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Principal Component Analysis: Deeper Aquifer Groundwater Quality of Bhaskar Rao Kunta Watershed, Nalgonda District, Andhra Pradesh, India

机译:主成分分析:印度安得拉邦纳尔贡达区Bhaskar Rao Kunta流域的深层含水层地下水质量

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Principal component analysis (PCA) is an appropriate tool for water quality evaluation and management. Inthe study area, PCA was used for multivariate factor analysis of hydrogeochemical variables of pH, EC,Ca 2+ , Mg 2+ , Na + , K + , HCO 3 - , SO 4 2- , Cl - , NO 3 - , F - , TH and TDS. Influence on chemical composition ofgroundwater quality and statistically characterize (Eigen value ≥ 1 and % of variance) two factors wereextracted as well as identified, principal component-I and II. The principal component-I accounts for 36.62and 39.80% of variance and principal component-II accounts for 17.84 and 18.10% of variance in pre andpost-monsoon seasons respectively. Graphical presentation of the principal component-I and II showedloading relationship between the variables EC, TDS and Ca 2+ as high positive relation; and variables betweenTH, Mg 2+ , NO 3 - and F - as low positive relation in pre-monsoon season. Principal component-I and II showedloading relationship variables between pH, as high positive relation; and variables between HCO 3 - and SO 4 2-as high positive relation in post monsoon seasons respectively. These two principal components results werepredicted for hydrochemical process of rock water interaction, process of degradation products of the ions,process of alkalinity and process of anthropogenesis activity. It was concluded that hydrochemical processis controlled by geogenic and non-geogenic factors.
机译:主成分分析(PCA)是用于水质评估和管理的适当工具。在研究区域中,PCA用于pH,EC,Ca 2+,Mg 2+,Na +,K +,HCO 3-,SO 4 2-,Cl-,NO 3-,F的水文地球化学变量的多因素分析。 -,TH和TDS。提取并确定了对地下水质量化学成分的影响并进行统计表征(特征值≥1和方差%),并确定了两个因素,主要成分I和II。季风前后,主成分I分别占变化的36.62%和39.80%,主成分II分别占季风前后的17.84和18.10%。主成分I和II的图形表示表明,变量EC,TDS和Ca 2+之间的负载关系为正相关;在季风前季节,TH,Mg 2+,NO 3-和F-之间的变量呈低正相关。主成分I和II显示出pH之间的负荷关系变量,为高正相关。季风后季节,HCO 3-和SO 4 2-之间的变量呈高度正相关。预测了这两个主要成分的结果,包括岩石水相互作用的水化学过程,离子的降解产物过程,碱度过程和人为活动过程。结论是,水化学过程受地缘和非地缘因素控制。

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