1995
DOI: 10.1252/jcej.28.732
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Frost Formation Under Different Gaseous Atmospheres.

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Cited by 6 publications
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“…We proposed a set of analytical equations to quantitatively evaluate the removal rates of vapor and mist and proved them experimentally using n-butanol as condensable vapor. Afterward, we investigated another simultaneous heat and mass transfer process with water mist formation and frost formation, where natural convection is generated in a closed vessel with a cooled horizontal plate under various gaseous atmospheres relating with t,he fcu system(6) (7). Variations of the heat and mass t,ransfer rates and frost formation rates with different cooling temperatures in different atmospheres (Hz, He, Nz and CH4) were well predicted by our equations.…”
Section: Introductionmentioning
confidence: 62%
“…We proposed a set of analytical equations to quantitatively evaluate the removal rates of vapor and mist and proved them experimentally using n-butanol as condensable vapor. Afterward, we investigated another simultaneous heat and mass transfer process with water mist formation and frost formation, where natural convection is generated in a closed vessel with a cooled horizontal plate under various gaseous atmospheres relating with t,he fcu system(6) (7). Variations of the heat and mass t,ransfer rates and frost formation rates with different cooling temperatures in different atmospheres (Hz, He, Nz and CH4) were well predicted by our equations.…”
Section: Introductionmentioning
confidence: 62%