Effect of Brinkman boundary layer on the onset of Marangoni convection in a fluid-saturated porous layer
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Publication:1384765
DOI10.1007/BF01170376zbMath0930.76029MaRDI QIDQ1384765
Publication date: 14 February 2000
Published in: Acta Mechanica (Search for Journal in Brave)
linear stability analysismethod of matched asymptotic expansionsporosity parametersurface tension gradientssingle-term Galerkin expansionadiabatic free boundaries
Flows in porous media; filtration; seepage (76S05) Capillarity (surface tension) for incompressible viscous fluids (76D45) Convection in hydrodynamic stability (76E06)
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Brinkman-Bénard-Marangoni convection in a magnetized ferrofluid saturated porous layer, Transitions and bifurcations of Darcy-Brinkman-Marangoni convection, Onset of surface tension driven convection in a fluid layer overlying a layer of an anisotropic porous medium, Darcy-Bénard-Marangoni convection in porous media
Cites Work
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- Asymptotic analysis of natural convection through horizontal porous layer
- The method of weighted residuals and variational principles. With application in fluid mechanics, heat and mass transfer
- On convection cells induced by surface tension
- On cellular convection driven by surface-tension gradients: effects of mean surface tension and surface viscosity
- Surface tension and buoyancy effects in cellular convection