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 in | International journal of heat and mass transfer Vol. 49; no. 21; pp. 4106 - 4115 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Oxford
Elsevier Ltd
01.10.2006
Elsevier |
Subjects | |
Online Access | Get full text |
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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. |
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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 |