首页> 外文期刊>International Journal of Advanced Geosciences >The geological setting of arsenic enrichment in groundwater of the shallow aquifers of the Tista Floodplain, Rangpur, Bangladesh
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The geological setting of arsenic enrichment in groundwater of the shallow aquifers of the Tista Floodplain, Rangpur, Bangladesh

机译:孟加拉国TANTA洪水勘察浅含水层地下水中砷富集的地质环境

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Arsenic is present in water samples within the studied active floodplain areas of the Tista river, Rangpur Division, Bangladesh. All the water samples contain less arsenic than the WHO prescribed limit of 10 μg/L. 93.33% groundwater samples have higher Mn content than the permissible limit of 0.01 mg/L of WHO. The heavy metal concentrations of water can be expressed as FeMnZnAs on the basis of their mean content. The heavy metals are negatively correlated with the well depth which is indicative of the influence of the anthropogenic activities on the concentrations of heavy metals. The arsenic concentration in water samples is higher in the central part of the study area. The coarser grain size, dominance of physical weathering, elevated topography and the effective flushing of groundwater resulted low concentration of arsenic in the groundwater. The EDS study reveals that arsenic occurs as coating materials of the silicate minerals. The river waters also have arsenic content lower than WHOs permissible limit. The factor analysis reveals that the iron and arsenic is released by the chemical weathering of arsenic bearing minerals like pyrite and arsenopyrite. The Fe and Mn derived in the groundwater by the chemical weathering of iron and manganese bearing minerals such as iron rich clay, silicate minerals and iron sulfides.
机译:砷在孟加拉国张河师傅研究的活性洪泛区的水样中存在砷。所有的水样品含有少于10μg/升的砷的砷。 93.33%的地下水样品具有较高的Mn含量,比允许的限制为0.01mg / L.重金属浓度的水可以表示为Fe> Mn> Zn>,基于其平均含量。重金属与孔深度呈负相关,这表明人类学活性对重金属浓度的影响。水样中的砷浓度在研究区的中央部分较高。较粗糙的粒度,物理风化,地形高度的优势和地下水的有效冲洗导致地下水中砷浓度低。 EDS的研究表明,砷发生作为硅酸盐矿物的涂料。河水也有比允许极限低的砷含量低。因子分析表明,铁和砷被砷含有矿物质的化学风化释放,如黄铁矿和砷吡啶。通过铁和锰轴承矿物如铁富含粘土,硅酸盐矿物和硫化铁等铁和硅酸盐的Fe和Mn来源于地下水。

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