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Hydrogeochemical processes and impact of tanning industries on groundwater quality in Ambur, Vellore district, Tamil Nadu, India

机译:印度泰米尔纳德邦韦洛尔区安布尔的水文地球化学过程及其制革业对地下水质量的影响

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The present study was carried out to determine the hydrogeochemical processes and the impact of tanning industries on groundwater in Ambur, Vellore district, Tamil Nadu, India. Thirty groundwater samples were collected during pre monsoon (July 2015) and post monsoon (January 2016) from the open and shallow wells around this region and were analyzed for major ions and chromium. The major ion concentration follows the order of Na+ > Ca2+ > Mg2+ > K+ (cations) and Cl- > HCO3 (-) > SO4 (2-) > NO3 (-) (anions) for both seasons. The high concentrations of Na+, Cl-, and Cr around the tannery regions indicate the impact of effluent discharged from tannery units. In general, the groundwater of this study area is of Na+-Cl- type, which is due to the mixing of tannery effluent and cation exchange process. Ionic ratio indicates that the silicate weathering influences the groundwater chemistry. The permissible limit of chromium in the groundwater exceeds in over 50 % of the sampling wells. The factor analysis reveals that the dominant source for ionic contents is due to tannery effluents and cation exchange processes. To overcome this situation, it is essential to improve the performance of the effluent treatment plants so as to remove the salinity of wastewater and to plan for rainfall recharge structures for improving the groundwater recharge.
机译:本研究旨在确定印度泰米尔纳德邦韦洛尔区安布尔的水文地球化学过程以及制革业对地下水的影响。在季风爆发前(2015年7月)和季风爆发后(2016年1月)从该地区周围的浅井和浅井中采集了30个地下水样品,并对其中的主要离子和铬进行了分析。在两个季节中,主要离子浓度均按Na +> Ca2 +> Mg2 +> K +(阳离子)和Cl-> HCO3(-)> SO4(2-)> NO3(-)(阴离子)的顺序排列。制革厂区域周围高浓度的Na +,Cl-和Cr指示从制革厂排放的废水的影响。通常,该研究区的地下水为Na + -Cl-型,这是由于制革厂废水和阳离子交换过程的混合所致。离子比表明硅酸盐的风化影响地下水的化学性质。地下水中铬的允许极限超过采样井的50%以上。因子分析表明,离子含量的主要来源是制革厂废水和阳离子交换过程。为了克服这种情况,必须提高污水处理厂的性能,以去除废水中的盐分,并规划降雨补给结构以改善地下水补给。

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