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Hydrochemical Characteristics of Groundwater in Noyyil River Basin, Tamil Nadu, India

机译:印度泰米尔纳德邦诺伊伊尔河流域地下水的水化学特征

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Groundwater is the major source for domestic, agricultural and other related activities. An attempt has been made to study the hydrogeochemistry characterization of Noyyil river basin. The seasonal variation of the chemical budget of ions was determined from the hydrogeochemical investigation of the groundwater. Though, the effect of monsoon does not change the order of abundance of cations, it does change the concentration of various ions, and it is found that there was a considerable change in case of all major ions. Broadly speaking, the groundwater has a chemical composition within the permissible limits suggested for drinking water. Nitrates is higher than the acceptable limits in some samples, that is mainly due to the usage of fertilizers. Hydrogeochemistry of groundwater of Noyyil river basin, which is predominantly a hard rock terrain, has been studied to evaluate the quality of groundwater for domestic and agricultural purposes. Groundwater samples from sixty locations were collected both during January 2007 and January 2008 in and around Noyyil river basin and analysed for their major cations and anions. Physical and chemical parameters of groundwater such as EC, TDS and ionic concentrations of Na~+, K~+, Ca~(2+), Mg~(2+), Cr~-, HCO_3~-, CO_3~(2-), SO_4~(2-), NO_3~- and F~- have been determined. Based on the analytical data hydrohemical indices like Na%, SAR, RSC and PI have been calculated. The ionic concentration of TDS, Na, K, SO_4~(2-), NO_3~- and EC in the sampled locations vary spatially and temporajly and the same is attributed for severe contaminations. Salinity, SAR, Na% indicate that the majority of the samples are not suitable for domestic and irrigational purposes and far from drinking water standards as prescribed by WHO.
机译:地下水是家庭,农业和其他相关活动的主要来源。已经尝试研究诺伊伊尔流域的水文地球化学特征。离子的化学收支的季节性变化是根据地下水的水文地球化学调查确定的。尽管季风效应并没有改变阳离子丰度的顺序,但确实改变了各种离子的浓度,并且发现在所有主要离子的情况下都发生了相当大的变化。广义上讲,地下水的化学成分在建议的饮用水允许极限内。硝酸盐含量高于某些样品的可接受限度,这主要是由于使用了肥料。努伊伊尔河流域(主要是坚硬的岩石地带)的地下水水文地球化学已得到研究,以评价用于家庭和农业目的的地下水质量。从2007年1月至2008年1月在Noyyil流域及其周围地区收集了来自60个地点的地下水样品,并分析了其中的主要阳离子和阴离子。地下水的理化参数,如EC,TDS和Na〜+,K〜+,Ca〜(2 +),Mg〜(2 +),Cr〜-,HCO_3〜-,CO_3〜(2- ),SO_4〜(2-),NO_3〜-和F〜-已经确定。基于分析数据,已经计算出了诸如Na%,SAR,RSC和PI的水溶指数。采样位置中TDS,Na,K,SO_4〜(2-),NO_3〜-和EC的离子浓度在空间和时间上会发生变化,这也归因于严重的污染。盐度,SAR,Na%表示大多数样品不适合用于家庭和灌溉目的,并且与WHO规定的饮用水标准相去甚远。

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