将扩展的异质斯特凡问题从孔隙尺度放大到永久冻土的达西尺度

Malgorzata Peszynska, Naren Vohra, Lisa Bigler
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引用次数: 0

摘要

多尺度建模与仿真》,第 22 卷第 1 期,第 436-475 页,2024 年 3 月。 摘要本文将热模型从孔隙尺度提升到达西尺度,以应用于永久冻土。我们在孔隙尺度上加入了水的融化和冻结,并将[A. Visintin, SIAM J. Math. Anal., 39 (2007), pp.为了使有效模型与已知的达西尺度经验模型保持一致,我们重新审视并扩展了孔隙尺度模型,以包括小孔隙中微观尺度的物理特性。我们还为非线性有效电导率提出了一个实用的简化模型。我们通过模拟进行了说明。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Upscaling an Extended Heterogeneous Stefan Problem from the Pore-Scale to the Darcy Scale in Permafrost
Multiscale Modeling &Simulation, Volume 22, Issue 1, Page 436-475, March 2024.
Abstract. In this paper we upscale thermal models from the pore–scale to the Darcy scale for applications in permafrost. We incorporate thawing and freezing of water at the pore-scale and adapt rigorous homogenization theory from [A. Visintin, SIAM J. Math. Anal., 39 (2007), pp. 987–1017] to the original nonlinear multivalued relationship to derive the effective properties. To obtain agreement of the effective model with the known Darcy scale empirical models, we revisit and extend the pore-scale model to include the delicate microscale physics in small pores. We also propose a practical reduced model for the nonlinear effective conductivity. We illustrate with simulations.
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