The effect of a nonuniform basic temperature gradient on the convective instability of a fluid-saturated porous layer with general velocity and thermal conditions

DOI10.1007/BF01176809zbMath0949.76027MaRDI QIDQ1977058

R. P. Thangaraj

Publication date: 9 May 2000

Published in: Acta Mechanica (Search for Journal in Brave)

zbMATH Keywords

Rayleigh-Bénard convectionmulti-layer mediumpermeable wallssparsely packed porous mediumnonuniform basic temperature gradientsingle term Galerkin method

Mathematics Subject Classification ID

Flows in porous media; filtration; seepage (76S05) Convection in hydrodynamic stability (76E06)

Cites Work

• Unnamed Item
• Convection in a fluid-saturated porous layer with non-uniform temperature gradient
• On the Boundary Condition at the Surface of a Porous Medium
• Finite-amplitude cellular convection in a fluidsaturated porous layer
• The onset of transient convective instability

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