Hydrostratigraphic characterization using geoelectrostratigraphic information and hydraulic flow unit analysis for high-resolution aquifer mapping in heterogeneous systems

Ndifreke I. Udosen , Kufre R. Ekanem , Nyakno J. George
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Abstract

Accurate characterization of aquifers requires comprehensive understanding of groundwater hydraulic properties. Traditional aquifer assessment techniques are usually insufficient in characterizing hydrostratigraphic variability, leading to inaccurate prediction of aquifer flow dynamics. To address these limitations, this work integrated geoelectrical stratigraphy with hydraulic flow unit, flow zone indicator, and stratigraphic modified Lorenz plot strategies, the goal being to enhance the resolution of aquifer characterization along river channels and tributaries in Akwa Ibom State, Southern Nigeria. Unlike conventional approaches, the stratigraphic modified Lorenz plot (SMLP) provided a more precise strategy for quantifying permeability distribution within the heterogeneous aquifer system, enabling enhanced prediction of aquifer performance. Furthermore, SMLP delineated flow efficiency across the distinct hydrostratigraphic units. Results indicated the presence of four hydraulic flow units, with individual units exhibiting distinctive transmissivity properties. Computed inclination angles of the four flow units were 34°, 29°, 49°, and 33°, respectively, and these indicated the extent of hydraulic efficiency. Hydraulic flow units 1, 3, and 4 had higher transmissivity and were key conduits for groundwater flow. Hydraulic flow unit 2, on the other hand, had reduced transmissivity, indicating restricted fluid migration. The techniques employed in this study enhanced subsurface characterization and generated high-resolution and cost-effective strategies for delineating high-yield aquifer zones within river channels and tributaries with better accuracy than with use of traditional hydrogeological models. These findings are important for optimizing groundwater resource management in the study area and analogous hydrogeological settings worldwide.

Abstract Image

利用地电地层信息和水力流动单元分析进行非均质系统高分辨率含水层制图的水文地层表征
准确表征含水层需要对地下水水力特性有全面的了解。传统的含水层评价技术在表征水文地层变异性方面往往存在不足,导致含水层流动动态预测不准确。为了解决这些限制,本研究将地电地层学与水力流动单元、流动带指示器和地层修正洛伦兹图策略结合起来,目的是提高尼日利亚南部阿夸伊博姆州沿河道和支流的含水层表征的分辨率。与传统方法不同,地层修正洛伦兹图(SMLP)提供了一种更精确的策略来量化非均质含水层系统内的渗透率分布,从而增强了对含水层性能的预测。此外,SMLP还描绘了不同水文地层单元的流动效率。结果表明存在四个水力流动单元,每个单元表现出不同的透射率特性。四个流动单元的计算倾角分别为34°、29°、49°和33°,这表明了水力效率的程度。水力流单元1、3、4具有较高的透水性,是地下水渗流的关键通道。另一方面,水力流量单元2的透过率降低,表明流体运移受到限制。本研究中采用的技术增强了地下特征,并产生了高分辨率和成本效益的策略,用于描绘河道和支流内的高含水含水层,其准确性优于使用传统水文地质模型。这些发现对于优化研究区和世界范围内类似水文地质环境的地下水资源管理具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
4.70
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