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A Multi-Scale Approach in Hydraulic Characterization of a Metamorphic Aquifer: What Can Be Inferred about the Groundwater Abstraction Possibilities

机译:变质含水层水力表征的多尺度方法:关于地下水提取可能性的推断

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Hard-rock aquifers, which constitute a water supply source in many countries, are highly heterogeneous and defining a realistic model of an aquifer can be extremely complex. The objective of this study was to hydraulically characterize a metamorphic aquifer in a representative area of Italy and to identify the most appropriate approach for tapping of groundwater in this challenging environment. The results of surface fracture surveys, injection tests, pumping tests, and a simplified numerical model were compared. From the surface fracture survey, a model of the rock mass characterized by a well-developed discontinuity network and by a high frequency of discontinuities resulted. The injection tests showed the extreme heterogeneity and the lower hydraulic conductivity of the rock mass in comparison with the results of the pumping tests. The independent estimate of the hydraulic parameter resulting from numerical model highlighted a range of values higher than those resulting from the pumping tests. The study demonstrated that the continuum medium approach can be used in the case of hard-rock aquifers with a dense network of discontinuities. The multi-scale approach is recommended for investigating hydraulic heterogeneity and significantly helps to identify the most promising areas for well locations and their characteristics in relation to the style of fracturing.
机译:硬岩含水层是许多国家的水源,它们是高度异质的,要定义一个现实的含水层模型可能会非常复杂。这项研究的目的是对意大利代表性地区的变质含水层进行水力表征,并确定在这种充满挑战的环境中开采地下水的最合适方法。比较了表面断裂调查,注入试验,抽水试验和简化数值模型的结果。通过表面裂缝调查,得出了一个岩体模型,该模型的特征是发达的不连续网络和高不连续频率。与泵送测试的结果相比,注入测试显示出岩体的极端异质性和较低的水力传导率。由数值模型得出的液压参数的独立估计值突出了一个比抽水试验得到的值更高的值范围。研究表明,连续介质法可用于具有不连续密集网络的硬岩含水层。建议采用多尺度方法来研究水力非均质性,并显着帮助确定最有前途的井位区域及其与压裂方式有关的特征。

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