尼日利亚富格尔江户州地下水水文地球物理调查

Omasheye G.A.J, Onavwie Ufuoma, Ekibade Jahswill
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引用次数: 0

摘要

利用斯伦贝谢电极阵列配置进行12台垂直电测深(VES)获取数据,并采用斯伦贝谢自动解释分析方法。研究区岩性剖面显示该区为基底杂岩,地表下为较厚的新鲜基底。风化基底的电阻率较低,是地下水的良好聚集地。对数据的解释显示,在VES位置有9个地电层,总累积厚度为203.55m (677.82ft)、272.29m (906.73ft)和27l。43米(903.83英尺)深。从地下物质的地质解释来看,这些值表明对含水层进行了更深入的探测。该研究将为研究地点(江户州Etsako中央地方政府Fugar)的有效含水层位置提供指导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
HYDROGEOPHYSICAL SURVEY FOR UNDERGROUD WATER IN FUGAR EDO STATE NIGERIA
Twelve (12) vertical electrical sounding (VES) was done using the Schlumberger electrode array configuration to obtain data and the Schlumberger automatic analysis method of interpretation was adopted. The lithological section of the study area revealed that the area is a basement complex with a thick fresh basement beneath the surface. The weathered basement is a good accumulation for underground water due to its low resistivity values. The interpretation of the data showed a resolution of nine geoelectric layers for the VES locations and a total cumulative thicknesses of 203.55m (677.82ft), and 272.29m (906.73ft) and 27l.43m (903.83ft) depth. From the geologic explanation of the subsurface materials, these values indicate a deeper probing into the aquifer zone. This study would give a guide on effective aquifer layer position in the studied locations (Fugar, Etsako Central Local Government of Edo State).
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