Surface-tension-driven convection in a fluid overlying a porous layer.

DOI10.1006/JCPH.2001.6739zbMath1039.76052OpenAlexW2091170377MaRDI QIDQ5943991

Brian Straughan

Publication date: 2001

Published in: Journal of Computational Physics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1006/jcph.2001.6739

zbMATH Keywords

Marangoni effectChebyshev tau methodmultilayer convection

Mathematics Subject Classification ID

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

Related Items (9)

Instability of plane Poiseuille flow in a fluid-porous system ⋮ Transitions and bifurcations of Darcy-Brinkman-Marangoni convection ⋮ Double-diffusive convection induced by selective absorption of radiation in a fluid overlying a porous layer ⋮ Onset of surface tension driven convection in a fluid layer overlying a layer of an anisotropic porous medium ⋮ Marangoni mixed convection boundary layer flow ⋮ Stability of convection induced by selective absorption of radiation in a fluid overlying a porous layer ⋮ Thermal convection in superposed fluid and porous layers subjected to a horizontal plane Couette flow ⋮ Thermal convection in superposed fluid and porous layers subjected to a plane Poiseuille flow ⋮ A Comparative Study of Nonlinear Convection in a Confined Fluid Overlying a Porous Layer

Cites Work

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• Buoyancy-surface tension instability by the method of energy
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