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Experimental dropwise condensation of unsaturated humid air - Influence of humidity level on latent and convective heat transfer for fully developed turbulent flow

机译:实验性不饱和湿空气的逐滴冷凝-湿度水平对充分发展的湍流流动的潜热和对流传热的影响

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摘要

Dropwise condensation is experimentally studied on the lower surface of a 0.03 m × 0.3 m rectangular test section. Turbulent flow develops along an isothermal horizontal 2 m-long section before single-sided condensation is initiated over a 0.1 m × 0.2 m cooled surface. The relative humidity level of unsaturated moist air is controlled by steam injection and ranges from 13% to 94%. Drop size and its distribution are followed from small droplets up to puddle formation just before the appearance of a liquid film. The latent contribution of condensation is determined from instantaneous condensed mass data. Comparison between latent and global heat flux demonstrates that drop growth has secondary effects on the condensation rate and that mass rises almost linearly for dropwise condensation. In addition, transition from droplets to large drops and puddles plays a direct role in global heat flux density and strongly influences convective heat transfer contribution.
机译:在0.03 m×0.3 m的矩形测试段的下表面进行了滴滴凝结的实验研究。在0.1 m×0.2 m冷却表面上开始单面冷凝之前,湍流沿着水平2 m长的等温线发展。不饱和湿空气的相对湿度水平通过蒸汽注入控制,范围为13%至94%。液滴大小及其分布从小液滴一直到液膜出现之前的水坑形成。冷凝的潜在贡献是根据瞬时冷凝质量数据确定的。潜热通量和总热通量之间的比较表明,液滴的生长对凝结速率具有次要影响,而对于逐滴凝结,质量几乎呈线性增加。另外,从液滴到大液滴和水坑的转变在整体热通量密度中起直接作用,并强烈影响对流传热的贡献。

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