Scholars@Duke publication: NATURAL CONVECTION NEAR 4 degree C IN A WATER SATURATED POROUS LAYER HEATED FROM BELOW.

NATURAL CONVECTION NEAR 4 degree C IN A WATER SATURATED POROUS LAYER HEATED FROM BELOW.

Publication , Journal Article

Blake, KR; Bejan, A; Poulikakos, D

Published in: International Journal of Heat and Mass Transfer

1984

The objective of the present study was to document numerically the characteristics of natural circulation in a porous layer heated from below, and in this way to verify the linear stability predictions regarding the onset of convection. Another objective of this study was to illustrate the high Rayleigh number characteristics of the phenomenon, i. e. the circulation pattern at Rayleigh numbers higher than critical.

Duke Scholars

Author Adrian Bejan Thomas Lord Department of Mechanical Engineering and Materia ...

Published In

International Journal of Heat and Mass Transfer

Publication Date

1984

Volume

Issue

Start / End Page

2355 / 2364

Related Subject Headings

Mechanical Engineering & Transports
09 Engineering
02 Physical Sciences
01 Mathematical Sciences

Citation

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MLA

NLM

Blake, K. R., Bejan, A., & Poulikakos, D. (1984). NATURAL CONVECTION NEAR 4 degree C IN A WATER SATURATED POROUS LAYER HEATED FROM BELOW. International Journal of Heat and Mass Transfer, 27(2), 2355–2364.

Blake, Kenneth R., Adrian Bejan, and Dimos Poulikakos. “NATURAL CONVECTION NEAR 4 degree C IN A WATER SATURATED POROUS LAYER HEATED FROM BELOW.” International Journal of Heat and Mass Transfer 27, no. 2 (1984): 2355–64.

Blake KR, Bejan A, Poulikakos D. NATURAL CONVECTION NEAR 4 degree C IN A WATER SATURATED POROUS LAYER HEATED FROM BELOW. International Journal of Heat and Mass Transfer. 1984;27(2):2355–64.

Blake, Kenneth R., et al. “NATURAL CONVECTION NEAR 4 degree C IN A WATER SATURATED POROUS LAYER HEATED FROM BELOW.” International Journal of Heat and Mass Transfer, vol. 27, no. 2, 1984, pp. 2355–64.

Blake KR, Bejan A, Poulikakos D. NATURAL CONVECTION NEAR 4 degree C IN A WATER SATURATED POROUS LAYER HEATED FROM BELOW. International Journal of Heat and Mass Transfer. 1984;27(2):2355–2364.