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Upscaling transport with mass transfer models: Mean behavior and propagation of uncertainty

机译:传质模型提升运输:平均行为和不确定性传播

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摘要

The choice of an adequate large-scale conceptual transport model constitutes a major challenge associated with the upscaling of solute transport. Among the different alternatives to the classical advection-dispersion model, the (multirate) mass transfer model has been proposed as a valuable and convenient alternative to model the large-scale behavior of solute transport. This paper evaluates the use of mass transfer models as a constitutive equation for upscaling solute transport. To achieve this, we compare Monte Carlo simulations of solute transport at two different support scales. Transport simulations performed at the smallest scale represent a set of reference transport solutions described at a high resolution, which are contrasted against transport simulations obtained using an upscaled model (low resolution). Several formulations of the multirate mass transfer model, which differ in the type of memory function (single rate, double rate, and truncated power law), are used as a constitutive transport equation. The large-scale scenario represents a simplified model obtained by partially homogenizing the reference solution. Results show that the double-rate and the truncated power law mass transfer models are capable of properly describing the ensemble average behavior of the main features associated with the integrated breakthrough curves. However, the uncertainty associated with the upscaled mass transfer models was substantially smaller than that attributed to the reference solution. Importantly, the cumulative distribution function of concentrations associated with the upscaled model follows a distribution similar to the reference solution but with smaller statistical dispersion. The reason is that while appropriate memory functions can be used to preserve the residence time distribution of mass particles during upscaling, the lack of memory in space prevents the model from reproducing mass fluxes in all directions. Specifically, the reproduction of mass fluxes taking place at the interface between two homogenized blocks of the upscaled model is not satisfied, thus providing a poor description of the spatial distribution of mass particles in a given realization.
机译:选择适当的大规模概念性运输模型构成了与溶质运输规模扩大相关的主要挑战。在经典对流扩散模型的不同替代方案中,(多速率)传质模型已被提出为模拟溶质运移的大规模行为的一种有价值且方便的替代方案。本文评估了传质模型作为本构方程用于提高溶质迁移率的方法。为此,我们在两种不同的支持规模下比较了溶质运移的蒙特卡洛模拟。以最小规模执行的传输模拟表示以高分辨率描述的一组参考传输解决方案,这些参考传输解决方案与使用放大模型(低分辨率)获得的传输模拟形成对比。在存储函数的类型(单速率,双速率和截断幂定律)方面不同的多速率传质模型的几种公式用作本构传递方程。大规模场景表示通过部分均化参考溶液获得的简化模型。结果表明,双速率和截断幂律传质模型能够正确地描述与综合突破曲线相关的主要特征的集合平均行为。但是,与放大的传质模型相关的不确定性明显小于归因于参考解决方案的不确定性。重要的是,与放大模型相关的浓度的累积分布函数遵循与参考溶液相似的分布,但统计色散较小。原因是,虽然可以使用适当的存储功能来保留按比例放大过程中质量粒子的停留时间分布,但空间存储不足会阻止模型在所有方向上重现质量通量。具体地,不能满足在放大模型的两个均化块之间的界面处发生的质量通量的再现,因此在给定的实现中不能很好地描述质量粒子的空间分布。

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  • 来源
    《Water resources research》 |2009年第10期|W10411.1-W10411.16|共16页
  • 作者单位

    Department of Geotechnical Engineering and Geosciences, Technical University of Catalonia, E-08034 Barcelona, Spain;

    Department of Hydraulics and Environmental Engineering, Universidad Politecnica de Valencia, E-46071 Valencia, Spain;

    Department of Hydraulics and Environmental Engineering, Universidad Politecnica de Valencia, E-46071 Valencia, Spain;

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