Zonation of coastal geo-electrostratigraphic units via stratigraphic modified Lorenz plots and rock typing

Ndifreke I. Udosen
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Abstract

The characterization of aquifers presents hydrogeophysical challenges due to complexities inherent in their lithology and groundwater flow regimes. This work advances subsurface characterization by integrating geoelectrostratigraphic information with a hydraulic flow unit (HFU) and flow zone indicator framework. Comprehensive geoelectrical surveys were conducted within a heterogeneous coastal milieu, the goal being to delineate the spatial architecture of the aquifer system. The surveys yielded resistivity distributions indicating stratified geological formations comprising fine-to-coarse grained sands intercalated with low-permeability clay horizons. The introduction of the stratigraphic modified Lorenz plots (SMLP) refined the permeability-porosity relationship by revealing spatial variations in flow efficiency, thereby differentiating between conductive and superconductive hydraulic zones. Hydraulic conductivity ranged from 5.29 × 10–6 to 8.79 × 10–5 m/s, permeability ranged from 751.24 to 12467.23 mD, hydraulic capillary radius ranged from 1.21 × 10–6 to 3.25 × 10–6 m, and Aquifer Quality Index ranged from 1.65 to 4.83. Via the application of petrophysical correlations, four distinct hydraulic flow units (HFU1–HFU4) were identified based on values of permeability, effective porosity, and Flow Zone Indicator (FZI). The steeper slope of HFU3 suggested enhanced groundwater transmissivity, whereas the moderate slopes of HFU1, HFU2, and HFU4 indicated restricted hydraulic connectivity. A major novelty of this study lies in integrating petrophysical, electro-hydraulic, and geospatial data to generate high-resolution 2D parametric maps. This approach has enabled the visualization of spatial permeability distributions and groundwater storage variations, offering a diagnostic tool for aquifer productivity assessment. The results obtained have implications for optimizing groundwater extraction strategies and improving regional water resource management policies.
通过地层修正洛伦兹图和岩石分型划分海岸地电地层单元
由于含水层的岩性和地下水流动状况固有的复杂性,对含水层的表征提出了水文地球物理挑战。这项工作通过将地电地层信息与水力流动单元(HFU)和流动带指示框架相结合来推进地下表征。在异质海岸环境中进行了全面的地电调查,目的是描绘含水层系统的空间结构。调查结果显示,电阻率分布表明层状地质地层包括细粒至粗粒砂岩,夹层为低渗透粘土层。地层修正洛伦兹图(SMLP)的引入通过揭示流动效率的空间变化来细化渗透率-孔隙度关系,从而区分导电和超导水力带。水力导率范围为5.29 × 10-6 ~ 8.79 × 10-5 m/s,渗透率范围为751.24 ~ 12467.23 mD,水力毛管半径范围为1.21 × 10-6 ~ 3.25 × 10-6 m,含水层质量指数范围为1.65 ~ 4.83。通过应用岩石物理相关性,根据渗透率、有效孔隙度和流动区指标(FZI)的值,确定了4种不同的水力流动单元(HFU1-HFU4)。HFU3坡度较陡表明地下水通过性增强,而HFU1、HFU2和HFU4坡度适中表明水力连通性受限。该研究的一个主要新颖之处在于整合岩石物理、电液和地理空间数据,生成高分辨率的2D参数图。该方法实现了空间渗透率分布和地下水储量变化的可视化,为含水层产能评估提供了一种诊断工具。研究结果对优化地下水开采策略和改进区域水资源管理政策具有重要意义。
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