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Predicting the depth of penetration of DNAPLs in fractured aquifers: Facing the uncertainties

机译:预测骨折含水层中DNAPLS的渗透深度:面对不确定因素

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We are now facing the legacy of over half a century of groundwater pollution resulting from the release of dense non-aqueous phase liquids (DNAPLs), in particular the chlorinated solvents, to the subsurface. Only recently has the severity and scale of the contamination been made apparent. The rapid migration of DNAPLs is promoted by the presence of preferential pathways such as fractures, which are ubiquitous in the majority of bedrock aquifers. However, heterogeneity, inherent at a range of scales in all fractured rocks, suggests that accurate prediction of the fate of DNAPLs will be limited by our abilities to measure, interpret and represent key fracture parameters. The broader objectives of the study are to provide results that will enhance risk assessment, focus remediation technologies, and develop better management of groundwater resources.
机译:我们现在面临超过半个世纪的地下水污染,由致密的非水相液(DNAPLS),特别是氯化溶剂,含有氯化溶剂。只有最近的污染的严重程度和规模显而易见。通过优先途径(如骨折)的存在,促进了DNAPL的快速迁移,这些裂缝是大多数基岩含水层中普遍存在的裂缝。然而,所有骨折岩石中一系列鳞片固有的异质性表明,准确预测DNAPLS的命运将受到我们测量,解释和代表关键骨折参数的能力的限制。该研究的更广泛的目标是提供将提高风险评估,重点修复技术的结果,并培养更好地管理地下水资源。

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