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Groundwater Exploration Using Vertical Electrical Sounding Technique in Parts of Gindiri, North-Central Nigeria

机译:使用垂直电测深技术在尼日利亚中北部部分地区进行地下水勘探

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This research involved the use of electrical resistivity technique which is considered most appropriate for subsurface investigation of structures and/or lithologies associated with the occurrence of groundwater; to investigate the geo-electric characteristics of the subsurface formations that underlie the study area. The aim was to provide a data base for sustainable groundwater development in the study area. The geophysical investigation involved the acquisition of twenty two (22) vertical electrical sounding (VES) data via the ABEM terrameter SAS 300C model using the Schlumberger configuration. These were quantitatively and qualitatively analysed using partial curve matching and computer iteration to obtain subsurface information in the study area. The results obtained from the interpretation of the VES data show earth models with geo electric layers ranging from three (3) to four (4). The representative type curves are H, A, HA, QH, HK and KH types. The subsurface is made up of four layers, namely the topsoil, the weathered layer, the partially weathered/fractured bedrock and the fresh bedrock, with the weathered layer and the partially weathered/fractured bedrock layers constituting the aquifer units of generally low, medium and high groundwater yielding capacities.
机译:这项研究涉及电阻率技术的使用,该技术被认为最适合用于与地下水发生有关的结构和/或岩性的地下调查。研究位于研究区域之下的地下地层的地电特征。目的是为研究区域的可持续地下水开发提供数据库。地球物理研究涉及使用Schlumberger配置通过ABEM地形仪SAS 300C模型获取二十二(22)个垂直电测深(VES)数据。使用部分曲线匹配和计算机迭代对这些进行定量和定性分析,以获得研究区域的地下信息。从VES数据的解释中获得的结果表明,地球模型的地电层范围为三(3)到四(4)。代表性的类型曲线为H,A,HA,QH,HK和KH类型。地下由四层组成,即表层土壤,风化层,部分风化/破裂的基岩和新鲜基岩,其中风化层和部分风化/破裂的基岩层构成了通常为低,中,高的含水层单元。高地下水产生能力。

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