尼日利亚Ekpoma地区含水层垂直电测深研究。

F. Ezomo, S. Ifedili
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引用次数: 1

摘要

利用斯伦贝谢阵列垂直电测深(VES)技术,在尼日利亚埃多州eguure - egoro、Ekpoma地区对含水层或含水地层进行了调查。该阵列的最小钻距为2m,最大钻距为500m。由于该地区严重缺水,调查equale - egoro含水层存在的必要性变得不可避免。该地区严重缺水主要是由于其不利的气候和地质条件,使含水层非常深。考虑到机器的大泵送距离,这个大深度常常导致钻孔失效。初步采用曲线解译,提供计算机迭代模型。获得的结果以地电剖面的形式呈现,然后使用钻孔测井作为对照进行解释,以检测该地区遇到的各种岩性和含水层的存在。含水层可能是砂、粘土、砂石和或粘土夹层砂。探测到的现有含水层的电阻率值从40欧姆到12000欧姆不等。JONAMP Vol. 11 2007: 597-604页
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Vertical electric sounding investigation of aquifers in the Ekpoma area of Nigeria.
Aquifers or water bearing formations existence was investigated in Eguare-Egoro, Ekpoma, Edo State, Nigeria by using vertical electric sounding (VES) of schlumberger array. The array was employed with minimum drilling spread of 2m and maximum spread of 500m. The need to investigate aquifer existence in Eguare-Egoro becomes inevitable because of acute shortage of water in the area. The acute shortage of water in the area is primarily due to its unfavourable climate and geology that made the aquifer level to be very deep. This great depth often leads to borehole failure considering the great pumping distance of the machine. Interpretation of data was done initially by curve which provided computer iterative model. The results obtained were presented in the form of geoelectric sections which was then interpreted using bore-hole log as a control to detect various lithologies encountered and aquifers existence in the area. The aquifers are probably sands, clays, sand stones and or sands with clay intercalation. The resistivity values for the existed aquifers detected vary from 40 ohm-m to 12,000 ohm-m. JONAMP Vol. 11 2007: pp. 597-604
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