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2- D Electrical Imaging And Its Application In Groundwater Exploration In Part Of Kubanni River Basin-Zaria, Nigeria

机译:尼日利亚库班尼河流域-扎里亚地区的二维电成像技术及其在地下水勘探中的应用

摘要

A modern field system, Terrameter (Signal Averaging System) SAS 4000/1000, was used to accomplish the task of exploring groundwater in Kubanni River Basin. 23 image lines were measured at different strategic locations of the study area based on the fractured map of the area and previous information obtained from the area. Four straight line profiles with a spread of 200 m per section were traversed during the course of this survey with three of them generally trending along a North-South direction while the fourth, trends approximately along the East- West direction. The four profiles have a total coverage distance of about 4.2 km. The data used for this survey was acquired by measuring a series of constant traverse along the same line but with the electrode spacing being increased with each successive traverse. Since increasing separation leads to greater depth penetration, the measured apparent resistivities was used to construct a vertical contoured section displaying the variation of resistivity both laterally and vertically over the section. Interpretation of the data acquired using this equipment revealed the suitability of the Southern part of the study area for location of boreholes, as the resistivity values of rock obtained around this zone reflects aquiferous materials. More layers of rock units around Area BZ and Tudun Sarki were revealed than what was reported by previous workers. Also observed were slight variation in depth to bed rock around area BZ and the Nigerian College of Aviation Technology as compared with observations made by previous workers. However, the observation of the increasing undulating bedrock geometry with depth towards the southern part of the study area was consistent with that of the previous workers.
机译:使用现代现场系统terraometer(信号平均系统)SAS 4000/1000完成了库班尼河流域地下水的勘探任务。根据该区域的裂缝图和从该区域获得的先前信息,在研究区域的不同战略位置测量了23条图像线。在此调查过程中,遍历了四个直线剖面,每个剖面的传播距离为200 m,其中三个剖面通常沿南北方向走向,而第四个剖面大致沿东西方向走向。四个剖面的总覆盖距离约为4.2 km。通过测量沿着同一条线的一系列恒定导线来获取用于此调查的数据,但是每次连续导线都会增加电极间距。由于增加的分离导致更大的深度穿透,因此使用测得的视在电阻率来构建垂直轮廓部分,以显示该部分的横向和纵向电阻率变化。对使用该设备获得的数据的解释表明,研究区域的南部适合钻孔的位置,因为在该区域附近获得的岩石的电阻率值反映了含水物质。揭露了BZ区和Tudun Sarki周围更多的岩石单元,这比以前的工人报告的要多。与先前工作人员的观察结果相比,还观察到了BZ地区和尼日利亚航空技术学院周围基岩的深度略有变化。但是,随着研究区域南部深度的增加,起伏的基岩几何形状的增加与先前的工作人员的观察结果一致。

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