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Controlling factors and mechanism of groundwater quality variation in semiarid region of South India: an approach of water quality index (WQI) and health risk assessment (HRA)

机译:南印度半干旱地区地下水质量变化的控制因素及机制:水质指数(WQI)和健康风险评估方法(HRA)

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The study region comprises fractured granitic, basaltic and lateritic aquifer system constituted by Precambrian rocks. Groundwater is the primary source for drinking and household needs. Its quality is a big issue in the three aquifers, which are mostly of human health concern. Many developing regions suffer from lack of safe drinking water, thereby health problems arise in many parts of the regions, and Telangana state is one of them. For this reason, 194 groundwater samples were collected and analyzed for fluoride, nitrate, chloride and other physicochemical parameters. The concentrations of fluoride (F-), nitrate (NO3-), magnesium (Mg2+), total dissolved solids and total hardness are above the acceptable limits for drinking purposes, prescribed by the World Health Organization. The higher concentrations of fluoride and nitrate in drinking water cause health hazards, and above 50% of the groundwater samples are not suitable for drinking purposes with respect to fluoride and nitrate. Weathering of rocks and dissolution of fluoride-bearing minerals can be a cause for higher fluoride concentrations, while anthropogenic sources are one of the major reasons for higher nitrate concentrations in the study area. Groundwater suitability for irrigation suggests that more than 90% of the groundwater sampling locations are suitable for irrigation. In addition, health risk assessments were evaluated by using the United States Environmental Protection Agency model, to determine the non-carcinogenic risk of fluoride and nitrate in drinking water for adults (females and males) and children. The ranges of hazard index in all sampling locations are varied from 0.133 to 8.870 for males, 0.146 to 10.293 for females and 0.419 to 29.487 for children, respectively. The health risk assessment results indicated that children were more exposed to health risk, due to the intake of high contaminated drinking water with respective of nitrate and fluoride in the study region.
机译:该研究区包括护锋岩石构成的裂缝花岗岩,玄武岩和外链含水层系统。地下水是饮酒和家庭需求的主要来源。其质量是三种含水层的一个大问题,主要是人类健康问题。许多发展中地患有缺乏安全的饮用水,从而在地区的许多地区出现了健康问题,而Telangana国家是其中之一。因此,收集194个地下水样品并分析氟化物,硝酸盐,氯化物和其他物理化学参数。氟化物(F-),硝酸盐(NO 3-),镁(Mg2 +),总溶解固体和总硬度高于世界卫生组织规定的饮用目的的可接受限制。饮用水中较高浓度的氟化物和硝酸盐会导致健康危害,并且在50%以上的地下水样品中不适合相对于氟化物和硝酸盐的饮用目的。岩石的风化和氟化物矿物质的溶解可以是氟化物浓度较高的原因,而人为源是研究区域中硝酸盐浓度较高的主要原因之一。地下水适用于灌溉建议,超过90%的地下水采样地点适用于灌溉。此外,通过使用美国环境保护局模型来评估健康风险评估,以确定成人(女性和男性)和儿童饮用水中氟化物和硝酸盐的非致癌风险。所有采样场所的危险指数的范围从雄性的0.133〜8.870各不相同,为女性0.146至10.293,儿童分别为0.419至29.487。健康风险评估结果表明,由于研究区中的硝酸盐和氟化物相应的高污染饮用水,儿童更加暴露于健康风险。

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