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Geophysical Survey as a Surface Tool in Groundwater Exploration in Delta North District, Nigeria

机译:尼日利亚三角洲北区地下水勘探中的地球物理调查

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Geophysical survey based on electrical resistivity method employing the techniques of vertical electrical sounding (VES) was carried out in order to investigate Groundwater existence in Delta North District, of Nigeria. This research work became necessary in order to solve the problem of acute water shortage in the area by way of prospecting or searching for additional aquifers which would subsidize the existing one, domestically, industrially and agriculturally. Ten (10) vertical electrical sounding (VES) (uniformly distributed) tests were conducted in the area and its environs using "Schlumberger" electrode array. The VES were carried out with half current electrode spacing with the spread Im-928m at six (06) points per decade. The results of the interpretation identified wet sand/clean sand as perched aquifer which can deliver ground water to the bore-hole at perceptible rates between depths of 85m to 145m below sea level. The resistivity of the aquifer detected varied from 95.0 ohm-m to 110,000 ohm-m while the thickness ranged from 30.0m to 105.0m.
机译:进行了基于采用垂直电气探测技术(VES)技术的电阻率法的地球物理测量,以调查尼日利亚三角洲北区地下水存在的地下水存在。这项研究工作是必要的,以便通过勘探或寻求额外的含水层来解决该地区急性缺水问题,该含水层将在国内,工业上和农业地补贴现有的含水层。使用“Schlumberger”电极阵列在该区域及其环境中进行十(10)次垂直电气探测(VES)(均匀分布)试验。 VES以半电流电极间距与分布IM-928M的半电极间距,每十年六(06)点。解释的结果确定了湿砂/清洁砂作为栖息的含水层,可以以85米至145米的深度为85米至145米的可察觉速度将地水送到钻孔。检测到的含水层的电阻率在95.0欧姆-m至110,000欧姆-m中变化,而厚度范围为30.0m至105.0m。

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