The onset of convection caused by buoyancy during transient heat conduction in deep fluids

The onset of convection in a thermal layer generated by transient heat conduction in deep fluid is examined. It is generally accepted that buoyancy driven convection predominates in deep fluids while surface tension driven convection can occur only in very thin layers of liquid. The occurrence of bu...

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Main Authors: Tan, Ka Kheng, Thorpe, Rex B.
Format: Article
Language:English
English
Published: Elsevier Science 1996
Online Access:http://psasir.upm.edu.my/id/eprint/42489/
http://psasir.upm.edu.my/id/eprint/42489/1/The%20onset%20of%20convection%20caused%20by%20buoyancy%20during%20transient%20heat%20conduction%20in%20deep%20fluids.pdf
http://psasir.upm.edu.my/id/eprint/42489/7/1-s2.0-0009250996002552-main.pdf
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author Tan, Ka Kheng
Thorpe, Rex B.
author_facet Tan, Ka Kheng
Thorpe, Rex B.
author_sort Tan, Ka Kheng
building UPM Institutional Repository
collection Online Access
description The onset of convection in a thermal layer generated by transient heat conduction in deep fluid is examined. It is generally accepted that buoyancy driven convection predominates in deep fluids while surface tension driven convection can occur only in very thin layers of liquid. The occurrence of buoyancy convection can be predicted from conventional linear stability analysis for steady-state heat conduction. Its results are summarised in terms of critical Rayleigh numbers. The point of instability in transient heat conduction is, however, less well understood. Its onset in deep fluids is determined by the mode and rate of cooling. In this paper, the judicial application of transient heat conduction equations and a newly defined transient local Ra with the appropriate boundary conditions has allowed the tracking of the time and spatial development of local hydrodynamic equilibrium to the point of instability. The onset of convection can be predicted from the maximum transient Ra whose values are the same as those previously obtained by linear stability analysis for the same boundary conditions. The critical times and critical depths for stable diffusion in fluids (i.e. without convection) can thus be determined accurately. Agreement with observed values from the literature is very good. The mode and rate of heat conduction are confirmed to be the controlling factors in determining the time of onset of convection.
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publishDate 1996
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spelling upm-424892024-09-25T07:06:52Z http://psasir.upm.edu.my/id/eprint/42489/ The onset of convection caused by buoyancy during transient heat conduction in deep fluids Tan, Ka Kheng Thorpe, Rex B. The onset of convection in a thermal layer generated by transient heat conduction in deep fluid is examined. It is generally accepted that buoyancy driven convection predominates in deep fluids while surface tension driven convection can occur only in very thin layers of liquid. The occurrence of buoyancy convection can be predicted from conventional linear stability analysis for steady-state heat conduction. Its results are summarised in terms of critical Rayleigh numbers. The point of instability in transient heat conduction is, however, less well understood. Its onset in deep fluids is determined by the mode and rate of cooling. In this paper, the judicial application of transient heat conduction equations and a newly defined transient local Ra with the appropriate boundary conditions has allowed the tracking of the time and spatial development of local hydrodynamic equilibrium to the point of instability. The onset of convection can be predicted from the maximum transient Ra whose values are the same as those previously obtained by linear stability analysis for the same boundary conditions. The critical times and critical depths for stable diffusion in fluids (i.e. without convection) can thus be determined accurately. Agreement with observed values from the literature is very good. The mode and rate of heat conduction are confirmed to be the controlling factors in determining the time of onset of convection. Elsevier Science 1996-09 Article PeerReviewed text en http://psasir.upm.edu.my/id/eprint/42489/1/The%20onset%20of%20convection%20caused%20by%20buoyancy%20during%20transient%20heat%20conduction%20in%20deep%20fluids.pdf text en http://psasir.upm.edu.my/id/eprint/42489/7/1-s2.0-0009250996002552-main.pdf Tan, Ka Kheng and Thorpe, Rex B. (1996) The onset of convection caused by buoyancy during transient heat conduction in deep fluids. Chemical Engineering Science, 51 (17). pp. 4127-4136. ISSN 0009-2509; ESSN: 1873-4405 http://www.sciencedirect.com/science/article/pii/0009250996002552 10.1016/0009-2509(96)00255-2
spellingShingle Tan, Ka Kheng
Thorpe, Rex B.
The onset of convection caused by buoyancy during transient heat conduction in deep fluids
title The onset of convection caused by buoyancy during transient heat conduction in deep fluids
title_full The onset of convection caused by buoyancy during transient heat conduction in deep fluids
title_fullStr The onset of convection caused by buoyancy during transient heat conduction in deep fluids
title_full_unstemmed The onset of convection caused by buoyancy during transient heat conduction in deep fluids
title_short The onset of convection caused by buoyancy during transient heat conduction in deep fluids
title_sort onset of convection caused by buoyancy during transient heat conduction in deep fluids
url http://psasir.upm.edu.my/id/eprint/42489/
http://psasir.upm.edu.my/id/eprint/42489/
http://psasir.upm.edu.my/id/eprint/42489/
http://psasir.upm.edu.my/id/eprint/42489/1/The%20onset%20of%20convection%20caused%20by%20buoyancy%20during%20transient%20heat%20conduction%20in%20deep%20fluids.pdf
http://psasir.upm.edu.my/id/eprint/42489/7/1-s2.0-0009250996002552-main.pdf