尼日利亚西南部Ikpere - Ekiti地下水资源的地球物理评价

E. Festus Omozeje , F. Oluwatoyin Ijasan , O. Marvellous Omorogieva
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引用次数: 0

摘要

该研究采用自然音频大地电磁法(NAFTM)研究了尼日利亚西南部Ikpere-Ekiti的地下地球物理特性。剖面图和电阻率曲线以H型、KH型、HK型和a型为主,反映了岩性、流体含量和边界界面的变化。结果表明:表土厚度为0.3 ~ 0.6 m,覆盖层深度为3.36 ~ 31.88 m,风化层延伸至56.65 m,其中Igbede、Ilesemon和GRA风化程度较高。这些条件有利于地下水的积累,静态水位为2.9-9.2 m,并且在大约120 m的深度存在一个无约束的潜水含水层。该数据与现有井眼测井数据具有很强的相关性,表明地下水存在深度可达120 m,有些井眼达到100 m。研究结果表明,可持续开发地下水以支持该地区的社会经济发展具有巨大潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geophysical assessment of groundwater resources in Ikpere – Ekiti, South Western Nigeria
The study employed the Natural Audio Frequency Telluric Method (NAFTM) to investigate subsurface geophysical properties in Ikpere-Ekiti, southwestern Nigeria. Profile maps and resistivity curves revealed predominantly H, KH, HK, and A-type curves, indicating variations in lithology, fluid content, and boundary interfaces. Results show topsoil thicknesses of 0.3–0.6 m, overburden depths of 3.36–31.88 m, and weathered layers extending up to 56.65 m, with higher weathering observed at Igbede, Ilesemon, and GRA. These conditions favor groundwater accumulation, supported by static water levels of 2.9–9.2 m and evidence of a phreatic unconfined aquifer at approximately 120 m depth. The data demonstrate strong correlation with existing borehole logs, indicating groundwater occurrence at depths up to 120 m, with some boreholes reaching 100 m. The findings suggest significant potential for sustainable groundwater exploitation to support socio-economic development in the area.
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