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薄亲水纤维层堆叠中液体再分布的连续尺度建模

Continuum-Scale Modeling of Liquid Redistribution in a Stack of Thin Hydrophilic Fibrous Layers.

作者信息

Tavangarrad Amir Hossein, Mohebbi Behzad, Hassanizadeh S Majid, Rosati Rodrigo, Claussen Jan, Blümich Bernhard

机构信息

1Department of Earth Sciences, Environmental Hydrogeology Group, Utrecht University, Princetonplein 9, 3584 CC Utrecht, The Netherlands.

2Procter & Gamble Service GmbH, Sulzbacher Str. 40, 65824 Schwalbach am Taunus, Germany.

出版信息

Transp Porous Media. 2018;122(1):203-219. doi: 10.1007/s11242-018-0999-0. Epub 2018 Jan 12.

DOI:10.1007/s11242-018-0999-0
PMID:31258226
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6566212/
Abstract

Macroscale three-dimensional modeling of fluid flow in a thin porous layer under unsaturated conditions is a challenging task. One major issue is that such layers do not satisfy the representative elementary volume length-scale requirement. Recently, a new approach, called reduced continua model (RCM), has been developed to describe multiphase fluid flow in a stack of thin porous layers. In that approach, flow equations are formulated in terms of thickness-averaged variables and properties. In this work, we have performed a set of experiments, where a wet -thin porous layer was placed on top of a dry layer of the same material. We measured the change of average saturation with time using a single-sided low-field nuclear magnetic resonance device known as NMR-MOUSE. We have employed both RCM and the traditional Richards equation-based models to simulate our experimental results. We found that the traditional unsaturated flow model cannot simulate experimental results satisfactorily. Very close agreement was obtained by including the dynamic capillary term as postulated by Hassanizadeh and Gray in the traditional equations. The reduced continua model was found to be in good agreement with the experimental result without adding dynamic capillarity term. Moreover, the computational effort needed for RCM simulations was one order of magnitude less than that of traditional models.

摘要

在非饱和条件下对薄多孔层内流体流动进行宏观三维建模是一项具有挑战性的任务。一个主要问题是,这样的层不满足代表性单元体积长度尺度要求。最近,一种称为简化连续介质模型(RCM)的新方法已被开发出来,用于描述一叠薄多孔层中的多相流体流动。在该方法中,流动方程是根据厚度平均变量和性质来制定的。在这项工作中,我们进行了一组实验,将一个湿的薄多孔层放置在相同材料的干层之上。我们使用一种称为NMR-MOUSE的单侧低场核磁共振装置测量了平均饱和度随时间的变化。我们同时采用了RCM和传统的基于理查兹方程的模型来模拟我们的实验结果。我们发现传统的非饱和流动模型不能令人满意地模拟实验结果。通过在传统方程中纳入Hassanizadeh和Gray假设的动态毛细项,得到了非常接近的结果。发现简化连续介质模型在不添加动态毛细项的情况下与实验结果吻合良好。此外,RCM模拟所需的计算量比传统模型少一个数量级。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/84e02806abad/11242_2018_999_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/7f0ae3fc2965/11242_2018_999_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/4e94cd8790ed/11242_2018_999_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/4d318177aa6b/11242_2018_999_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/e9218aeeecdb/11242_2018_999_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/966128d4cb86/11242_2018_999_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/2633d71be234/11242_2018_999_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/d1835b7fe895/11242_2018_999_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/84e02806abad/11242_2018_999_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/7f0ae3fc2965/11242_2018_999_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/4e94cd8790ed/11242_2018_999_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/4d318177aa6b/11242_2018_999_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/e9218aeeecdb/11242_2018_999_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/966128d4cb86/11242_2018_999_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/2633d71be234/11242_2018_999_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/d1835b7fe895/11242_2018_999_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fa83/6566212/84e02806abad/11242_2018_999_Fig8_HTML.jpg

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