Stability of buoyancy-driven convection in an Oldroyd-B fluid-saturated anisotropic porous layer

DOI10.1007/s10483-018-2329-6zbMath1392.76088OpenAlexW2789615006WikidataQ130122749 ScholiaQ130122749MaRDI QIDQ725126

I. S. Shivakumara, K. R. Raghunatha, Sowbhagya

Publication date: 1 August 2018

Published in: AMM. Applied Mathematics and Mechanics. (English Edition) (Search for Journal in Brave)

Full work available at URL: http://eprints-bangaloreuniversity.in/9056/1/raghunath.pdf

zbMATH Keywords

porous mediumconvectionOldroyd-B fluidcubic Landau equation

Mathematics Subject Classification ID

Flows in porous media; filtration; seepage (76S05) Viscoelastic fluids (76A10) Convection in hydrodynamic stability (76E06)

Related Items (3)

Intricacies of coupled molecular diffusion on double diffusive viscoelastic porous convection ⋮ An investigation of heat transfer and magnetohydrodynamics flow of fractional Oldroyd-B nanofluid suspended with carbon nanotubes ⋮ Cattaneo-LTNE effects on the stability of Brinkman convection in an anisotropic porous layer

Cites Work

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• Convection in Porous Media
• Finite amplitude cellular convection
• Oscillatory convection in a viscoelastic fluid through a porous layer heated from below
• Nonlinear thermal convection in anisotropic porous media
• Effect of modulation on the onset of thermal convection

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