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Numerical modeling of heat exchange and unsaturated-saturated flow in porous media

机译:多孔介质中热交换和非饱和饱和流动的数值模拟

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We discuss the numerical modeling of heat and mass transport in unsaturated-saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. (C) 2018 Elsevier Ltd. All rights reserved.
机译:我们讨论了不饱和饱和多孔介质中传热和传质的数值模型。热量通过渗透在毛细管和重力作用下的渗透水进行传输。热能由渗透水和多孔介质基质之间的分子扩散,对流,分散和交换控制。考虑具有边界条件的不饱和饱和流,该边界条件反映了外部驱动力。提出的数学模型是通过对立面的湿热隔离特性进行分析得出的。主要贡献在于确定模型参数,包括土壤参数,弥散系数,热传递系数,多孔介质基质的导热系数和外部传递系数。所使用的数学模型不包括由于汽化和冷凝而引起的蒸汽传输及其与水的相交换。这将是我们研究的下一步。因此,我们模型的实际应用受到限制。所开发的数值方法是解决相应逆问题的理想选择。数值实验支持我们的方法。 (C)2018 Elsevier Ltd.保留所有权利。

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