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Geoelectric evaluation of groundwater potential within sunshine garden estate, akure southwestern Nigeria

机译:尼日利亚阿库雷西南部阳光花园庄园内地下水潜力的地电评估

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The Vertical Electrical Resistivity surveys in the Sunshine Garden Estate have contributed to a better understanding of the basement complex of Southwestern Nigeria. Nine (9) vertical electrical sounding (VES) using the Schlumberger electrode array were interpreted and the results shows three (3) subsurface geoelectric layers within the study area. These are the weathered layer, topsoil, fresh/fractured basement. Groundwater pockets such as fractured zones, valley fills/basement depressions, and weathered zones were delineated in the study area. Weathered/partially weathered layer and weathered basement/fractured basement were the two major aquifer mapped out and these aquifers are characterized by thick overburden, found within basement depressions. The groundwater potential of the study area was zoned into low, medium and high potentials. Zones where the overburden thickness (which constitutes the main aquifer unit) is greater than 13m and of low clay composition (average resistivity value between 200 - 400?m) are considered zones of high groundwater potential. Area where the thickness of the aquifer ranges from 11-13m with less clay composition are considered to have medium groundwater potential and the areas where the thickness of the aquifer is less than 11m are considered to have a low groundwater. The VES station underlained by high and medium groundwater potential zones are envisaged to be viable for groundwater development within the area.
机译:阳光花园村的垂直电阻率调查有助于人们更好地了解尼日利亚西南部的地下室。解释了使用Schlumberger电极阵列的九(9)个垂直电测深(VES),结果显示研究区内三(3)个地下地电层。这些是风化层,表土,新鲜/破裂的地下室。在研究区域中划定了地下水袋,如裂缝带,河谷填充物/基底凹陷和风化带。风化/部分风化层和风化的地下室/断裂的地下室是规划出的两个主要含水层,这些含水层的特征是在地下洼地中发现了厚覆盖层。研究区域的地下水潜力分为低,中和高潜力。覆盖层厚度(构成主要含水层单元)大于13m且粘土成分低(平均电阻率值在200-400?m之间)的区域被认为是具有较高地下水潜力的区域。含水层厚度在11-13m范围内且粘土成分较少的区域被认为具有中等地下水潜力,而含水层厚度小于11m的区域被认为具有低地下水潜力。设想到由高和中层地下水潜在区带支撑的VES站对于该地区的地下水开发是可行的。

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