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Natural convection heat and moisture transfer with thermal radiation in a cavity partially filled with hygroscopic porous medium

机译:局部充满吸湿性多孔介质的空腔中的自然对流传热和水分传热

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This article deals with natural convection heat and moisture transfer with thermal radiation in a cavity partially filled with hygroscopic porous medium. The governing equations for the momentum and heat transfer in both free fluid and hygroscopic porous medium and moisture content transfer in hygroscopic porous medium were solved by the finite element method. The radiative heat transfer is calculated by making use of the radiosity of the surfaces that are assumed to be grey. Comparisons with experimental and numerical results in the literature have been carried out. Effects of thermal radiation and Rayleigh number on natural convection and heat transfer in both free fluid and porous medium and moisture content transfer in porous medium were analyzed. It was found that surface thermal radiation can significantly change the temperature and moisture content fields in the regions of free flow and porous medium. The mean temperature at the interface decreases, the temperature and moisture content gradients are created on the upper two corners of the porous medium region, and the moisture content in the porous medium decreases in the porous medium as Ra increases.
机译:本文介绍了在部分充满吸湿性多孔介质的空腔中通过自然辐射进行自然对流传热和水分传递的过程。用有限元方法求解了自由流体和吸湿性多孔介质中的动量和热传递以及吸湿性多孔介质中的水分传递的控制方程。辐射热传递是通过利用假定为灰色的表面的辐射度来计算的。与文献中的实验和数值结果进行了比较。分析了热辐射和瑞利数对自由流体和多孔介质中自然对流和传热以及多孔介质中水分传递的影响。发现表面热辐射可以显着改变自由流动和多孔介质区域中的温度和水分含量场。界面处的平均温度降低,在多孔介质区域的上两个角处形成温度和水分含量梯度,并且随着Ra的增加,多孔介质中的多孔介质中的水分含量降低。

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