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Identification of controlling processes of groundwater quality in a developing urban area using principal component analysis

机译:主成分分析法识别发展中城市地区地下水水质的控制过程

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Hydrogeochemistry is an important tool for the evaluation of the effect of human activities on aquifer system. Sixty eight groundwater samples were collected from bore wells during pre- and post-monsoon from Nagpur, a fast growing city in India, to assess the spatial controlling processes of groundwater contamination using principal component analysis (PCA). Groundwater has variable total dissolved solid (TDS) and total hardness (TH) values classifying them from fresh to saline and moderately hard to very hard types. About 36 and 33 % of the total groundwater samples during pre-and post-monsoon, respectively, are not suitable for drinking purpose. The graphical presentation of groundwater chemistry has indicated Ca-HCO3, mixed Ca-Na-HCO3 and mixed Ca-Mg-Cl types. The PCA summarizes the chemical variables of pH, EC, TDS, TH, TA, Na+, K+, Ca2+, Mg2+, HCO3-, Cl-, SO42- and NO3- into two PC loadings, accounting for 61.33 and 62.09 % of the total variance during pre-and post-monsoon, respectively. The first PC shows high loadings of EC, TDS, TH, Cl-, NO3-, Ca2+ and Mg2+, which considered as pollution-controlled processes of anthropogenic sources. Second PC has high loadings of Na+ and HCO3-, which is taken as alkalinity and pollution-controlled processes of geogenic and anthropogenic sources, respectively. The PC scores suggest the causes of variation in the groundwater chemistry. Negative values of chloro-alkaline indices suggest the prevalence of reverse ion exchange irrespective of the season, silicate weathering and anthropogenic activities over the controlling of groundwater quality which further PCA. Thus, the PCA helps as a tool to assess the controlling processes of the groundwater quality.
机译:水文地球化学是评估人类活动对含水层系统影响的重要工具。在季风前后,从印度快速发展的城市那格浦尔,从井眼中收集了68个地下水样品,以使用主成分分析(PCA)评估地下水污染的空间控制过程。地下水具有可变的总溶解固体(TDS)和总硬度(TH)值,可将它们从淡水分类为盐水,从中硬分类为非常硬。在季风前后,分别约有36%和33%的地下水不适合饮用。地下水化学的图形表示表明有Ca-HCO3,混合的Ca-Na-HCO3和混合的Ca-Mg-Cl类型。 PCA将pH,EC,TDS,TH,TA,Na +,K +,Ca2 +,Mg2 +,HCO3-,Cl-,SO42-和NO3-的化学变量汇总为两个PC负载量,分别占总量的61.33和62.09%季风前后的变化。第一台PC显示出高浓度的EC,TDS,TH,Cl-,NO3-,Ca2 +和Mg2 +,这被认为是人为污染源的污染控制过程。第二PC的Na +和HCO3-含量较高,分别被视为地源和人为源的碱度和污染控制过程。 PC分数表明了地下水化学变化的原因。氯碱指数的负值表明反向离子交换的流行,与季节,硅酸盐风化和人为活动有关,而不管地下水质量如何,这进一步加剧了PCA。因此,PCA有助于评估地下水质量的控制过程。

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