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Transient and steady natural convection from a heat source embedded in thermally stratified porous layer

Numerical results are presented for transient and steady natural convection from a heat source buried in a saturated, porous layer. The porous layer is thermally stratified with a negative temperature gradient but its corresponding Rayleigh number is not greater than that of the critical value (Ra c...

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Bibliographic Details
Published in:International journal of thermal sciences 2010-09, Vol.49 (9), p.1527-1535
Main Authors: Zhang, J., Subotic, M., Lai, F.C.
Format: Article
Language:English
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Summary:Numerical results are presented for transient and steady natural convection from a heat source buried in a saturated, porous layer. The porous layer is thermally stratified with a negative temperature gradient but its corresponding Rayleigh number is not greater than that of the critical value (Ra c = 40). The effects of the size of the heat source and its buried depth are also investigated. The results, which include the buoyancy-induced flow patterns and temperature profiles, as well as the heat transfer coefficient in terms of the Nusselt number, are presented for a wide range of Rayleigh number and stratification parameter. The results thus obtained have important implications for applications in geothermal energy and underground disposal of nuclear wastes.
ISSN:1290-0729
1778-4166
DOI:10.1016/j.ijthermalsci.2010.03.009