首页> 外文期刊>Pacific Journal of Science and Technology >Groundwater Prospectivity Assessment of a Field of Hand-Dug Wells in the Area Around the Murtala Muhammed Postgraduate Hall OAU, Ile-Ife, Using Geoelectric Parametric Soundings
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Groundwater Prospectivity Assessment of a Field of Hand-Dug Wells in the Area Around the Murtala Muhammed Postgraduate Hall OAU, Ile-Ife, Using Geoelectric Parametric Soundings

机译:地下水预期评估Murtala Muhammed Postgraduare Hall OAU,ILE-IFE的地区各地的手挖井领域的水挖井领域

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This paper presents the results of geoelectric parametric soundings carried out on a field of hand-dug wells within the Murtala Muhammed Postgraduate Hall in Obafemi Awolowo University (OAU), Ile-Ife, Southwest Nigeria, with a view to assessing the groundwater potential and establishing the feasibility of increasing the well depths, for enhanced groundwater yield. The Vertical Electrical Sounding (VES) utilized the Schlumberger array whose curves were interpreted quantitatively by partial curve matching and computer assisted 1D forward modeling. The VES interpretation results were used to generate 2D geoelectric sections and thematic maps of overburden thickness, aquifer resistivity and basement bedrock relief. Using multi-criteria evaluation in a GIS environment, the thematic maps were integrated to evolve the groundwater potential of the study area. The feasibility of increasing the well depths was based on the current well depths, estimates of water column in the wells and estimated aquifer thicknesses. The topsoil; laterite; clay/sandy clay weathered layer; partly weathered/fractured basement and the fresh basement bedrock constitute the underlying geologic layers. The weathered layer constitutes the main aquifer unit. The depths to the basement bedrock ranged from 4.5 - 44.3 m but are generally >19.1 m except beneath wells 1 and 2 (<7.2 m). The groundwater potential rating for the study area ranged from very low (4.1%) to low (79%) and moderate (16.9%). The well depths ranged from 7.55 to 12.63 m which for most wells barely or rarely penetrated the 6.85 - 32.8 m thick weathered layer aquifer. The study concluded that there is prospect for enhanced and sustainable groundwater yield if the well depths are increased to a minimum of 19 m.
机译:本文介绍了在奥巴福(OAU)的Murtala Muhamp博物馆(OAU),Ile-Ife,西南尼日利亚伊洛省穆罕默德霍姆(OAU)内进行了电气调节器的结果,以评估地下水潜力和建立增加井深的可行性,以增强地下水产量。垂直电气探测(VES)利用了钢板阵列,其曲线通过部分曲线匹配和计算机辅助1D前向建模定量解释。 VES解释结果用于生成2D电气切片和覆盖层厚度,含水层电阻率和基底体粘屑的主题图。在GIS环境中使用多标准评估,集成了主题地图以发展研究区域的地下水潜力。增加井深的可行性基于当前的井深,井中的水柱估计和估计的含水层厚度。表土;后卫;粘土/砂质粘土风化层;部分风化/裂缝地下室和新的地下室基岩构成了下面的地质层。风化层构成了主要的含水层单元。底座基岩的深度范围为4.5-44.3米,但通常>除孔1和2下方除外,除了> 19.1m之外(<7.2米)。研究区的地下水潜力等级从非常低(4.1%)到低(79%)和中等(16.9%)。井深度从7.55到12.63 m,这对于大多数井几乎或很少渗透到6.85 - 32.8米厚的风化层含水层。该研究得出结论,如果井深度增加至至少19米,则存在增强和可持续的地下水产量的前景。

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