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Evaluation of modeling approaches to simulate contaminant transport in a fractured limestone aquifer

机译:评估模拟方法来模拟裂缝性石灰岩含水层中的污染物运移

摘要

Understanding the fate and transport of contaminants in limestone aquifers is important because they are a major drinking water resource. This is challenging because they are often heavily fractured and contain chert layers and nodules. Several modeling approaches have been developed to describe contaminant transport in fractured media, such as discrete fracture, equivalent porous media, and dual continuum models. However, these modeling concepts are not well tested for real limestone geologies. Our goal is therefore to develop, evaluate and compare approaches for modeling transport of contaminants in fractured limestone aquifers. The model comparison is conducted for a contaminated site in Denmark, where a plume of dissolved PCE has migrated through a fractured limestone aquifer. Field data includes information on spill history, distribution of the contaminant (multilevel sampling), geology and hydrogeology. To describe the geology and fracture system, data from borehole logs and cores was combined with an analysis of heterogeneities and fractures from a nearby excavation and pump test data. We present how field data is integrated into the different model concepts. A challenge in the use of field data is the determination of relevant hydraulic properties and interpretation of aqueous and solid phase contaminant concentration sampling data. Traditional water sampling has a bias towards fracture sampling; however, concentrations in the limestone matrix are needed for assessing contaminant rebound and remediation strategies. Each model is compared with field data, considering both model fit and model suitability. Results show a considerable difference between the approaches, and that it is important to select the right one for the actual modeling purpose. The comparison with data showed how much information is required to discriminate between models, and recommendations on how to identify the best modeling approach are made.
机译:了解石灰石含水层中污染物的去向和运输很重要,因为它们是主要的饮用水资源。这是具有挑战性的,因为它们经常被严重折断并且包含石层和结节。已经开发了几种建模方法来描述裂缝介质中的污染物运移,例如离散裂缝,等效多孔介质和双重连续介质模型。但是,这些建模概念并未针对真实的石灰岩地质条件进行良好的测试。因此,我们的目标是开发,评估和比较模拟破碎石灰岩含水层中污染物运移的方法。模型比较是在丹麦一个受污染的地点进行的,在那里,一股溶解的PCE羽流已通过裂缝的石灰岩含水层迁移。现场数据包括有关泄漏历史,污染物分布(多级采样),地质和水文地质的信息。为了描述地质和裂缝系统,将来自钻孔测井和岩心的数据与来自附近开挖和泵测试数据的非均质性和裂缝分析相结合。我们介绍了如何将现场数据集成到不同的模型概念中。使用现场数据的一个挑战是确定相关的水力特性以及解释水相和固相污染物浓度采样数据。传统的水采样偏向于裂缝采样。但是,需要使用石灰石基质中的浓度来评估污染物的反弹和修复策略。考虑模型拟合和模型适用性,将每个模型与现场数据进行比较。结果表明这两种方法之间存在很大差异,因此对于实际的建模目的选择正确的方法非常重要。与数据的比较表明,区分模型需要多少信息,并就如何确定最佳建模方法提出了建议。

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