A Geo-Electric Survey of Potential Aquifer Inome Parts of Amaigbo, in Imo State, Using Vertical Electrical Sounding and Well Log Data

Deborah Chidimma Ndubueze, Jiriwari Amoneah, Opiriyabo Horsfal
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Abstract

The method employed was an electrical resistivity survey which was carried out to study the subsurface layer with a view of determine the depth of potential aquifers, the thickness of an aquifer, and to determine the potential aquifer for groundwater exploration. Using the Schlumberger array technique, Vertical Electric Sounding (VES), along with Self Potential well logging was carried out at six (6) VES stations in Amaigbo using the ABEM SAS 1000 terrameter and ABEM SAS 1000 logger respectively. The field data obtained have been analysed using the computer software (IP2win) which automatically interprets the apparent resistivity. The VES result revealed the heterogeneous nature of the subsurface geological sequence. Result from the Geo-electric section showed that the aquifer resistivity of the study ranges from 352\(\Omega\)\(\mathit{m}\) to 7514\(\Omega\)\(\mathit{m}\) , with potential groundwater depths ranging from 45m to 119m which shows that the study area is perfect for groundwater development. The data from the SP well logs correspond to the VES data obtained.
利用垂直电测深和测井数据对Imo州Amaigbo潜在含水层收益部分进行地电调查
该方法采用电阻率测量法对地下含水层进行研究,目的是确定潜在含水层的深度和厚度,确定地下水勘探的潜在含水层。利用斯伦贝谢阵列技术,垂直电测深(VES)和自电位测井分别使用ABEM SAS 1000和ABEM SAS 1000记录仪在Amaigbo的6个VES测深站进行。利用IP2win计算机软件对现场数据进行了分析,该软件可自动解释视电阻率。探测结果揭示了地下地质层序的非均质性。地电剖面结果表明,研究区含水层电阻率范围为352 \(\Omega\)\(\mathit{m}\) ~ 7514 \(\Omega\)\(\mathit{m}\),地下水潜在深度为45m ~ 119m,是地下水开发的理想区域。SP测井数据与获得的VES数据相对应。
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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