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Application Of Electromagnetic Method And Electrical Resistivity Sounding In Hydrogeological Studies, A Case Study Of Vandeikya Area, Central Nigeria

机译:电磁法和电阻率测深法在水文地质研究中的应用-以尼日利亚中部范德基亚地区为例

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Abstract: VLF-EM profiles and Schlumberger depth soundings were carried out in Vandeikya area of Central Benue Trough of Nigeria. The area is underlain by both sedimentary and Basement complex rocks.Groundwater potential and aquifer characteristics of the area were analized using Dar Zarrouk parameters. The geoelectric data acquired were interpreted using partial curve matching, IX1D, Surfer, Grapher and Win-Resist software programmes. The qualitative interpretation of VLF-EM results identifies areas of hydro-geologic importance and forms basis for Schlumberger depth soundings. The study shows that most aquifers in the area lie between the second and the third layer with resistivity varying from 29.5-232.7Ωm. The thicknesses of aquifers in the area vary between 7.3-38.0m. Overburden thicknesses in the area vary between 0.9-6.7m. The study shows that aquifers in the area are prolific with the exception of VES 8 and VES 10 with poor hydrogeologic significance. Dar Zarrouk parameter of longitudinal conductance revealed that transmissivity within the area ranges from 0.49-13.99m2/day.However hydraulic conductivity in the area ranges from 0.0671-1.7124. Correlation coefficient between the modeled transmissivity and hydraulic conductivity gave R2 value of 0.8249 which signifies a perfect correlation.
机译:摘要:在尼日利亚中部贝努海槽的Vandeikya地区进行了VLF-EM剖面和斯伦贝谢深度探测。该地区被沉积岩和基底复杂的岩石所覆盖。使用Dar Zarrouk参数分析了该地区的地下水位和含水层特征。使用部分曲线匹配,IX1D,Surfer,Grapher和Win-Resist软件程序来解释获取的地电数据。 VLF-EM结果的定性解释确定了水文地质重要区域,并为斯伦贝谢深度探测奠定了基础。研究表明,该地区大多数含水层位于第二层和第三层之间,电阻率范围为29.5-232.7Ωm。该地区含水层的厚度在7.3-38.0m之间变化。该区域的覆盖层厚度在0.9-6.7m之间变化。研究表明,该地区的含水层丰富,但VES 8和VES 10的水文地质意义较差。 Dar Zarrouk的纵向电导率参数表明,该区域的渗透率范围为0.49-13.99m2 / day,而该区域的水力传导率范围为0.0671-1.7124。所模型的透射率与水力传导率之间的相关系数给出的R2值为0.8249,这表示一个完美的相关性。

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