利用GIS和电阻率技术综合评价地下水:以塞拉利昂Bullom组沉积物为例

Yaguba Jalloh, M. Thomsa, K. Sasaki
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摘要

电阻率与地理信息系统(GIS)技术的结合已广泛应用于地下水资源管理。在这项研究中,将电阻率法垂直电测深(VES)与GIS相结合,描绘了塞拉利昂Bullom组沉积物的地电特征并评估了地下水潜力。本次评估共在场址内建立了5个垂直电测深站。采用斯伦贝谢电极配置和扩展程序进行数据采集。利用部分曲线匹配的方法对生成的VES曲线进行解释。利用测深解释结果生成地电剖面,据此圈定了含水层。该含水层揭示了四个亚表层,包括沙质表土、作为含水层的粘土砂和作为研究区域可移动水源的沙质砾石(限制含水层)。然后开发了一个GIS模型来定位合适的地下水远景区,该模型显示地下水的平均深度在10米至30米之间。研究结果表明,该井位于地震探测系统1、2、3和4层的高导电性区域,可能含有高产含水层。
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Groundwater Assessment through an Integrated Approach Using GIS and Electrical Resistivity Technique: A Case Study from the Bullom Group of Sediments in Sierra Leone
Electrical Resistivity in conjunction with Geographic Information System (GIS) techniques have been widely used in groundwater resource management. In this research, Vertical Electric Sounding (VES), an Electrical Resistivity method, was integrated with GIS to delineate geo-electric characteristics and evaluate groundwater potential of the Bullom group of sediments in Sierra Leone. For this assessment, a total of 5 vertical electrical sounding stations were established within the site. The Schlumberger electrode configuration and the expanding procedure were used for data acquisition. The VES curves generated were interpreted using partial curve matching. The depth sounding interpretation results were used to generate geo-electric sections from which the aquifer was delineated. The aquifer revealed four subsurface layers which comprises of sandy topsoil, clayey sand which acts as aquitard and sandy gravel (confine aquifer) that serves as a source of portable water in the study area. A GIS model was then developed to locate the suitable groundwater prospective zones which reveals the average depth to groundwater to be between 10 m to 30 m. This research concluded that the boreholes were sited in high conductivity zones in VES layers 1, 2, 3 and 4 as they contain probable aquifers with good yield.
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