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首页> 外文期刊>Journal of Geography and Geology >Hydrogeochemical Signatures of Different Aquifer Layers in the Crystalline Basement of Oban Area (SE Nigeria)
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Hydrogeochemical Signatures of Different Aquifer Layers in the Crystalline Basement of Oban Area (SE Nigeria)

机译:奥本地区(尼日利亚东南部)结晶基底中不同含水层的水文地球化学特征

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The shallow and deep aquifer horizons of the crystalline basement of Oban massif of (SE Nigeria) were studied during the dry and wet seasons. The criteria were ascertaining hydrogeochemistry relative to seasonal and spatial variations across the study region. The results obtained show that major elements such as Ca, Mg, Na and K were higher in the shallow aquifers than in the deep aquifers, during the study period. The major anions Cl, SO 4 , HCO 3 and NO 3 were higher in the deep aquifers compared to the shallow ones. Two water types were identified for both (shallow and deep) aquifers: Ca/Mg-HCO 3 and Ca/Na-Cl/SO 4 . Most of the water parameters considered was within the international limits for drinking and domestic purposes. Assessment by use of Sodium Absorption Ratio (SAR), percent Sodium (% Na) and the Wilcox diagram reveal that the waters are suitable for irrigation purposes.
机译:在干旱和潮湿季节,对(东南尼日利亚)奥本断层的结晶基底的浅层和深层含水层进行了研究。标准是确定研究区域内相对于季节和空间变化的水文地球化学。获得的结果表明,在研究期间,浅层含水层中的钙,镁,钠和钾等主要元素含量高于深层含水层。深层含水层中的主要阴离子Cl,SO 4,HCO 3和NO 3高于浅层含水层。对于(浅层和深层)含水层,确定了两种水类型:Ca / Mg-HCO 3和Ca / Na-Cl / SO 4。所考虑的大多数水参数均在饮用水和家庭用水的国际限制之内。通过使用钠吸收率(SAR),钠百分比(%Na)和Wilcox图进行的评估表明,这些水适合灌溉。

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