利用水质指数和多元统计分析印度北方邦地下水可饮用性和灌溉潜力的特征

Supriya Chaudhary, G. Singh, Deepak Gupta, Suruchi Singh Maunas, V. Mishra
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引用次数: 0

摘要

本研究包括来自印度北方邦 69 个县 290 个监测点的地下水质量数据。数据分析显示,分别有 1.3%、75.52%、47.93% 和 31.03% 的地下水样本的电导率 (EC)、总硬度 (TH)、Mg2+ 和 HCO3- 浓度高于最高允许限值。对这 290 个监测点的地下水质量指数(GWQI)进行了计算,结果显示,21 个监测点(7.24%)的地下水质量指数不适合作为饮用水,18 个监测点(7.24%)的地下水质量指数不适合作为灌溉用水。大多数采样点(98.97%)的地下水导电率含量较高,平均值为 999.33 μS/cm。95.52% 的样本氟含量在允许范围内,4.48% 的样本氟含量较高。采用分层聚类分析法将所有地点分为两组:一组污染严重,另一组污染较轻。在相关矩阵中,理化指标和灌溉指标之间存在显著的相关性。在第一个主成分中,EC、TH、Ca2+、Mg2+、Na+、Cl- 和 SO42- 的载荷较高,这被认为是人为来源的污染控制过程。根据 Chadha 图,CaHCO3 和 Ca-Mg-HCl 是水中最常见的两种化学物质。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characterization of groundwater potability and irrigation potential in Uttar Pradesh, India using water quality index and multivariate statistics
This study includes groundwater quality data from 290 monitoring sites from 69 districts of Uttar Pradesh, India. The analysis of the data showed that 1.3, 75.52, 47.93, and 31.03% of groundwater samples had concentrations of electrical conductivity (EC), total hardness (TH), Mg2+, and HCO3−, respectively, higher than the maximum permissible limit. Groundwater quality index (GWQI) was calculated for these 290 monitoring sites which revealed that 21 sites (7.24%) had inappropriate GWQI for drinking water, and 18 sites (7.24%) had an unsuitable index for irrigation. Most of the sampling sites (98.97%) showed high EC contents in groundwater with a mean value of 999.33 μS/cm. Fluoride content was found within the permissible limits in 95.52% of the samples, while 4.48% had high concentrations. The use of hierarchical cluster analysis differentiated all the sites into two clusters: one with high pollution and the other with low pollution. Significant correlations exist between physicochemical and irrigation indicators in the correlation matrix. High loadings of EC, TH, Ca2+, Mg2+, Na+, Cl−, and SO42− were identified in the first principal component, which are thought to be pollution-controlled processes from anthropogenic sources. According to the Chadha diagram, CaHCO3 and Ca–Mg–HCl were the two most prevalent chemicals in the water.
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