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On the sub-model errors of a generalized one-way coupling scheme for linking models at different scales

机译:关于在不同尺度上链接模型的广义单向耦合方案的子模型误差

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Multi-scale modeling of the localized groundwater flow problems in a large-scale aquifer has been extensively investigated under the context of cost-benefit controversy. An alternative is to couple the parent and child models with different spatial and temporal scales, which may result in non-trivial sub-model errors in the local areas of interest. Basically, such errors in the child models originate from the deficiency in the coupling methods, as well as from the inadequacy in the spatial and temporal discretizations of the parent and child models. In this study, we investigate the sub-model errors within a generalized one-way coupling scheme given its numerical stability and efficiency, which enables more flexibility in choosing sub-models. To couple the models at different scales, the head solution at parent scale is delivered downward onto the child boundary nodes by means of the spatial and temporal head interpolation approaches. The efficiency of the coupling model is improved either by refining the grid or time step size in the parent and child models, or by carefully locating the sub-model boundary nodes. The temporal truncation errors in the sub-models can be significantly reduced by the adaptive local time-stepping scheme. The generalized one-way coupling scheme is promising to handle the multi-scale groundwater flow problems with complex stresses and heterogeneity. (C) 2017 Elsevier Ltd. All rights reserved.
机译:在成本效益争论的背景下,已经对大规模含水层中局部地下水流问题的多尺度模型进行了广泛研究。一种替代方法是将具有不同空间和时间范围的父子模型耦合在一起,这可能会导致感兴趣的局部区域出现非平凡的子模型错误。基本上,子模型中的此类错误源于耦合方法的不足以及父子模型的空间和时间离散化不足。在这项研究中,鉴于其数值稳定性和效率,我们研究了广义单向耦合方案中的子模型误差,这为选择子模型提供了更大的灵活性。为了以不同的比例耦合模型,通过空间和时间头部插值方法将父比例的头部解决方案向下传递到子边界节点上。通过完善父模型和子模型中的网格或时间步长大小,或通过仔细定位子模型边界节点,可以提高耦合模型的效率。子模型中的时间截断误差可以通过自适应局部时间步长方案显着降低。广义的单向耦合方案有望解决具有复杂应力和非均质性的多尺度地下水流问题。 (C)2017 Elsevier Ltd.保留所有权利。

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