Abstract
Numerical and experimental investigations of melting of ice in a three-dimensional cubical object are presented. The ice, initially at a temperature well below its freezing point, is subjected to a temperature higher than its melting point at a part of its top surface. Other boundaries are subjected to natural convection with the surroundings. A liquid phase starts to form in the solid near the region in contact with the hot surface. Experimental results under different boundary conditions show a fast melting rate in the initial period of melting and then a slower rate of melting. Heat losses from the walls of the ice box have a strong effect on the time required for the ice to melt. Results of a simplified numerical model show good agreement with the experimental results.
| Original language | English |
|---|---|
| Journal | International Symposium on Advances in Computational Heat Transfer |
| DOIs | |
| State | Published - 1997 |
Bibliographical note
Publisher Copyright:© 1997, Begell House Inc. All rights reserved.
ASJC Scopus subject areas
- Fluid Flow and Transfer Processes
- Mechanical Engineering
- Condensed Matter Physics
- Computer Science Applications
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