INTEGRATED GEOPHYSICAL MAPPING OF GROUNDWATER AQUIFER FOR SPATIAL DISTRIBUTION OF GROUNDWATER DEVELOPMENT IN IPERINDO AND ITS ENVIRONS, SOUTHWESTERN NIGERIA

Kazeem O.Olomo, Oluwatoyin K. Olaleye, Temitayo, O. Ale, Michael T. Asubiojo, O. E. Faseki
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Abstract

Assessment of groundwater potential of Iperindo area, Southwestern Nigeria was conducted by mapping spatial distribution of groundwater availability within the area and consequently locating areas of groundwater reserve to serve the community and its environs. This was achieved by integrating geophysical techniques involving landsat ETM-7 satellite data, aeromagnetic data, VLF-EM and electrical resistivity methods to delineate subsurface structures, understand the direction of groundwater flow, and detect the depth to groundwater aquifer. The result of landsat and aeromagnetic revealed some lineament intersection approximately NE-SW direction and interpreted to be potential sites for groundwater development. VLF-EM revealed geologic structures of significant hydrogeological importance at depths of 40 m to 200 m. Vertical electrical sounding (VES) confirmed high groundwater prospect in the areas with estimated depth to water table between 30 m and 100 m. The integrated results of the study revealed adequate groundwater spatial distribution for effective groundwater development in the area.
尼日利亚西南部iperindo及其周边地区地下水开发空间分布的地下水含水层综合地球物理制图
对尼日利亚西南部Iperindo地区的地下水潜力进行了评估,方法是绘制该地区地下水可用性的空间分布图,从而确定为社区及其周边地区服务的地下水储备区域。这是通过整合地球物理技术实现的,包括陆地卫星ETM-7卫星数据、航空磁数据、VLF-EM和电阻率方法,以描绘地下结构,了解地下水流动方向,并探测地下水含水层深度。陆地卫星和航磁结果显示,该地区有近NE-SW方向的地貌交点,被解释为地下水开发的潜在场所。VLF-EM揭示了40 ~ 200 m深度具有重要水文地质意义的地质构造。垂直电测深(VES)证实,在水深30 ~ 100 m的区域,地下水远景较高。综合研究结果表明,该地区地下水空间分布合理,地下水开发有效。
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