加纳Ho市达梅扬组和多哥系地球化学过程地下水水质数据的主成分分析

I. Hodgson, S. Obiri, S. Cobbina, G. Quarcoo, AA Duah
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引用次数: 9

摘要

从何市36个钻孔中提取的地下水理化质量数据表明,11个水源的pH值超出了世卫组织的指导范围,而5个水源的浊度高于世卫组织的指导限值。钠含量为1.80 ~ 544 mg/L,平均值为111±132 mg/L;氯含量为2.98 ~ 898 mg/L,平均为124±183 mg/L,正阴离子优势度依次为Na+ > mg 2+ > Ca 2+ > K +和hco3 - > Cl - > so4.2 -。对质量数据进行主成分分析,提取PC1和PC2两个成分。PC1代表了近88.17%的方差,具有较高的电导率、钙、碱度和氯化物的绝对负荷,表明达梅岩组和多哥系列矿物与该地区地下水相互作用。PC2占总方差的6.62%,显示出高负荷的颜色,浊度,hco3和总铁。发生的主要地球化学过程可能是碳酸盐和白云岩的存在和溶解、蒸发的矿物以及含水层中涉及反向离子交换的化学反应
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Principal component analysis of groundwater quality data underlying Geochemical processes of Dahomeyan formation and Togo series in the Ho Municipality (Ghana)
The physico-chemical quality data of groundwater extracted from 36 boreholes in Ho Municipality indicated that 11 sources recorded pH values outside WHO guideline range, while 5 recorded turbidity levels above WHO guideline limits. Sodium levels ranged from 1.80 to 544 mg/L with a mean of 111 ± 132 mg/l; chloride level ranged from 2.98 to 898 mg/L with a mean of 124 ± 183 mg/L, and cation and anion dominance was in the ord-er Na+ > Mg 2+ > Ca 2+ > K + and HCO 3 - > Cl - > SO 4 2- respectively. The quality data was subjected to Principal Component Analysis, and two components (PC1 and PC2) were extracted. The PC1 represented nearly 88.17 % of the variance and had high absolute loadings for electrical conductivity, calcium, alkalinity and chloride, indi-cating interactions of minerals from the Dahomeyan formation and Togo series with the groundwater in the area. The PC2 accounted for 6.62 % of total variance, showing high loadings for colour, turbidity, HCO 3 and total iron. The major geochemical processes taking place might be the presence and dissolution of carbonates and dolomites, evaporated minerals and chemical reactions involving reverse ion-exchange in the aquifer
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