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Evaluation of the seasonal variation on the geochemical parameters and quality assessment of the groundwater in the proximity of River Cooum, Chennai, India

机译:印度金奈库姆河附近地区地球化学参数的季节性变化评估和地下水质量评估

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The seasonal variations of the chemical budget of ions were determined from the hydrochemical investigation of the groundwater. Though the effect of monsoon does not change the order of abundance of cations, but it does change the concentration of various ions and it is found that there was a considerable change in the case of all major ions. The unique characteristic of the ground water is the linear relationship among the principal ions. Hydrochemical characteristics of ions in the groundwater were studied using 1:1 equiline diagrams. The nature of the water samples were determined using the piper diagram. The correlation studies and R-mode factor analysis were carried out on the various groundwater parameters. The study of factor scores reveals the extent of influence of each factors on the overall water chemistry at each sampling stations. The trace metal concentration in the water was determined. The quality of the groundwater in the study area has been assessed using Percent sodium, SAR and Wilcox diagrams. The groundwater results of the premonsoon shows the dominance of excessive evaporation, silicate weathering and anthropogenic activities whereas in postmonsoon, dilution predominates over that of other factors.
机译:离子化学收支的季节性变化是根据地下水的水化学调查确定的。尽管季风效应并没有改变阳离子丰度的顺序,但是它确实改变了各种离子的浓度,并且发现所有主要离子的情况都发生了相当大的变化。地下水的独特特征是主离子之间的线性关系。使用1:1等值线图研究了地下水中离子的水化学特征。使用吹笛者图确定水样品的性质。对各种地下水参数进行了相关研究和R-模式因子分析。因子得分的研究揭示了每个采样站上每个因子对整体水化学的影响程度。测定水中的痕量金属浓度。研究区域的地下水质量已使用钠百分比,SAR和Wilcox图进行了评估。前季风的地下水结果显示出过度蒸发,硅酸盐风化和人为活动的优势,而在季后风中,稀释度高于其他因素。

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