Abstract
The work in this paper concerns the one-dimensional melting of a finite thickness layer. An asymptotic series solution describes the temperature in the melt regions. In the solid region the thermal boundary layers are approximated by a cubic polynomial. Results are compared with the exact solution for a semi-infinite block, and shown to agree to within less than 1%. The method is then applied to a situation where no analytical solution is available. A finite thickness frozen solid is placed on a warm substrate in a warm environment: initially the base of the solid heats to the melting temperature when a single melted region develops and subsequently a second melting front appears on the top boundary. We also present an example relevant to heating an ice layer from below, which occurs with de-icing systems.
Original language | English |
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Pages (from-to) | 5305-5317 |
Number of pages | 13 |
Journal | International Journal of Heat and Mass Transfer |
Volume | 50 |
Issue number | 25-26 |
DOIs | |
Publication status | Published - Dec 2007 |
Externally published | Yes |
Keywords
- Heat balance integral method
- Phase change