Bardhaman, Howrah, Hooghly <strong>and</strong> Kolkata),where more than 300 µg/L arsenic concentrations was found <strong>in</strong> tube-wells are categorized asseverely affected. Out <strong>of</strong> 135,555 samples analyzed from these n<strong>in</strong>e districts 67,306 (49.7%)had arsenic concentrations above 10µg/L <strong>and</strong> 33,470 (24.7%) above 50 µg/L.It can be noted from Figure 2.5 that all 9 severely affected districts (concentration > 50 µg/L)are <strong>in</strong> a l<strong>in</strong>ear track along the river Bhagirathi ( the stretches <strong>of</strong> the river Ganga passed throughKolkata). Most <strong>of</strong> the affected areas lie along the left h<strong>and</strong> side <strong>of</strong> the river along the direction <strong>of</strong>groundwater flow. The groundwater flow direction <strong>in</strong> those areas is towards south-eastdirection, <strong>and</strong> the affected areas also swell mostly along the same direction. The geologicalNIH & CGWB 19

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