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首页> 外文期刊>Transport in Porous Media >Pre-asymptotic Transport Upscaling in Inertial and Unsteady Flows Through Porous Media
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Pre-asymptotic Transport Upscaling in Inertial and Unsteady Flows Through Porous Media

机译:通过多孔介质的惯性和非恒定流中的渐近前运输增量

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摘要

In most classical formulations of flow and transport through porous media Reynolds numbers are assumed to be small (), meaning that the role of inertia is considered negligible. However, many examples of practical relevance exist where this is not the case and inertial effects can be important leading to changes in flow structure and even giving rise to unsteady and turbulent flows as Reynolds numbers become larger. This change in flow structure can have a profound impact on how solutes are transported through the porous medium, influencing how effective large-scale transport should be modeled. Here we simulate, using high-resolution numerical models, flow and transport through an idealized porous medium for flow conditions over a range of Reynolds numbers, including steady and unsteady flows. For all these conditions we propose and test three upscaled models for transport-an advection dispersion equation, an uncorrelated spatial model (USM) and a spatial Markov model (SMM). The USM and SMM fall into the wider and more general family of continuous time random walk models. We test these models by their ability to reproduce pre-asymptotic and asymptotic plume second centered moments and breakthrough curves. We demonstrate that for steady flows where inertial effects are strong, the spatial Markov model outperforms the other two, faithfully capturing many of the non-Fickian features of transport, while for unsteady flows the uncorrelated spatial model performs best, due to the fact that unsteadiness in the flow field dampens the role of correlation on large scale transport. We conclude that correlation must be accounted for to properly upscale transport in steady flows, while it can be neglected in unsteady flows.
机译:在大多数经典的通过多孔介质流动和传输的公式中,雷诺数被认为很小(),这意味着惯性的作用可以忽略不计。但是,存在许多实际相关的例子,但事实并非如此,惯性效应可能会导致流动结构的变化,甚至随着雷诺数变大而引起不稳定和湍流,也很重要。流动结构的这种变化会对溶质如何通过多孔介质传输产生深远的影响,影响应如何模拟大规模传输的有效方式。在这里,我们使用高分辨率数值模型模拟通过理想化多孔介质的流动和传输,以在一定范围的雷诺数范围内进行流动条件,包括稳态和非稳态流动。对于所有这些条件,我们提出并测试了三个用于输运的对流扩散方程,不相关空间模型(USM)和空间马尔可夫模型(SMM)的放大模型。 USM和SMM属于更广泛,更通用的连续时间随机游动模型系列。我们通过重现渐近前和渐近羽状第二中心矩和突破曲线的能力来测试这些模型。我们证明,对于惯性效应很强的稳定流,空间马尔可夫模型的性能优于其他两个模型,如实地捕获了运输的许多非菲克式特征,而对于不稳定流,由于不稳定性,不相关的空间模型表现最佳在流场中,它减弱了相关性在大规模运输中的作用。我们得出结论,必须考虑相关性,才能在稳定流量中适当地进行高端运输,而在不稳定流量中可以忽略不计。

著录项

  • 来源
    《Transport in Porous Media》 |2015年第2期|411-432|共22页
  • 作者单位

    Univ Notre Dame, Dept Civil & Environm Engn & Earth Sci, Notre Dame, IN 46556 USA;

    Univ Notre Dame, Dept Civil & Environm Engn & Earth Sci, Notre Dame, IN 46556 USA;

    Univ Texas Austin, Inst Computat Engn & Sci, Austin, TX 78712 USA;

    Univ Texas Austin, Inst Computat Engn & Sci, Austin, TX 78712 USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Dispersion; Random walk; Inertia; Nonlocal;

    机译:分散;随机行走;惯性;非局部;

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