首页> 外文期刊>Journal of applied science & environmental management: JASEM >Hydro geophysical Investigation for Groundwater Development at Gbongudu Area, Akobo Ojurin, Ibadan, Southwestern Nigeria
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Hydro geophysical Investigation for Groundwater Development at Gbongudu Area, Akobo Ojurin, Ibadan, Southwestern Nigeria

机译:尼日利亚西南部伊巴丹Akobo Ojurin Gbongudu地区地下水开发的水文地球物理调查

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This paper presents the geophysical investigation for groundwater at Gbongudu area, Akobo Ojurin, Ibadan, Southwestern Nigeria. The area is underlain by the crystalline basement complex rocks and accessibility to potable water especially in the dry period of the year has been a major challenge. The Vertical Electrical Sounding using the Schlumberger configuration was employed. Twelve (12) vertical electrical sounding points were established in order to delineate the geo-electric layers in the area as well as evaluate the groundwater potential. The results are presented as profiles, geologic sections, curves, and maps. The VES results revealed a maximum of five geo-electric layers, viz: topsoil/lateritic sand, shale/clay, weathered layer, fractured basement and fresh basement respectively. Geo-electric sounding results were critically analyzed and interpreted. The yields of wells dug in most of these locations may be insufficient, even for domestic use because of its relatively small thicknesses. However, at a depth of 9.1 m a fracture zone occurs in VES 6 with resistivity value of 17.8 Ωm suggesting the presence of groundwater. Groundwater potential in this area is low on the average with VES 6 and VES 7 considered to be the main aquifer units suitable for groundwater exploration.
机译:本文介绍了尼日利亚西南部伊巴丹Akobo Ojurin,Gbongudu地区地下水的地球物理研究。该地区被晶体基底复合岩石所覆盖,尤其是在一年的干燥时期,饮用水的可及性一直是一个主要挑战。采用了使用斯伦贝谢配置的垂直电测深仪。建立了十二个(12)垂直电探测点,以描绘该区域的地电层并评估地下水位。结果显示为剖面,地质剖面,曲线和地图。 VES结果显示最多五个地电层,分别是:表土/红土砂,页岩/粘土,风化层,断裂的地下室和新鲜的地下室。对地电探测结果进行了严格的分析和解释。由于厚度相对较小,在这些位置的大部分中挖出的井的产量可能不足,即使是家庭使用。然而,在9.1 m的深度处,VES 6中出现了一个断裂带,电阻率值为17.8Ωm,表明存在地下水。该地区的地下水潜力平均较低,而VES 6和VES 7被认为是适合于地下水勘探的主要含水层单元。

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