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HEAT SOURCES IN A POROUS MEDIUM

机译:多孔介质中的热源

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Porous materials are usually treated as homogeneous substances in which the classical differential Fourier equation can be applied for the description of heat transfer processes. However, this approach can lead to substantial errors due to mass transport processes that in such media occur simultaneously with heat conduction. The mass transport consists mainly in the flow of gas or liquid through pores, vapor absorption and condensation in capillaries, diffusion of water vapor present in the air or of other gases the fill the pores. These mass transport processes generate heat sources which have been shown [1, 2, 3 ] to significantly distort temperature fields in porous media. In the present paper, equation will be derived that determine heat source densities associated with various mass transport processes. Next, effect of the processes on temperature fields will be estimated and a generalized equation formulated for the case of heat transfer in a porous medium.
机译:多孔材料通常被视为均匀物质,其中可以应用典型差动傅里叶方程用于传热过程的描述。 然而,这种方法可能导致由于大规模运输过程而导致具有热传导同时发生的大规模运输过程。 大通传输主要由气体或液体流过孔隙,蒸气吸收和胶凝中的凝结在毛细血管中,水蒸气的扩散存在于空气中或其他气体填充孔。 这些质量传输过程产生了已经示出的热源,其已经显示为[1,2,3],以显着扭曲多孔介质中的温度场。 在本文中,将导出方程,以确定与各种大规模运输过程相关的热源密度。 接下来,将估计温度场对温度场的效果,并且为多孔介质中的传热情况配制的广义方程。

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