Convection in a porous medium with internal heat source and variable gravity effects

DOI10.1016/0020-7225(90)90052-KzbMath0718.76102OpenAlexW2048193715MaRDI QIDQ2639733

Salvatore Rionero, Brian Straughan

Publication date: 1990

Published in: International Journal of Engineering Science (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/0020-7225(90)90052-k

zbMATH Keywords

gravitational fieldexchange of stabilitiesnonlinear energy stabilityfluid saturated porous layer

Mathematics Subject Classification ID

Absolute and convective instability and stability in hydrodynamic stability (76E15) Flows in porous media; filtration; seepage (76S05) Free convection (76R10)

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Thermal convection in an inclined porous layer with Brinkman law, Nonlinear thermal instability in a horizontal porous layer with an internal heat source and mass flow, Nonlinear stability analysis of double diffusive convection in a fluid saturated porous layer with variable gravity and throughflow, Double-diffusive convection in an inclined porous layer with a concentration-based internal heat source, Resonant penetrative convection with an internal heat source/sink, Linear and weakly nonlinear analysis of a ferrofluid layer for an LTNE model with variable gravity and internal heat source, Effects of spatially varying gravity, temperature and concentration fields on the stability of a chemically reacting fluid layer, Chaotic convection in a viscoelastic fluid saturated porous medium with a heat source, Linear and nonlinear thermosolutal instabilities in an inclined porous layer, Energy methods for nonlinear stability in convection problems primarily related to geophysics, Onset of convection in a porous medium with internal heat source and variable gravity, The onset of convection in a magnetic nanofluid layer with variable gravity effects, Penetrative convection in fluid layers with internal heat sources, Effect of thermal non-equilibrium and internal heat source on Brinkman-Bénard convection, Linear and global stability analyses on the influences of thermal non-equilibrium and non-uniform gravity field on Darcy-Brinkman-Bénard convection

Cites Work

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