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Hydrogeochemistry of the alluvial aquifers of the central Gangetic Plain in India: Constraints on source and mobility of arsenic

机译:印度中央难民平原的冲积含水层的水力代,砷源和流动性的制约因素

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Until recently, most estimates of arsenic (As) pollution have focused on the predominance of As poisoning in the groundwater of West Bengal (India) and Bangladesh (Ahmed et al., 2004), which has been thought to be limited to the Ganges Delta (the lower Ganges Plain). Several authors suggested that the reductive dissolution of Fe (Ⅲ)-oxyhydroxides in strongly reducing conditions of the young alluvial sediments is the cause for As mobilization (Bhattacharya et al., 1997; Ahmed et al., 2004; McArthur et al., 2001; Nickson et al., 1998; von Bromssen et al., 2007). Holocene alluvial aquifers of Ballia, Ghazipur and Bhagalpur district in the middle Gangetic Plain have high concentrations of geogenic As.
机译:直到最近,砷(AS)污染的大多数估计都侧重于西孟加拉邦(印度)和孟加拉国地下水中的中毒(Ahmed等,2004)的职称,这被认为是仅限于Ganges Delta (较低的圆形平原)。若干作者表明,Fe(Ⅲ) - 氧基羟基氧化物在幼苗沉积物的强大条件下的还原溶解是动员的原因(Bhattacharya等,1997; Ahmed等,2004; Mcarthur等,2001 ; Nickson等,1998; von Bromssen等,2007)。中东秃牛,Galia,Ghazipur和Bhagalpur区的全新世海拔含水层具有高浓度的造环。

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