电磁法对地下水状态的启发式评价

Olagoke Victoria Oluwadamilola, Adekitan Adetoun Abimbola, B. Hassan Tolulope, Vincent Olufunke Rebecca
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引用次数: 0

摘要

利用电磁地球物理方法对奥贡州Odeda地方政府Obantoko的Oloruntedo社区的地下水状况进行了评估,以划定研究区内最丰富的含水层单元。本文提出了一种启发式的地下水产量评价方法。在整个测量区域建立了六(6)条电磁横向或剖面。利用PQWT-TC150型地球物理探水设备,在现有钻孔和手挖井附近进行调查,对裂缝和风化带进行了生动的刻印。调查区域的水文地质意义描绘了横断面内的地下水结构。研究结果生成了每个横向位置的曲线图和地下剖面图。结果表明,随着含水层深度的变化,EM剖面1、3、6具有较高的地下水势区,而EM剖面4、5具有较低的地下水势区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Heuristic Evaluation of the State of Groundwater Using Electromagnetic Method
The Electromagnetic (EM) geophysical method was used to assess the groundwater condition of the Oloruntedo community in Obantoko, Odeda Local Government of Ogun State, to delineate the most prolific aquifer unit within the study area. This study presents a heuristic evaluation of ground water yield. Six (6) EM transverses or profiles were established across the survey area. The survey was run close to existing boreholes and hand-dug wells to vividly imprint the fracture and the weathered zone using PQWT-TC150 geophysical water detector equipment. The hydrogeologic significance of the surveyed area delineates the groundwater architecture within the traverses. The results obtained from this study produced curve graphs and subsurface profile maps of each transverse location. It was observed from the result that EM profile 1, 3, and 6 has a high groundwater potential with varying aquifer depth, while EM profile 4 and 5 imprint a low groundwater potential zone.
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