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Geoelectric assessment of groundwater prospect and vulnerability of overburden aquifers at Adumasun Area, Oniye, Southwestern Nigeria

机译:尼日利亚西南部奥尼耶市Adumasun地区地下水前景和覆盖层含水层脆弱性的地电评估

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Adumasun lies on a Precambrian basement complex of Southwestern Nigeria. Some kilometers away from the study area especially at Igangan is characterized by outcrops of crystalline basement rocks. Inadequate municipal water supply from State Water Corporation, coupled with hydrogeologically difficult nature of the terrain, individuals and corporate bodies indiscriminately sink tube wells and boreholes within the unconsolidated overburden materials, with glaring lack of concerns for the vulnerability status of aquifers, and possible environmental risk. Vertical Electrical Sounding method was used to map Adumasun area, Oniye, Oyo State with a view to assessing the groundwater prospect, focused on the thickness of the unconsolidated materials overlying the crystalline bedrock. The resistivity parameters of the geoelectric topmost layer across the area were also used to assess the vulnerability of the underlying aquifers to near-surface contaminants. The thickness of the unconsolidated overburden varies from 3.1m to 20.1m, where about 60% falls within the 10m-14.9m brackets. This shows that unconsolidated materials are not thick and hence averagely low groundwater prospect. 80% of the topmost geoelectric layer in the study area has resistivity mostly within the range of 1-100Wm. Resistivity values within these brackets tend to indicate silt or clay sequence, which can constitute effective protective geologic barriers for the underlying aquifers. This suggests that aquifers within the unconsolidated overburden at Adumasun are mostly capped by impervious/semi-pervious materials, geologically protecting the underlying aquifers from near-surface contaminants.
机译:Adumasun位于尼日利亚西南部的前寒武纪地下室。距研究区几公里的地方,特别是在伊甘甘(Igangan),其特征是结晶基底岩石的露头。国家供水公司的市政供水不足,再加上地形的水文地质困难性,个人和公司团体在未固结的覆盖层材料中不加选择地将管井和钻孔下沉,明显担心水层的脆弱性以及可能的环境风险。为了评估地下水前景,使用垂直电测深法绘制了奥尤州奥尼耶市阿杜马松地区的地图,重点是覆盖在结晶基岩上的未固结材料的厚度。整个区域中地电最上层的电阻率参数也用于评估下伏含水层对近地表污染物的脆弱性。未固结覆盖层的厚度从3.1m到20.1m不等,其中约60%位于10m-14.9m范围内。这表明未固结的物质并不厚,因此地下水前景一般较低。研究区域最顶层的地电层中80%的电阻率大多在1-100Wm的范围内。这些括号内的电阻率值往往表示粉砂或黏土层序,可对下伏含水层构成有效的保护性地质屏障。这表明,Adumasun松散覆盖层内的含水层大部分被不透水/半透水材料所覆盖,在地质学上保护了下层含水层免受近地表污染物的污染。

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