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Application of Geophysical Well Logging in Investigation of Salt–Water Intrusion in Parts of Lagos State, Southwestern Nigeria

机译:地球物理测井在尼日利亚西南部拉各斯州部分地区咸水入侵调查中的应用

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The salineation of freshwater aquifer units with the view of assessing groundwater quality in parts of Lagos State areas has been investigated in this study. The objectives task was achieved via exploring the potential of borehole geophysical method. The obtained suites of geophysical well logs covering the west – east and south – northeast directions were subjected to lithostratigraphic correlation analysis using the Petrel software. Based on the analysed results, five aquifer units characterized the study area with thickness ranging from > 5 m to 205 m were delineated. Further analysis established that saline water aquifer, brackish water sand, fresh water sand with resistivity values in the range of 0 – 60 ohm-m, 60 – 80 ohm-m and > 80 ohm-m, respectively at the depths of 10 – 165 m were delineated using the resistivity well log tool along the lithostratigraphic sequence. It was evidenced from the analysis that saline water often occurred greatly at depth of 10 – 160 m and the depth at which fresh water can occur in the area is greater than 200 m along the east – west and 0 – 200 m in the southwest – northeast sections. This study concludes that borehole geophysical wireline logs can be effectively relied upon in the delineation of aquifer units and assessment of groundwater quality in the investigated area.
机译:为了评估拉各斯州部分地区的地下水水质,已经研究了淡水含水层单元的盐化作用。通过探索钻孔地球物理方法的潜力,实现了目标任务。使用Petrel软件对获得的覆盖西,东和南,东北方向的地球物理测井套件进行岩体地层相关分析。根据分析结果,划定了五个研究区域的含水层单元,厚度范围从> 5 m到205 m。进一步的分析表明,在10 – 165的深度处,盐水层,微咸水砂,淡水砂的电阻率值分别在0 – 60 ohm-m,60 – 80 ohm-m和> 80 ohm-m范围内使用电阻率测井工具沿着岩石地层层序划定了m。分析表明,咸水通常在10 – 160 m的深度处大量发生,而该区域沿东–西部的深度大于200 m,而在西南– 0 – 200 m的深度可以发生淡水。东北部分。这项研究得出的结论是,在确定调查区域的含水层单位和评估地下水质量时,可以有效地依靠钻孔地球物理电缆测井。

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