Unicellular natural circulation in a shallow horizontal porous layer heated from below by a constant flux

DOI10.1017/S0022112095002874zbMath0854.76086OpenAlexW2134203875MaRDI QIDQ4873004

Shigeo Kimura, Farid Alavyoon, Michael Vynnycky

Publication date: 19 January 1997

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1017/s0022112095002874

zbMATH Keywords

analytical solutionslinear stabilityaspect ratiofinite supercritical Rayleigh number

Mathematics Subject Classification ID

Flows in porous media; filtration; seepage (76S05) Free convection (76R10)

Related Items (3)

Onset of gravitactic bioconvection in a square anisotropic porous medium with arbitrary orientation of the principal axes ⋮ Bistability and hysteresis induced by form drag in nonlinear subcritical and supercritical double-diffusive Lapwood convection in shallow porous enclosures ⋮ Thermoconvective instabilities in an inclined porous channel heated from below

Cites Work

• Convection in a porous medium with inclined temperature gradient
• Onset of convection in a vertical slab of saturated porous media between two impermeable conducting blocks
• Multiple steady states for unicellular natural convection in an inclined porous layer
• Computation of steady and oscillatory convection in saturated porous media
• Convection in a porous medium with horizontal and vertical temperature gradients
• On natural convection in vertical porous enclosures due to prescribed fluxes of heat and mass at the vertical boundaries
• Natural convection in a thin, inclined, porous layer exposed to a constant heat flux
• The influence of side wall heat transfer on convection in a confined saturated porous medium

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