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首页> 外文期刊>Current Journal of Applied Science and Technology >Hydrogeophysical Delineation andHydrogeochemical Characterization of theAquifer Systems in Umuahia-South Area,Southern Nigeria
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Hydrogeophysical Delineation andHydrogeochemical Characterization of theAquifer Systems in Umuahia-South Area,Southern Nigeria

机译:尼日利亚南部Umuahia-South地区含水层系统的水文地球物理描述和水文地球化学特征

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In Umuahia-South Local Government Area of Abia State Nigeria, some cases of boreholes failure and groundwater discolouration have been observed. An investigation in order to determine the hydrogeological conditions of the area was carried out using geoelectrical, drill-hole and hydrogeochemical data. Using the Schlumberger electrode configuration, ten vertical electrical sounding data were acquired and the computer-aided Resist software method was used for further processing and interpretation. The interpretation of the VES data obtained from the study area shows that the vicinity of VES station 1 is likely to record failure in bore-hole exploration. A high variation in aquifer thicknesses is observed with the least as 27m at VES Station 5, and the highest 226m at VES Station 3. A new approach was used in the estimation of aquifer hydraulic parameters such as hydraulic conductivity and transmissivity. Some geoelectric sections generated from VES stations were compared with some lithologs which gave a good geological description of the study area; thereby revealing a multi-aquifer hydrogeologic system. Water samples were taken from ten boreholes for hydrogeochemical investigation which reveals the occurrence of same geochemical process; but slightly varying water quality which is associated to the multi-aquifer status of the area. The discolouration of water observed in some boreholes owes its origin from the silty-sand aquiferous units with slightly high iron content. A further analysis of the samples when plotted on Gibb’s Diagram reveals that recharge occurs through precipitation, but the local geology of the area is the source of major ion concentrations in the samples.
机译:在尼日利亚阿比亚州的Umuahia-South Local Government Area,已经观察到一些井眼破裂和地下水变色的案例。为了确定该地区的水文地质条件,使用了地电,钻孔和水文地球化学数据进行了调查。使用斯伦贝谢电极配置,获取了十个垂直电测深数据,并使用计算机辅助的Resist软件方法进行了进一步的处理和解释。从研究区域获得的VES数据的解释表明,VES站1附近很可能会记录钻孔勘探中的失败情况。观测到的含水层厚度变化很大,在VES站5最小为27m,在VES站3最高为226m。一种新方法被用于估算含水层水力参数,例如水力传导率和透射率。比较了从VES站产生的一些地电断面和一些岩石学,这些岩石学对研究区域具有良好的地质描述。从而揭示了多含水层水文地质系统。从十个钻孔中抽取水样进行水文地球化学研究,揭示了相同地球化学过程的发生。但水质略有变化,这与该地区的多含水层状态有关。在某些井眼中观察到的水变色归因于铁含量略高的粉砂砂含水单元。根据吉布图绘制的样品的进一步分析显示,补给是通过降水发生的,但是该地区的局部地质是样品中主要离子浓度的来源。

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