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对描述多孔介质中自然对流的Darcy模型的改进形式——考虑各向异性的Brinkman模型,给出了其基本方程的一些代数显式解析解,这些解析解除有重要的理论意义外(例如分析各向异性非Darcy效应对对流的影响),还可以作为标准解促进计算传热传质学的发展.
An improved version of Darcy’s model describing natural convection in porous media - a Brinkman model with anisotropy is given, and some algebraic explicit analytical solutions of its basic equations are given, which are of important theoretical significance (for example, The effect of anisotropic non-Darcy effect on convection), and can also be used as a standard solution to promote the development of computational heat and mass transfer.