Subsurface geological, hydrogeophysical and engineering characterisation of Etioro-Akoko, southwestern Nigeria, using electrical resistivity tomography

Adedibu Sunny Akingboye, I. Osazuwa
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引用次数: 8

Abstract

ABSTRACT Noninvasive geoelectrical subsurface characterisation provides screening of the earth medium to resolve complexity in subsurface geology caused by inhomogeneity of the overburden strata and bedrock architectures. The subsurface geological, hydrogeophysical and engineering conditions of Etioro-Akoko, southwestern Nigeria, were investigated using electrical resistivity tomography (ERT). This was aimed at unravelling the hydrogeodynamic and litho-structural complexity that are responsible for low groundwater yield in wells/boreholes and foundation failures. Field 2D resistivity data sets of the study area were inverted and used to produce geotomographic models for detailed insights into the complex subsurface geological setting. Results of the 2D resistivity inverted models showed three to four distinct layers; the topsoil, weathered layer, partially weathered/fractured bedrock and fresh bedrock. Bedrock structures occasioned by fracturing and deep weathering of the bedrock were delineated with resistivities and thicknesses ranging from 40 to 950 Ωm and 10–25 m, respectively. The fracture systems; F1, F2, F3, F4 and F5 in NW-SE, NNW-SSE, NE-SW and ENE-WSW orientations act as the major groundwater collecting centres in the area. The orientations and geometries of these geologic features are the manifestations of structural deformation of the underlying geology. Fourteen hand-dug well and four borehole points were proposed based on the ERT results. Conversely, the localised bedrock structures and oscillating bedrock topography were suggestive of potential threats to the foundations of engineering structures in the studied area. Reinforcement of concrete foundations at certain sites where ERT suggested that the underlying strata were not capable of bearing loads was recommended as well. This study has offered a detailed understanding of the subsurface geological disposition for sustainable groundwater development and siting of durable civil engineering structures in the studied area and other areas with typical complex geological settings.
利用电阻率层析成像技术对尼日利亚西南部Etioro-Akoko的地下地质、水文地球物理和工程特征进行了描述
非侵入性地电地下表征提供了对地球介质的筛选,以解决由覆盖层和基岩结构的不均匀性引起的地下地质复杂性。利用电阻率层析成像技术(ERT)对尼日利亚西南部Etioro-Akoko地区的地下地质、水文地球物理和工程条件进行了研究。该研究旨在揭示导致井/钻孔中地下水产量低和基础破坏的水文地球动力学和岩石构造复杂性。对研究区域的现场二维电阻率数据集进行了反演,并用于生成地理层析模型,以详细了解复杂的地下地质环境。二维电阻率反演模型结果显示出3 ~ 4个明显的分层;表土、风化层、部分风化/断裂基岩和新鲜基岩。圈定了基岩破裂和深度风化作用形成的基岩构造,其电阻率和厚度分别为40 ~ 950 Ωm和10 ~ 25 m。裂缝系统;NW-SE、NNW-SSE、NE-SW和ENE-WSW方向的F1、F2、F3、F4和F5是该地区主要的地下水收集中心。这些地质特征的方位和几何形状是下伏地质构造变形的表现。根据ERT结果,提出了14口手挖井和4个钻孔点。相反,基岩构造的局部性和基岩地形的震荡提示了研究区工程结构基础的潜在威胁。此外,建议在某些地点对混凝土基础进行加固,因为在这些地点,ERT认为下伏地层无法承受荷载。该研究为研究区和其他典型复杂地质环境地区地下水可持续开发和耐久土木工程结构选址提供了详细的地下地质配置。
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