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Melting in a side heated tall enclosure by a uniformly dissipating heat source

机译:通过均匀散发的热源在侧面加热的高矮外壳中融化

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Melting of an organic phase change material (PCM) n-triacontane (C_30H_62) in a side heated tall enclosure of aspect ratio l0, by a uniformly dissipating heat source has been studied computationally and experimentally. Whi1e heat transfer data for melting in enclosures under isothermal wall boundary condition are available in the literature, other boundary conditions, such as constant heat flux often arise in applications of PCM for transient thermal management of electronics. An implicit enthalpy--porosity approach was utilized for computational modeling of the melting process. Experimental visualization of melt front locations was performed. Comparisons between experimental and computational heat transfer data and me1t interface locations were good. Fluid flow and heat transfer characteristics during melting suggested that natural convection plays a dominant role during initial stages of melting. At later times, the strength of natural convection diminishes as melting is completed. Correlations of heat transfer rate and melt fraction with time were obtained.
机译:计算和实验研究了通过均匀散热的方法在侧面加热的长宽比为10的高围墙中熔融有机相变材料(PCM)正三烷(C_30H_62)。文献中提供了在等温壁边界条件下在外壳中熔化的传热数据,其他边界条件(例如恒定热通量)在PCM用于电子瞬态热管理的应用中经常出现。隐式焓-孔隙率方法被用于熔融过程的计算模型。进行了熔体前沿位置的实验可视化。实验和计算传热数据以及介面界面位置之间的比较很好。熔融过程中的流体流动和传热特性表明,自然对流在熔融初期起主要作用。在以后的时间,自然对流的强度随着熔化的完成而降低。得到了传热速率和熔体分数与时间的关系。

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