尼日利亚南部沿海地区的水文地质评估和含水层潜力:VES 勘测和空间分析的启示

J. A. Umoh, Okechukwu Ebuka Agbasi, N. George, Emem Mbong, Udofia Mfoniso Aka
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引用次数: 0

摘要

本研究利用在尼日利亚埃凯特进行的垂直电测(VES)勘测对含水层特性进行了全面分析,以应对沿海地区地下水管理的挑战。采用垂直电测法进行了水文地质电气分析,并调查了该地区的水文地质动态。结果表明,不同的地下水层具有不同的电阻率值。空间分布分析表明,人口密集地区的电阻率较低,而人口稀少地区的电阻率较高。标为 EK2 的空间位置的含水层最大,达 246.70 米,主要位于研究区中部。含水层深度从 87.10 米到 250.20 米不等,厚度的变化凸显了地理异质性及其对地下水传输的影响。地下水特征的这些空间差异对于了解地下水运动、储存和开采潜力至关重要。研究强调了孔隙度的显著差异,反映了含水层储水能力和易受污染程度的不同。这些发现对地下水流速和开采可行性具有重要影响。这项研究为水文地质调查和地下水资源管理提供了重要数据,强调了地质构造、含水层特性、人类活动之间错综复杂的关系,以及可变孔隙度区域的潜在污染风险。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrogeological assessment and aquifer potential of a coastal area, South Nigeria: insights from VES surveys and spatial analysis
This study provides a comprehensive analysis of aquifer properties using vertical electrical sounding (VES) surveys conducted in Eket, Nigeria, to address the challenges of groundwater management in coastal areas. The VES method was employed for hydrogeo-electrical analysis and to investigate the hydrogeological dynamics of the region. The results reveal varying subsurface layers with distinct resistivity values. Spatial distribution analysis indicates densely settled areas exhibit lower resistivities, while sparsely settled regions show higher resistivities. The spatial location labeled EK2 features the largest aquifer, measuring 246.70 m, predominantly located in the central research area. Aquifer depths range from 87.10 to 250.20 m, with variations in thickness highlighting geographical heterogeneity and its impact on groundwater transport. These spatial differences in groundwater characteristics are crucial for understanding groundwater movement, storage, and extraction potential. The study underscores significant variability in porosity, reflecting differences in the aquifers’ water storage capacity and susceptibility to contamination. These findings have important implications for groundwater flow rates and extraction feasibility. The research provides essential data for hydrogeological investigations and groundwater resource management, emphasizing the intricate relationship among geological formations, aquifer properties, human activities, and the potential risks of contamination in variable porosity zones.
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