Re-Construction of Palaeo-Sedimentation Processes of Aquifers underlying Igueben and Environs using Geo-Electrical Resistivity Signature and Borehole Data

Salufu S. O., Aigbedion I., Atama J. O.
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Abstract

ISSN: XXXX-XXXX Abstract: Igueben is located in the central of Edo State, Nigeria. It has neighbouring towns; Ogwa, Ugbegun, Ugiogba, Ebelle, and Ekpon. These towns have the same aquifer but significant variations in the water table. However this study was intended to unravel the salient ancient hydrological processes that occurred in the study area which resulted to this variation. Vertical electrical sounding (VES) data and borehole data of the area were integrated to generate geoelectrical resistivity section of the area, to identify the aquifer trends, body, and shape in order to re-construct the palaeo-sedimentation processes of the aquifers that underlie Iguebe and the neighbouring towns. The inversion model result for the seven VES conducted in the study area showed that the curve types are HQA, AHA, A, AHA, AHA, HAQ, and AQA, respectively. These curve type suggested that the aquifer type is arenite sandstone aquifer that has been transported from a long distance. The geo-electrical pattern and shape showed that Igueben and Ogwa (shallow marine) are the point of deposition from where other nearby towns (Ugbegun, Ugiogba, Ebelle, and Ekpon) sourced their aquifer by gravity settling from suspended sediments in water body into adjacent deep marine environment (Ugbegun, Ugiogba, Ebelle, and Ekpon).This geological processes were responsible for the variation in the water table in the study area.
利用地电阻率特征和钻孔资料重建伊格本及其周边含水层古沉积过程
摘要:伊格本位于尼日利亚埃多州中部。它有邻近的城镇;Ogwa, ugbegan, Ugiogba, Ebelle和Ekpon。这些城镇有相同的含水层,但地下水位有很大的变化。然而,本研究旨在揭示研究区域发生的导致这种变化的显着古代水文过程。将该地区的垂直电测深(VES)数据和钻孔数据相结合,生成该地区的地电阻率剖面,以识别含水层趋势、体和形状,从而重建Iguebe及其邻近城镇地下含水层的古沉积过程。对研究区7个VES反演模型结果显示,曲线类型分别为HQA、AHA、A、AHA、AHA、HAQ、AQA。这些曲线类型表明该含水层类型为长距离运移的砂质砂岩含水层。地电模式和形状表明,伊格本和小洼(浅海)是附近其他城镇(乌格京、乌乔巴、埃贝尔和埃克蓬)通过重力沉降将水体中的悬浮沉积物引入邻近的深海环境(乌格京、乌乔巴、埃贝尔和埃克蓬)的沉积点。这种地质作用是造成研究区地下水位变化的主要原因。
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