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Influence of anthropogenic contamination on fluoride concentration in groundwater: A study of Mulbagal town, Kolar district, Karnataka

机译:人为污染对地下水中氟化物浓度的影响:卡纳塔克邦科拉尔地区穆尔巴加尔镇的研究

摘要

Groundwater contamination is a serious concern in India. Major geogenic contaminants include fluoride, arsenic and iron, while common anthropogenic contaminants include nitrate, metals, organics and microbial contamination. Besides, known point and diffuse sources, groundwater c ontamination from inf iltration of pit to ilet leachate is an emerging concern. The study area of this paper is Kolar district in Karnataka that is hot spot of fluoride contamination. The absence of fluoride contamination in Mulbagal town and the alterations in groundwater chemistry from infiltration of pit toilet leachate motivated the author to examine the possible linkages between anthropogenic contamination and fluoride concentration in groundwater of Mulbagal town. Analysis of the groundwater chemistry revealed that the groundwater in Mulbagal town is under saturated with respect to calcite that suppresses the dissolution of fluorite and the fluoride concentration in the groundwater. The slightly acidic pH of the groundwater is considered responsible to facilitate calcite dissolution under saturation.
机译:在印度,地下水污染是一个严重的问题。主要的地质污染物包括氟化物,砷和铁,而常见的人为污染物包括硝酸盐,金属,有机物和微生物污染。此外,从已知的点源和扩散源来看,从坑的渗入到渗滤液的地下水污染是一个新出现的问题。本文的研究领域是卡纳塔克邦的科拉尔地区,那里是氟化物污染的热点地区。穆尔巴加尔镇没有氟化物污染以及井下厕所渗滤液渗透引起的地下水化学变化,促使作者研究了人为污染和穆巴加尔镇地下水中氟化物浓度之间的可能联系。地下水化学分析表明,穆尔巴加尔镇的地下水相对方解石而言处于饱和状态,从而抑制了萤石的溶解和地下水中氟化物的浓度。地下水的弱酸性pH被认为有助于在饱和状态下方解石溶解。

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  • 作者

    Rao Sudhakar M;

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  • 年度 2012
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