EVALUATION Of GROUNDWATER VULNERABILITY IN FRACTURED AQUIFER USING GEOELECTRIC LAYER SUSCEPTIBILITY INDEX AT OJU, SOUTHERN BENUE TROUGH NIGERIA

M. Eyankware, A. Selemo, P. Obasi, O. Nweke
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引用次数: 7

Abstract

A combination of geoelectric and hydrogeologic concept was used in the assessment of groundwater vulnerability in fractured aquifers of Oju and environs. The study area is underlain by the sediments of the Asu River Group, Southern Benue Trough Nigeria. A total of twenty-seven (27) Vertical Electrical Sounding (VES) was carried out within the study area. Geoelectric parameters (layer, resistivity and thickness) of the overlying layers across the study area were determined and used to evaluate the vulnerability of the underlying aquifers. Three charts were compared using geo-electrically derived models; LC (Longitudinal Conductance), GLSI (geoelectric layer susceptibility indexing) and GOD (groundwater occurrence, overlying lithology and depth to the aquifer. Results obtained from LC revealed that the study area fell within the moderate category, GLSI showed that aquifer vulnerability were categorize within negligible to low category and GOD fell within low to moderate category. On the average, groundwater within the study area is considered moderate vulnerable to groundwater contamination.
利用地电层敏感性指数评价尼日利亚贝努埃海槽南部OJU断裂含水层地下水脆弱性
将地电与水文地质相结合的概念应用于奥州及周边地区裂缝性含水层地下水脆弱性评价。研究区下部为尼日利亚贝努埃海槽南部阿苏河群沉积物。在研究区内共进行了27次垂直电测深(VES)。确定了研究区上覆层的地电参数(层数、电阻率和厚度),并用于评价下伏含水层的脆弱性。利用地电模型对三种图进行了比较;LC(纵向电导)、GLSI(地电层敏感性指标)和GOD(地下水产状、上覆岩性和含水层深度)。LC分析结果表明,研究区含水层脆弱性处于中等水平,GLSI分析表明,含水层脆弱性处于可忽略至低水平,GOD处于低至中等水平。平均而言,研究区内地下水易受地下水污染的程度为中等。
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