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Hydrochemical characterization and suitability assessment of groundwater in Baga-Calangute stretch of Goa, India

机译:印度果阿的Baga-Calangute段的地下水水化学特征和适宜性评估

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The present study is the first attempt to determine the suitability of groundwater for drinking and irrigation in the Baga-Calangute stretch of Goa. The suitability of groundwater for potable use was assessed by comparing observed values against standards prescribed by the Bureau of Indian Standards, and the quality was classified based on the Weighted Arithmetic Water Quality Index. Most of the groundwater samples (90%) were found to be suitable for drinking except for hardness, chlorides, and nitrates. The percent sodium (%Na), residual sodium carbonate, soluble sodium percentage, sodium adsorption ratio, Kelly's ratio, and Permeability Index were found to be within the prescribed limits for irrigation purposes. The major mechanism controlling groundwater chemistry, i.e., rock-water interaction, was also studied, and it was found that silicate weathering plays a major role in the dissolution of minerals. Based on the hydrochemical characterization, the water was observed to be of the Ca-Na-SO4 composition type except for one sample which was of the Na-Cl composition type. Classification of the meteoric genesis suggested that the groundwater in surficial aquifers in the region had a deep meteoric percolation, and its chemistry is regulated by rock-water interaction.
机译:本研究是确定果阿的Baga-Calangute地段地下水适合饮用和灌溉的首次尝试。通过将观测值与印度标准局规定的标准进行比较,评估了地下水对饮用水的适用性,并根据加权算术水质指数对水质进行了分类。除硬度,氯化物和硝酸盐外,大多数地下水样品(90%)都适合饮用。发现钠的百分比(%Na),残留的碳酸钠,可溶性钠的百分比,钠的吸附率,凯利比和渗透性指数在灌溉目的的规定范围内。还研究了控制地下水化学的主要机理,即岩水相互作用,并且发现硅酸盐风化作用在矿物溶解中起主要作用。基于水化学特征,观察到水为Ca-Na-SO 4组成类型,除了一个样品为Na-Cl组成类型。陨石成因的分类表明,该地区表层含水层的地下水有较深的陨石渗滤,其化学作用受岩水相互作用的调节。

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