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

โœ Scribed by Ka Kheng Tan; Rex B. Thorpe

Book ID
107731118
Publisher
Elsevier Science
Year
1996
Tongue
English
Weight
737 KB
Volume
51
Category
Article
ISSN
0009-2509

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๐Ÿ“œ SIMILAR VOLUMES

The onset of convection driven by buoyan
The onset of convection driven by buoyancy effects caused by various modes of transient heat conduction: Part I. Transient Rayleigh numbers
โœ Ka Kheng Tan; Rex B Thorpe ๐Ÿ“‚ Article ๐Ÿ“… 1999 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 240 KB

The onset of convection induced by transient heat conduction in deep fluid is examined for two boundary conditions, namely: fixed surface temperature (FST) and linear rate of change of surface temperature with respect to time (LTR). Transient Rayleigh numbers (Ra) for these boundary conditions are d

The onset of convection driven by buoyan
The onset of convection driven by buoyancy caused by various modes of transient heat conduction: Part II. The sizes of plumes
โœ Ka Kheng Tan; Rex B. Thorpe ๐Ÿ“‚ Article ๐Ÿ“… 1999 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 110 KB

A theory of formation of transient thermals or plumes generated by unsteady-state heat conduction is proposed. Rising or falling mushroom-shaped plumes formed during transient heating or cooling, respectively, originate from the extending thermal boundary layers. The sizes of the hemispherical caps