Influence of natural convection on the melting of ice block surrounded by water on all sides

The ice block at initial temperature T is = 0 °C is fixed at the center of a long, prismatic enclosure with isothermal vertical walls and insulated horizontal walls. The enclosure is completely filled with water at initial temperature T il = 0 °C. Six numerical simulations were performed by varying...

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Published inInternational journal of heat and mass transfer Vol. 49; no. 21; pp. 4106 - 4115
Main Authors Virag, Zdravko, Živić, Marija, Galović, Antun
Format Journal Article
LanguageEnglish
Published Oxford Elsevier Ltd 01.10.2006
Elsevier
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Summary:The ice block at initial temperature T is = 0 °C is fixed at the center of a long, prismatic enclosure with isothermal vertical walls and insulated horizontal walls. The enclosure is completely filled with water at initial temperature T il = 0 °C. Six numerical simulations were performed by varying vertical wall temperatures from T W = 2 to 12 °C (range of Rayleigh number from 4.22 × 10 6 to 2.28 × 10 7). In the case of T W > 8 °C the ice melts faster from above and for T W < 8 °C from below. In the case of T W = 8 °C, two vortices are separated by nearly vertical 4 °C isotherm and the average Nusselt number remains constant during the convection dominated regime.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:0017-9310
1879-2189
DOI:10.1016/j.ijheatmasstransfer.2006.04.007