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首页> 外文期刊>Journal of Civil & Environmental Engineering >Assessment of Drinking and Irrigation Water Quality of Surface Water Resources of South-West Kashmir, India
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Assessment of Drinking and Irrigation Water Quality of Surface Water Resources of South-West Kashmir, India

机译:印度西南克什米尔地表水饮用水和灌溉水质量评估

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Surface water samples have been collected from various streams of SW Kashmir and analyzed for major ions and trace elements to determine the mechanisms controlling the surface water chemistry and suitability of water for drinking, domestic and irrigation purposes. The order of cations is Ca > Mg > Na > K and anions is HCO3 > Cl > SO4 > NO3. As per the Gibb’s diagram, the major ion chemistry of surface water is controlled by rock-water interaction. The evolution of surface water into Ca-Mg-HCO3 water type of Piper trilinear plot is due to easy dissolution of carbonate minerals and less time for water-rock interaction. Surface water samples are characterized by one main trend of Ca-Mg-HCO3 i.e., carbonate dissolution of Langelier-Ludwig diagram. The major ions and trace elements in the water samples are well below the standards prescribed by WHO and BIS for drinking purposes. Based on EC and TDS classification, the water is fresh, good for irrigation and desirable for drinking purposes. The water samples fall between soft to hard categories of hardness classification with 16.66% belonging to soft, 50% to moderately hard and 33.33% to hard categories. The suitability of water for irrigation was evaluated based on the quality parameters and plots of water like Magnesium Content, Sodium Percent, Wilcox diagram, US Salinity hazard plot and Doneen’s plot. According to the values of these parameters the surface water of the study area was found suitable for irrigation and the water can be used for irrigating most of the crops and majority of the soils.
机译:已从西南克什米尔的各种溪流中收集了地表水样品,并对其中的主要离子和微量元素进行了分析,以确定控制地表水化学性质以及饮用水对饮用水,家庭用水和灌溉用水的适应性的机制。阳离子的顺序为Ca> Mg> Na> K,阴离子的顺序为HCO3> Cl> SO4> NO3。根据吉布(Gibb)的图表,地表水的主要离子化学性质受岩水相互作用的控制。 Piper三线性图的地表水向Ca-Mg-HCO3水类型的演化归因于碳酸盐矿物的易溶性和较少的水-岩相互作用时间。地表水样品的特征是Ca-Mg-HCO3的一个主要趋势,即Langelier-Ludwig图的碳酸盐溶解。水样中的主要离子和微量元素远低于WHO和BIS规定的饮用标准。根据EC和TDS分类,水是新鲜的,适于灌溉并且适合饮用。水样本介于硬度类别的软至硬类别之间,其中软类别为16.66%,中硬为50%,硬类别为33.33%。根据水的质量参数和水图(如镁含量,钠百分比,Wilcox图,美国盐度危害图和Doneen图)评估了灌溉用水的适宜性。根据这些参数的值,发现研究区域的地表水适合灌溉,并且该水可用于灌溉大部分农作物和大部分土壤。

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