Hostname: page-component-848d4c4894-nmvwc Total loading time: 0 Render date: 2024-07-08T01:52:32.043Z Has data issue: false hasContentIssue false

Three-dimensional convection in a cubic box of fluid-saturated porous material

Published online by Cambridge University Press:  19 April 2006

Joe M. Straus
Affiliation:
Space Sciences Laboratory, The Ivan A. Getting Laboratories, The Aerospace Corporation, Los Angeles, California 90009
Gerald Schubert
Affiliation:
Space Sciences Laboratory, The Ivan A. Getting Laboratories, The Aerospace Corporation, Los Angeles, California 90009 Permanent address: Department of Earth and Space Sciences, University of California, Los Angeles, California 90024.

Abstract

Calculations of finite amplitude convection in cubic boxes containing fluid-saturated porous material are reported for Rayleigh numbers R as large as 150. Steady two- or three-dimensional convection can always be forced by appropriate choice of initial conditions. Randomly chosen initial conditions will result in either two- or three-dimensional convection. Although there is a non-uniqueness associated with initial conditions which makes possible either two- or three-dimensional convection, the non-uniqueness is limited in the sense that only one two-dimensional or one three-dimensional solution appears to be realizable. Two-dimensional flows have larger Nusselt numbers than three-dimensional flows for R [lsim ] 97; the opposite is true for R [gsim ] 97.

Type
Research Article
Copyright
© 1979 Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Beck, J. L. 1972 Convection in a box of porous material saturated with fluid. Phys. Fluids 15, 1377.Google Scholar
Holst, P. H. & Aziz, K. 1972 Transient three-dimensional natural convection in confined porous media. Int. J. Heat Mass Transfer 15, 73.Google Scholar
Horne, R. N. 1978 Three-dimensional natural convection in a confined porous medium heated from below. A.I.A.A./A.S.M.E. Thermophys. Heat Transfer Conf.
Malkus, W. V. R. 1954 The heat transport and spectrum of thermal turbulence. Proc. Roy. Soc. A 225, 196.Google Scholar
Platzman, G. W. 1965 The spectral dynamics of laminar convection. J. Fluid Mech. 23, 481.Google Scholar
Straus, J. M. 1974 Large amplitude convection in porous media. J. Fluid Mech. 64, 51.Google Scholar
Straus, J. M. & Schubert, G. 1978 On the existence of three-dimensional convection in a rectangular box of fluid-saturated porous material. J. Fluid Mech. 87, 385.Google Scholar
Zebib, A. & Kassoy, D. R. 1978 Three-dimensional natural convection motion in a confined porous medium. Phys. Fluids 21, 1.Google Scholar