Hydrochemistry and Groundwater Quality in a Quaternary Phreatic Qquifer in Yenagoa, Southern Nigeria

E. Akpofure, K. Okiongbo, Arobo R. C. Amakiri
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Abstract

: Hydrochemical investigation of groundwater samples was carried out in Yenagoa, Southern Nigeria in an attempt to determine the suitability of the groundwater quality for domestic use. Twenty four groundwater samples were collected from domestic boreholes in the study area and were analyzed for major ions. The hydrochemical parameters determined were statistically examined and correlated. Factor analysis was applied to extract the principal factors responsible for the variation in the hydrochemistry. Water Quality Index (WQI) rating was calculated to quantify overall suitability of the water for human consumption. The results show that the correlation coefficient matrix between Electrical Conductivity (EC), Na + and Cl - was significant, which is an indication of seawater influence on the groundwater quality. The geochemistry of the groundwater is controlled mainly by rock-water interaction, ion exchange reactions, reductive dissolution of iron bearing minerals and weathering of silicate group of minerals. The WQI of the study area ranged from 5.7-32.7, indicating excellent water quality.
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尼日利亚南部叶纳戈阿第四纪潜水含水层的水化学和地下水质量
:在尼日利亚南部的叶纳戈阿对地下水样本进行了水化学调查,试图确定地下水质量是否适合家庭使用。从研究区国内钻孔中采集了24份地下水样品,进行了主要离子分析。测定的水化学参数进行了统计检验和相关分析。采用因子分析方法提取了导致水化学变化的主要因素。计算水质指数(WQI)评级,以量化水对人类消费的总体适宜性。结果表明,电导率(EC)与Na +和Cl -之间的相关系数矩阵显著,表明海水对地下水水质的影响。地下水的地球化学主要受岩水相互作用、离子交换反应、含铁矿物的还原性溶解和硅酸盐类矿物的风化作用控制。研究区的WQI为5.7-32.7,水质优良。
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