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首页> 外文期刊>Numerical Heat Transfer, Part B. Fundamentals: An International Journal of Computation and Methodology >Numerical simulation of coupled heat and mass transfer in hygroscopic porous materials considering the influence of atmospheric pressure
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Numerical simulation of coupled heat and mass transfer in hygroscopic porous materials considering the influence of atmospheric pressure

机译:考虑大气压影响的吸湿多孔材料传热传质耦合数值模拟

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摘要

A model of simultaneous transport in hygroscopic porous materials was developed. Water in fabrics is considered to be present in three forms: liquid water in the void space between fibers, bound water in the fibers, and vapor. It is assumed that the heat and mass transport mechanisms include movement of liquid water due to the capillarity and atmospheric pressure gradient, diffusion of vapor within interfibers due to the partial pressure gradient of vapor and total gas pressure gradient, diffusion of vapor into fiber, evaporation, and condensation of water. The moisture diffusion process into hygroscopic porous materials such as wool fabrics was simulated. At normal atmospheric pressure, the results were compared with experimental data on the temperature and water content changes reported in the literature. The distribution of temperature, moisture concentration, liquid water saturation, and atmospheric pressure in the void space between fibers at different boundary conditions are numerically computed and compared. The conclusion is that atmospheric pressure gradient has significant impact on heat and mass transport processes in hygroscopic porous materials.
机译:建立了在吸湿性多孔材料中同时运输的模型。织物中的水被认为以三种形式存在:纤维之间的空隙中的液态水,纤维中的结合水以及蒸汽。假设传热和传质机理包括:由于毛细作用和大气压梯度而引起的液态水运动;由于蒸汽的分压梯度和总气体压力梯度而引起的蒸汽在纤维间的扩散;蒸汽向纤维中的扩散;蒸发。以及水的凝结。模拟了水分在吸湿性多孔材料(如羊毛织物)中的扩散过程。在正常大气压下,将结果与文献中报道的有关温度和水含量变化的实验数据进行比较。计算并比较了在不同边界条件下纤维之间的空隙空间中的温度,水分浓度,液态水饱和度和大气压力的分布。结论是,大气压梯度对吸湿性多孔材料的传热和传质过程具有重要影响。

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