2015
DOI: 10.1016/j.applthermaleng.2015.06.098
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Experimental study on frost formation on a cold surface in low atmospheric pressure

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Cited by 27 publications
(3 citation statements)
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“…The results are In addition, as shown in Figure 2, the only condensation phenomenon (C→D) occurred on the cold surface under ideal condition, when the partial pressure P v of water vapor is greater than the triple point pressure P tp (P v > P tp ) and the cold surface temperature T cs was higher than the triple point temperature T tp but lower than the wet air dew point T dp (T tp < T cs < T dp ) [55]. Meanwhile, we can also see from Figure 2 that there are three kinds of different pathways to form frost layer, and that is gas-liquid-solid process (C 1 →D 1 ), gas-solid process (C 2 →D 2 ) and occurring simultaneously (C 1 →D 1 and C 2 →D 2 ) [22,55]. The results provided by Xu [56] also confirmed it.…”
Section: Figurementioning
confidence: 90%
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“…The results are In addition, as shown in Figure 2, the only condensation phenomenon (C→D) occurred on the cold surface under ideal condition, when the partial pressure P v of water vapor is greater than the triple point pressure P tp (P v > P tp ) and the cold surface temperature T cs was higher than the triple point temperature T tp but lower than the wet air dew point T dp (T tp < T cs < T dp ) [55]. Meanwhile, we can also see from Figure 2 that there are three kinds of different pathways to form frost layer, and that is gas-liquid-solid process (C 1 →D 1 ), gas-solid process (C 2 →D 2 ) and occurring simultaneously (C 1 →D 1 and C 2 →D 2 ) [22,55]. The results provided by Xu [56] also confirmed it.…”
Section: Figurementioning
confidence: 90%
“…Kwak and Bai [19] found that the heating capacity and COP of the system increased significantly by In addition, from the viewpoint of phase change kinetics, the phase change driving force leads to the freezing of the water droplets [61]. Chen et al [22] showed that a smaller phase change driving force will be obtained if the partial pressure of water vapor or atmospheric pressure decreases under keeping other conditions constant. This will contribute to keeping the cooling state of ambient air and the supercooling state of the water droplets without being frozen.…”
Section: Parameters Describing Frosting Mapmentioning
confidence: 99%
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