Physicochemical and Bacteriological Analysis of Groundwater Quality of Kathmandu Valley

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引用次数: 3

Abstract

The limited availability, accessibility and deterioration of the water quality in Kathmandu valley have led to the high demand of ground water. This study aims to evaluate ground water quality of the Kathmandu valley. In this study, the physio-chemical parameters of water samples were performed using standard procedures. Also, total coliforms were enumerated using standard membrane filtration technique to quantify the bacterial contamination. Water samples were collected from July 2017 to July 2018. The results revealed that 56% and 73% of well and boring water samples, respectively exceeded standard value of iron recommended by National Drinking Water Quality Standards, 2005. Likewise, ammonia content was higher in 41% of well water and 35% of boring water samples than standard. However, few numbers of water samples were contaminated with arsenic (0.27% and 2.6% of well and boring water samples, respectively) and nitrate (3% and 8% of well and boring water samples, respectively). Besides, 96% of well water samples and 88% of boring water samples were contaminated with total coliform bacteria. Our data indicated that groundwater quality of Kathmandu valley was poor, which was not suitable for direct drinking purposes. Therefore, regular monitoring and treatment of groundwater is recommended before using accordingly.
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加德满都谷地地下水水质理化和细菌学分析
加德满都河谷的可用性、可及性有限,水质恶化,导致地下水需求量大。本研究旨在评价加德满都谷地的地下水水质。在本研究中,采用标准程序对水样的理化参数进行了测定。此外,使用标准膜过滤技术对总大肠菌群进行计数,以量化细菌污染。2017年7月至2018年7月采集了水样。结果表明,水井和钻孔水样中,分别有56%和73%的样品超过了《国家饮用水质量标准》2005年推荐的铁标准值。同样,41%的井水和35%的钻孔水样中的氨含量高于标准。然而,很少有水样被砷(分别占井水和钻孔水样的0.27%和2.6%)和硝酸盐(分别占水井和钻孔水样品的3%和8%)污染。此外,96%的井水和88%的钻孔水样被总大肠菌群污染。我们的数据表明,加德满都山谷的地下水质量很差,不适合直接饮用。因此,建议在使用前对地下水进行定期监测和处理。
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