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Evaluation of groundwater quality and its suitability for drinking purpose in Rajshahi City, Bangladesh

机译:孟加拉国拉杰沙希市地下水质量及其对饮用目的的适用性评估

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A study was conducted to evaluate the hydrochemical processes controlling the water quality variations and to determine the water type of groundwater in Rajshahi City, Bangladesh, for drinking purposes. A total of 120 shallow and deep tubewell water samples were collected in pre- and post-monsoon seasons during the year 2008-2009 and analyzed for various physico-chemical parameters. The results of the analyses show that water samples were slightly alkaline to neutral pH. The average concentrations of Pb in all samples for the post-monsoon season were above the WHO'S guideline for drinking water. For both seasons, arsenic levels exceeded the drinking water standard in 25% of groundwater samples and lead (Pb) levels exceeded in about 60% samples which contained elevated levels (>0.01mg/L). The major cationic and anionic orders of dominance were unusual, being Ca2+ > Mg2+ > Na+ > K2 > Fe3+ > Pb2+ > zn2+ > Cu2+ > As (total) > Cd2+ and HCO3~ > Cl-> SO42" > NO3~, respectively. The study reveals that the water type of the groundwater was calcium bicarbonate (Ca-HCO3). Thus overall results suggest that groundwater quality of the study area was not suitable for drinking purposes without treatment especially for Pb and As.
机译:进行了一项研究,以评估控制水质变化的水化学过程,并确定孟加拉国拉杰沙希市的地下水水类型,以供饮用。在2008-2009年的季风前后,总共收集了120个浅层和深层试管水样品,并分析了各种理化参数。分析结果表明,水样品为弱碱性至中性pH。季风后季节所有样品中的Pb平均浓度均高于WHO的饮用水准则。在两个季节中,砷含量都超过了25%的地下水样品中的饮用水标准,铅(Pb)含量超过了约60%的含量较高的样品(> 0.01mg / L)。阳离子和阴离子的主要控制顺序不寻常,分别为Ca2 +> Mg2 +> Na +> K2> Fe3 +> Pb2 +> zn2 +> Cu2 +> As(总)> Cd2 +和HCO3〜> Cl-> SO42“> NO3〜。研究表明,地下水的水类型为碳酸氢钙(Ca-HCO3),因此总体结果表明,未经处理,特别是铅和砷,该研究区的地下水质量不适合饮用。

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