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Statistical analysis of the hydrogeochemical evolution of groundwater in hard rock coastal aquifers of Thoothukudi district in Tamil Nadu, India

机译:印度泰米尔纳德邦Thoothukudi地区硬岩沿海含水层中地下水水文地球化学演化的统计分析

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The study of groundwater hydrogeochemistry of a hard rock aquifer system in Thoothukudi district has resulted in a large geochemical data set. A total of 100 water samples representing various lithologies like Hornblende Biotite Gneiss, Alluvium Marine, alluvium Fluvial, Quartzite, Charnockite, Granite and Sandstone were collected for two different seasons and analyzed for major ions like Ca~(2+), Mg~(2+, Na~+, K~+, HCO_3~-, Cl~-, SO_4~(2-), NO_3~-, PO_4~-, F~- and H_4SiO_4. Statistical analysis of the data has been attempted to unravel the hidden relationship between ions. Correlation analyses and factor analyses were applied to classify the groundwater samples and to identify the geochemical processes controlling groundwater geochemistry. Factor analysis indicates that sea water intrusion followed by leaching of secondary salts, weathering and anthropogenic impacts are the dominant factors controlling hydrogeochemistry of groundwater in the study area. Factor score overlay indicate major active hydrogeochemical regimes are spread throughout the Eastern, Northwestern and Southeastern parts of the study area. The dominant ions controlling the groundwater chemistry irrespective of season are CP, Na~+, Mg~(2+), Ca~(2+), SO_4~(2-), K~+ and NO_3~-. An attempt has also been made to note the seasonal variation of the factor representations in the study area. This study also illustrates the usefulness of statistical analysis to improve the understanding of groundwater systems and estimates of the extent of salinity/salt water intrusion.
机译:Thoothukudi地区对硬岩含水层系统的地下水水文地球化学的研究产生了大量的地球化学数据集。在两个不同的季节中,总共收集了100个代表各种岩性的水样,包括Hornblende黑云母片麻岩,冲积层海洋,冲积层河流相,石英岩,孔雀石,花岗岩和砂岩,并分析了Ca〜(2 +),Mg〜(2 +,Na〜+,K〜+,HCO_3〜-,Cl〜-,SO_4〜(2-),NO_3〜-,PO_4〜-,F〜-和H_4SiO_4。试图对数据进行统计分析以阐明利用相关分析和因子分析对地下水样品进行分类,确定控制地下水地球化学的地球化学过程;因子分析表明,海水入侵,二次盐的浸出,风化和人为影响是控制地下水的主要因素。研究区地下水的水文地球化学,因子得分覆盖表明主要的活跃水文地球化学形态分布在研究区的东部,西北和东南部。不论季节如何,控制地下水化学的元素是CP,Na〜+,Mg〜(2 +),Ca〜(2 +),SO_4〜(2-),K〜+和NO_3〜-。还尝试记录了研究区域中因子表示的季节性变化。这项研究还说明了统计分析对于增进对地下水系统的理解和盐度/咸水入侵程度估计的有用性。

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