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Hydrogeochemical characterization of a shallow groundwater system in the weathered basement aquifer of Ilesha area, southwestern Nigeria

机译:尼日利亚西南部伊莱沙地区风化的地下含水层中浅层地下水系统的水文地球化学特征

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Hydrogeochemical characterization of a weathered basement aquifer in Ilesha area, southwest Nigeria, was carried out with respect to geogenic and anthropogenic influences on the shallow groundwater system. Physico-chemical parameters revealed a pH of 6.4-8.4 and EC of 22-825 μs/cm in the urban areas compared to a pH of 7.3-10.5 and relatively higher EC of 126-1027 (is/cm in the peri-urban area. The concentrations of major cations (Ca, Na, K, Mg) in the urban areas revealed relatively lower average concentrations of 28.4, 16.7, 8.4 and 5.0 mg/L, respectively, compared to 82.5, 33.4, 19.3 and 12.4 mg/L, respectively, for the peri-urban areas. The low concentrations of major cations in the urban areas can be attributed to low mineral dissolution of quartzite and muscovite quartz-schist bedrocks compared to the weathered granitic, amphibolite and biotite schist in the peri-urban areas. Hydrochemical characterization revealed two main water types; namely Ca-Mg-(Na)-HCO_3 mostly in the urban areas suggesting CO_2-charged infiltrating recharge rainwater, and Ca-Na-(K)-SO_4-Cl type in the peri-urban areas as products of water-rock interactions.
机译:考虑到地质和人为因素对浅层地下水系统的影响,对尼日利亚西南部Ilesha地区的风化地下含水层进行了水文地球化学表征。理化参数显示,城市地区的pH值为6.4-8.4,EC为22-825μs/ cm,而pH值为7.3-10.5,相对较高的EC为126-1027(在城市周边地区为is / cm 。城市地区主要阳离子(Ca,Na,K,Mg)的浓度分别相对较低,分别为88.4、33.4、19.3和12.4 mg / L,分别为28.4、16.7、8.4和5.0 mg / L。与城市周边风化的花岗岩,角闪石和黑云母片岩相比,城市地区主要阳离子的低浓度归因于石英岩和白云母石英片岩基岩的矿物溶解度低。水化学特征揭示了两种主要水类型:Ca-Mg-(Na)-HCO_3主要在城市地区,表明有CO_2填充的渗透补给雨水; Ca-Na-(K)-SO_4-Cl类型在郊区。城市地区是水-岩相互作用的产物。

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