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Geophysical Investigation of Groundwater Regime: Case Study of Etioro-Akoko Southwestern Nigeria

机译:地下水制度的地球物理研究:以尼日利亚西南部的Etioro-Akoko为例

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The electrical resistivity study of Etioro-Akoko has become imperative because of non-functional potable water. The study aims at resolving the geology setup through hydro-geophysical methods and modeling of the wells. Dipole- dipole, Schlumberger array and the positioning of the hand dug wells were carried out in the study area.Dipole-dipole array results in the study area do not show structures indicative of high groundwater yield potential. Three layers comprising of the topsoil, weathered layer, and the fresh basement were delineated using the Schlumberger array with overburden thicknesses ranging from 4.5-7.7m.The values are too thin to support productive wells. Well inventory (depth to well-base) results ranges from 5.3-7.3m and were used to model the direction of flow pattern of groundwater. The southernmost part of the map is continuously discharged. To tap into the groundwater resources in this area requires detailed geophysical mapping and investigations of the discharge area.DOI: http://dx.doi.org/10.5755/j01.erem.69.3.5334
机译:由于不能使用饮用水,因此对Etioro-Akoko进行电阻率研究变得势在必行。该研究旨在通过水文地球物理方法和油井建模来解决地质问题。在研究区内进行了偶极-偶极,斯伦贝谢阵列和手挖井的定位。研究区的偶极-偶极阵列结果没有显示出表明高地下水潜力的结构。使用Schlumberger阵列划定了由表土,风化层和新鲜地下室组成的三层,覆盖层厚度为4.5-7.7m,该值太薄而无法支撑生产井。井存量(深度至井底)的结果范围为5.3-7.3m,用于模拟地下水流向。地图的最南端持续放电。要开发该地区的地下水资源,需要详细的地球物理图和排放区域的调查。DOI:http://dx.doi.org/10.5755/j01.erem.69.3.5334

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