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The influence of detailed aquifer characterization on groundwater flow and transport models at Schoolcraft, Michigan.

机译:密歇根州Schoolcraft的详细含水层表征对地下水流和运输模型的影响。

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Aquifer characterization is a key aspect of any groundwater study, however it is difficult to determine when an aquifer has been adequately characterized. This study explored several methods of describing aquifer properties and the value of knowing those properties for developing accurate groundwater flow and transport simulations. Data collected from an aquifer bioremediation study in Schoolcraft Michigan was used for this research. The value of incorporating various levels of aquifer characterization was assessed using groundwater flow and transport simulations. The relationship between several aquifer properties including grain-size, ground penetrating radar velocity, and hydraulic conductivity were explored using rock physics approaches. Regional aquifer porosity estimates were estimated using ground penetrating radar tomography, and the impact of these porosity values were evaluated in solute transport models. The approaches developed through this research can be applied to future studies to help design cost-effective sampling strategies for detailed aquifer characterization.
机译:含水层的表征是任何地下水研究的关键方面,但是很难确定何时对含水层进行了充分的表征。这项研究探索了几种描述含水层特性的方法以及了解这些特性对开发准确的地下水流和输运模拟的价值。这项研究使用了从密歇根州Schoolcraft进行的含水层生物修复研究中收集的数据。使用地下水流和运输模拟评估了结合不同水平的含水层特征的价值。使用岩石物理学方法探索了包括粒度,探地雷达速度和水力传导率在内的几个含水层特性之间的关系。使用地面穿透雷达层析成像技术估算区域含水层孔隙度,并在溶质运移模型中评估这些孔隙度值的影响。通过这项研究开发的方法可以应用于未来的研究,以帮助设计具有成本效益的采样策略,以进行详细的含水层表征。

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