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Natural convection heat transfer from a discrete heat source coupled with conduction dominated phase change

机译:来自离散热源的自然对流传热与传导主导的相变

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A numerical study has been conducted for the heat transfer from a discrete heat source by natural convection in air above coupled with conduction dominated melting of a phase change material (PCM) below via a wall of finite thermal diffusivity.Results indicate that the presence of a PCM layer underneath the wall significantly delays the temperature rise of the heat source. The time delay increases as the thermal diffusivity of the wall material decreases and as the thickness of the PCM layerincreases. For high thermal conductivity wall materials k{sub}w/k{sub}m≥ 100 the steady state heat source temperatures are similar and independent of the PCM layer. On the other hand, for k{sub}w/k{sub}m≤ 10, the steady state temperatures are higher and dependent on the thickness of the PCM layer. A correlation is proposed in terms of the thickness of the PCM layer and the thermal conductivity ratio of the wall.
机译:进行了数值研究,通过空气中自然对流通过离散热源传热,再通过有限热扩散壁通过传导主导的相变材料(PCM)熔融融化,结果表明存在壁下的PCM层显着延迟了热源的温度上升。时间延迟随着壁材料的热扩散率降低以及PCM层厚度的增加而增加。对于高导热率墙材料k {sub} w / k {sub}m≥100,稳态热源温度相似且独立于PCM层。另一方面,对于k {sub} w / k {sub}m≤10,稳态温度较高并且取决于PCM层的厚度。提出了关于PCM层的厚度和壁的导热率的相关性。

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