尼日利亚南部翁多州地下水潜在探测的可能性

Onifade Yemi Sikiru, Egbejule Kingsley Arerebo
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引用次数: 0

摘要

针对尼日利亚Ondo州部分地区的沿海平原、砂和冲积矿床,提出了一种简便、快速的地下水勘探新方法。利用斯伦贝谢阵列垂直电测深(VES)技术对研究区地下水进行了电阻率法地球物理评价。利用ABEM四径仪(SAS 300)将8个垂直电测深测点的电阻率、厚度和层数制作成表格。绘制了现场结果,揭示了曲线类型和岩性层。图中显示q型、k型、a型和h型曲线合并,而ves3未显示任何类型的曲线。这是由于该点底泥均质沉积,非水平层状。有些测点的水平层不超过两层,例如ves1和ves3,而另一些测点的水平层最多有四层。区内基底电阻率范围为163.1 ~ 9113.4 ω -m,平均电阻率为2627.76 ω -m。在地质构造和含水层潜力方面,ves7和ves8具有良好的地质构造和含水层特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Groundwater Potential Detection Possibility in Southern Ondo State, Nigeria
A new simple and quick geophysical method for groundwater exploration of the coastal plains sands and alluvial deposits of parts of Ondo State, Nigeria has been developed. A geophysical evaluation using Electrical Resistivity method for groundwater exploration at the study area was carried out which involved the utilization of Vertical Electrical Sounding (VES) technique with schlumberger array system. About eight (8) points of vertical electrical sounding (VES) survey using ABEM tetrameter (SAS 300) was tabulated in a table which shows the resistivity, the thicknesses and the number of layers for each VES station. The field results were plotted, the curve types and lithologic layers were revealed. The plots showed type-Q, type-K, type-A and type-H curve merging while VES-3 did not reveal any type of curve. This was because of that point understudy being homogenously deposited and non-horizontally layered. Some of the VES points have horizontal layers not more than two for example, VES-1 and VES-3 whiles others have a maximum of four layers within them. The resistivity of the basement within the area ranges from 163.1 ohm-m to 9113.4 ohm-m with an average resistivity of 2627.76 ohm-m. In terms of geological structures and aquifer potential, VES-7 and VES-8 showed to possess characteristically a good geological structures and aquifers for groundwater potentials.
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