Geophysical Investigation of Groundwater Potentials of the Nanka Sand in Obosi and Its Environs, Anambra State Nigeria

Nelson Onyebuchi Nwobi, Solomon Ekene Okeke, Chekwube Nnamdi Didi, Augustine Obiora Okpara
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Abstract

Geophysical investigation for Groundwater which entails the use of vertical electrical sounding (VES) methods was carried out in parts of the Idemili area of Anambra State, Nigeria. Geologically the study area falls within the Nanka Sand, belonging to the Ameki Group in the Tertiary Niger Delta Basin. The investigation intends amongst others to assess the groundwater potential of the area, find out the existence of possible aquifer(s) within the area, and es-timate the possible depth of a borehole. 15 VES stations were established at the site using Ohmega System Tetrameter and Schlumberger electrode configuration with current electrode spacing (AB/2) of 350 meters. The geologic parameters, such as the number of geo-electric layers, the thickness of the geo-electric units, and their resistivities were interpreted from the VES curves. A qualitative assessment of the curves shows that a model with 5 layers would sufficiently model the field curves. The thickness value ranged from 0.1 to 86 m, the resistivity ranged from 258 to 13,258 Ωm, and the depth ranged between 1.2 and 109 m. Quantitative interpretation of field curves involved inversion with appropriate parameters using Zond Res1D software.
尼日利亚阿南布拉州奥博西及其周边地区南卡砂地下水位地球物理调查
在尼日利亚阿南布拉州的Idemili地区的部分地区进行了地下水地球物理调查,其中需要使用垂直电测深(VES)方法。研究区在地质上属于南卡砂组,属于尼日尔三角洲盆地的Ameki组。这项调查的目的之一是评估该地区的地下水潜力,找出该地区可能存在的含水层,并估计钻孔的可能深度。在现场建立了15个VES站,采用Ohmega System Tetrameter和斯伦贝谢电极配置,电流电极间距(AB/2)为350米。利用地震测深曲线解释了地电层数、地电单元厚度及其电阻率等地质参数。曲线的定性评价表明,一个5层的模型可以充分地模拟野外曲线。厚度范围为0.1 ~ 86 m,电阻率范围为258 ~ 13258 Ωm,深度范围为1.2 ~ 109 m。利用Zond Res1D软件,利用适当的参数进行反演,实现了场强曲线的定量解释。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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