尼日利亚西南部伊巴丹idii - ayunre含水层脆弱性Godt法多准则分析方法

Olukayode O.O., B. O.O., Adebisi N.O., Mosuro G.O., Ariyo S.O., Orimogunje O.B.
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摘要

利用垂直电测深(VES)斯伦贝谢阵列对伊巴丹的Idi-Ayunre进行了地球物理调查,这是一个典型的基底复杂地区,岩石成分为混杂岩-片麻岩、石英岩和黑云母-角闪岩。利用电阻率仪及其附件,在最大电流电极间距为100m的条件下,共获得40条垂直电测深数据。本研究的目的是评价研究区含水层对污染的脆弱性。利用部分曲线匹配对VES结果进行定性和定量解释,并进一步使用WINRESIST进行计算机迭代。生成并综合纵向导度、上覆含水层厚度和水力导度,生成脆弱性图。根据水文地质参数建立了地下水产状、覆盖层厚度、深度和地形的GODT多准则模型,并结合纵向电导值对研究区含水层脆弱性进行了评价,并对研究区进行了分类。得到的曲线类型为H和HA。解释显示了三到四个地电层:表土层(18.9-178.9Ωm)、粘土层(9.0-70.6Ωm)、断裂基底层(31.9-43.1Ωm)和新鲜基底层(1131-2916Ωm)。纵向单位电导范围为0.032-0.93mhos。从GODT模型推导可知,研究区高脆弱性等级占92.5%,低中等脆弱性等级占2.5%,中等脆弱性等级占5%;等级高的地区比等级低、中等和中等的地区更容易受到污染。因此,可能不鼓励在高度脆弱的地区开采地下水,如有必要,应在消费前不断进行水质评价。
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Multi-Criteria Analysis Method for Aquifer Vulnerability Investigation Using Godt Method at Idi-Ayunre, Ibadan, Southwestern Nigeria
Geophysical investigation involving Vertical Electrical Sounding (VES) Schlumberger array was carried out across Idi-Ayunre, Ibadan, a typical basement complex area having a rock composition of migmatite-gneiss, quartzite, and biotite-hornblende. A total of forty (40) vertical electrical sounding data were acquired with maximum current electrode separation of 100m using resistivity meter and its accessories. The aim of the study was to evaluate the aquifer vulnerability of the study area to contamination. The VES results were both qualitatively and quantitatively interpreted using partial curve matching and were further subjected to computer iteration using WINRESIST. The longitudinal conductance, thickness of layer overlying aquifer and hydraulic conductivity were generated and synthesized to produce the vulnerability map. A GODT multi-criteria model which is an acronym of Groundwater occurrence, Overburden thickness, Depth and Topography developed from the hydrogeologic parameters were evaluated alongside the longitudinal conductance values to determine the aquifer vulnerability of the area and to classify the study area accordingly. The curve type obtained are H and HA. The interpretation revealed three to four geoelectric layers: the topsoil (18.9-178.9Ωm), clayey (9.0-70.6Ωm), fractured basement (31.9-43.1Ωm) and fresh basement (1131-2916Ωm). The longitudinal unit conductance ranges from 0.032-0.93mhos. And from the GODT model derivations, the study area shows 92.5% of high vulnerability rating, 2.5% of low-moderate and 5% of moderate rating; areas with high rating are prone to contamination than areas with low-moderate and moderate rating. Hence, zones of high vulnerability may be not be encouraged for groundwater exploitation and, if need be, constant water quality assessment should be carried out before consumption.
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