The effect of surface wettability on frost melting

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

Frost melting on a vertical surface is divided into three stages: absorption, accumulation and draining, and the effect of surface wettability on melting is investigated analytically. The ratio of the volume flux of water to the melting rate is the key factor that determines meltwater motion. In the absorption stage, the ratio is greater than unity with meltwater is absorbed into the frost layer by capillary force. The volume flux of water depends on porosity and permeability of the frost layer, which are affected by the surface wettability. When the frost layer is saturated, meltwater accumulates on the surface, and the retention water is related to surface wettability. In the draining stage, meltwater flows along the surface, and the draining velocity depends on boundary conditions at the interfaces. Draining velocity increases on hydrophobic surfaces compared to that on hydrophilic surfaces owning to the presence of a slip velocity.

Original languageEnglish (US)
Pages (from-to)25-33
Number of pages9
JournalInternational Journal of Heat and Mass Transfer
Volume127
DOIs
StatePublished - Dec 1 2018

Fingerprint

frost
wettability
Wetting
Melting
melting
drainage
Water
water
Fluxes
unity
permeability
slip
Porosity
Boundary conditions
boundary conditions
porosity

Keywords

  • Draining velocity
  • Frost melting
  • Meltwater motion
  • Surface wettability
  • Volume flux of water

Cite this

The effect of surface wettability on frost melting. / Liu, Y.; Kulacki, Francis A.

In: International Journal of Heat and Mass Transfer, Vol. 127, 01.12.2018, p. 25-33.

Research output: Contribution to journalArticle

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abstract = "Frost melting on a vertical surface is divided into three stages: absorption, accumulation and draining, and the effect of surface wettability on melting is investigated analytically. The ratio of the volume flux of water to the melting rate is the key factor that determines meltwater motion. In the absorption stage, the ratio is greater than unity with meltwater is absorbed into the frost layer by capillary force. The volume flux of water depends on porosity and permeability of the frost layer, which are affected by the surface wettability. When the frost layer is saturated, meltwater accumulates on the surface, and the retention water is related to surface wettability. In the draining stage, meltwater flows along the surface, and the draining velocity depends on boundary conditions at the interfaces. Draining velocity increases on hydrophobic surfaces compared to that on hydrophilic surfaces owning to the presence of a slip velocity.",
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AB - Frost melting on a vertical surface is divided into three stages: absorption, accumulation and draining, and the effect of surface wettability on melting is investigated analytically. The ratio of the volume flux of water to the melting rate is the key factor that determines meltwater motion. In the absorption stage, the ratio is greater than unity with meltwater is absorbed into the frost layer by capillary force. The volume flux of water depends on porosity and permeability of the frost layer, which are affected by the surface wettability. When the frost layer is saturated, meltwater accumulates on the surface, and the retention water is related to surface wettability. In the draining stage, meltwater flows along the surface, and the draining velocity depends on boundary conditions at the interfaces. Draining velocity increases on hydrophobic surfaces compared to that on hydrophilic surfaces owning to the presence of a slip velocity.

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