根据电阻率数据和岩性估算尼日利亚北阿南布拉盆地 Idah 地区的含水层参数

A. I. Obasi, G.O. Aigbadon, F. Chinyem, C.N. Chukwu, J. B. Ahmed II, S.O. Abubakar, F.D. Attah, E. O. Akudo
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引用次数: 0

摘要

通过整合电阻率和岩性数据,确定了伊达地区含水层参数的特征。为此,通过应用一维斯伦贝谢(Schlumberger)电阻率阵列并将其与钻孔岩性数据相结合,共进行了二十三(23)次探测,根据经验确定了尼日利亚阿南布拉盆地北部伊达(Idah)地区的含水层参数。分析结果表明,含水层区电阻率范围在 36.65 - 2065.31 Ωm 之间,含水层厚度在 15.60 米至 66.66 米之间。其纵向电导率(S)、横向电阻率(TR)和水力传导率(k)值分别为 0.01-1.13 mhos、1518.90-90265.88 Ωm2 和 0.31-13.44 米/天。透射率 (T) 值从 4.88 到 2 557.78 米/天不等。T 与 TR 成反比,相关系数为 0.28。反射系数在-0.79 至 0.66 之间,而断裂对比度在 0.11 至 5.06 之间。结果表明,该地区地下主要是一个以断裂为主的含水层系统。岩化和成岩作用影响了水文特性。地图的中北部比南部/东部更适合地下水勘探/开发。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of aquifer parameters from electrical resistivity data and lithologs in Idah area, Northern Anambra basin, Nigeria
The parameters of the aquifers in Idah area were characterized by integrating resistivity and litholog data. To achieve this, a total of twenty-three (23) Soundings were conducted by applying the 1-D Schlumberger resistivity array and integrating it with borehole lithologs to empirically determine the aquifer parameters in the Idah area, Northern Anambra Basin, Nigeria. The results of the analyses indicate that the aquifer zone resistivity ranges from 36.65 – 2065.31 Ωm while the aquifer thickness is between 15.60 m and 66.66 m. Its values of the longitudinal conductance (S), transverse resistance (TR), and hydraulic conductivity (k) are 0.01-1.13 mhos, 1518.90-90265.88 Ωm2 , and 0.31-13.44 m/day, respectively. The transmissivity (T) values vary from 4.88 to 2 557.78 m /day. T is inversely proportional to TR with a correlation coefficient of 0.28. The result of the reflection coefficient is in the range of -0.79 to 0.66, while that of the fractured contrast is between 0.11 and 5.06. The results suggest that an aquifer system that is predominantly fracture-based is underlying the region. Lithification and diagenesis influence the hydrological properties. The northern–central portions of the map are more suitable for groundwater exploration /exploitation than the southern/eastern ends. 
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