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Hydrochemical and statistical evaluation of groundwater quality in coastal aquifers in Tamil Nadu, India

机译:印度泰米尔纳德邦沿海含水层地下水水质的水化学和统计评估

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摘要

Groundwater samples were collected from 36 wells during summer and monsoon seasons in a coastal region in Tamil Nadu, India in 2011. The chemical analysis of groundwater samples indicated that groundwater in the region was fresh to saline with cationic concentrations in the order Na+ Ca2+ Mg2+ K+ and anionic concentrations in the order Cl- HCO3- SO42- NO3-. Most of the groundwater samples had a chemical composition dominated by sodium and chloride ions. Scatter plots suggested that the principal processes influencing groundwater quality in the area are likely to be: ion exchange; reverse ion exchange; silicate weathering and evaporation. A Gibbs plot indicated that evaporation was the dominant process influencing groundwater salinity in the summer season, whereas both water-rock interactions and evaporation influenced the chemical composition and salinity of groundwater in the monsoon season. A principal component analysis of the data shows four principal components for the monsoon and three components for the summer seasons, which account for 85% and 87% of the total variance, respectively. The assessment has indicated that there is widespread seawater intrusion in coastal aquifers, which has led to changes in hydrochemical processes in the study area.
机译:2011年,印度泰米尔纳德邦沿海地区的夏季和季风季节期间,从36口井中采集了地下水样品。对地下水样品进行的化学分析表明,该地区的地下水新鲜到含盐浓度为Na +> Ca2 +>的盐水。 Mg2 +> K +和阴离子浓度按Cl-> HCO3-> SO42-> NO3-的顺序排列。大多数地下水样品的化学成分以钠和氯离子为主。散点图表明,影响该地区地下水质量的主要过程可能是:离子交换;反向离子交换硅酸盐风化和蒸发。吉布斯图表明,蒸发是影响夏季地下水盐度的主要过程,而水-岩相互作用和蒸发都影响季风季节地下水的化学组成和盐度。数据的主成分分析显示,季风有四个主要成分,夏季有三个成分,分别占总方差的85%和87%。评估表明,沿海含水层中海水大量入侵,这导致了研究区水化学过程的变化。

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