Statistical Evaluation and Hydrogeochemistry of Groundwater from Western Part of Chandrapur District, Maharashtra with Special Emphasis on Human Health Risk Assessment

M.P. Jaunjalkar, Y.A. Murkute
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Abstract

The groundwater samples were collected from the phreatic aquifers of PG2 watershed of western part Chandrapur district, Maharashtra. The geogenic processes like dissolution of calcium rich minerals are responsible for increase of Ca2+ content in groundwater. In the groundwater samples, HCO - and SO 2- are the prevailing dominant anions. The TDS, TH, Ca2+, Mg2+, Na+, HCO - as well as Cl- ions present in basement rocks have been attributed to the geogenic factor through the factor analysis. K+, SO 2- as well as NO - correspond to fertilizers and soil amendments used by people to enhance crop production, which is regarded as anthropogenic input. The silicate weathering at water-rock interface is the main process of generation of various solutes in groundwater. The multiple regression analysis expresses the TDS as a linear function of the ions and Ca2+, Mg2+, Na+, HCO -, Cl-, SO 2- and NO - contribute significantly to the bulk chemical composition of the groundwater from the study area. The health hazard quotient (HQ) for children (4.94%) and adults (7.95%) denotes the intensity of different health risk vulnerable zones at a specific site. Keywords: Rock-Water Interaction, Silicate Weathering, Statistical Evaluation, Health Risk Assessment, Chandrapur District, Maharashtra
马哈拉施特拉邦钱德拉普尔西部地区地下水水文地球化学统计评价与人类健康风险评价
地下水样本采集自马哈拉施特拉邦Chandrapur地区西部PG2流域的潜水含水层。富钙矿物溶解等地质作用是导致地下水Ca2+含量增加的主要原因。在地下水样品中,HCO -和so2 -是主要的阴离子。通过因子分析,认为基岩中存在的TDS、TH、Ca2+、Mg2+、Na+、HCO -、Cl-等离子均与地质因素有关。K+、so2 -和NO -与人类为提高作物产量而使用的肥料和土壤改良剂相对应,被认为是人为投入。水岩界面的硅酸盐风化作用是地下水中各种溶质生成的主要过程。多元回归分析表明,TDS是离子的线性函数,Ca2+、Mg2+、Na+、HCO -、Cl-、so2 -和NO -对研究区地下水的总体化学成分有显著影响。儿童(4.94%)和成人(7.95%)的健康危害系数(HQ)反映了某一地点不同健康风险脆弱区的强度。关键词:岩水相互作用,硅酸盐风化,统计评价,健康风险评价,Chandrapur地区,马哈拉施特拉邦
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