Onset of convection in a couple-stress fluid-saturated porous medium: effects of non-uniform temperature gradients

DOI10.1007/s00419-009-0347-5zbMath1271.76092OpenAlexW1989752011MaRDI QIDQ363158

I. S. Shivakumara

Publication date: 30 August 2013

Published in: Archive of Applied Mechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1007/s00419-009-0347-5

zbMATH Keywords

porous mediumconvectioncouple-stress fluidnon-uniform temperature gradient

Mathematics Subject Classification ID

Related Items (7)

Coriolis effect on thermal convection in a couple-stress fluid-saturated rotating rigid porous layer ⋮ Linear and nonlinear stability of double diffusive convection in a couple stress fluid-saturated porous layer ⋮ Effects of spatially varying gravity, temperature and concentration fields on the stability of a chemically reacting fluid layer ⋮ Plane waves and fundamental solution in a couple stress generalized thermoelastic solid ⋮ Transitions and bifurcations in couple stress fluid saturated porous media using a thermal non-equilibrium model ⋮ On the stability of penetrative convection in a couple-stress fluid ⋮ The well-posedness and the regularity of global attractor for a couple stress fluid through porous layer with the local thermal non-equilibrium effect

Cites Work

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• The Brinkman model for natural convection in a porous layer: Effects of nonuniform thermal gradient
• The onset of transient convective instability
• Convection in Porous Media
• Handbook of Porous Media
• Thermally Developing Forced Convection in a Porous Medium: Parallel-Plate Channel or Circular Tube with Isothermal Walls

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