Onset of stationary and oscillatory convection in a tilted porous cavity saturated with a binary fluid: Linear stability analysis
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Publication:3539053
DOI10.1063/1.870000zbMath1147.76428OpenAlexW2021019870MaRDI QIDQ3539053
Abdelkader Mojtabi, Marie Catherine Charrier-Mojtabi, Mohammad Karimi-Fard
Publication date: 17 November 2008
Published in: Physics of Fluids (Search for Journal in Brave)
Full work available at URL: http://oatao.univ-toulouse.fr/20664/1/Karimi_20664.pdf
Related Items (11)
Linear and nonlinear double diffusive convection in a rotating sparsely packed porous layer using a thermal non-equilibrium model ⋮ Double‐diffusive flow in a porous right‐angle trapezoidal enclosure with constant heat flux ⋮ Double diffusive convection in a cubic enclosure with opposing temperature and concentration gradients ⋮ Free convection of binary liquid with variable Soret coefficient in thermogravitational column: The steady parallel base states ⋮ Onset of convection in anisotropic porous media subject to a rapid change in boundary conditions ⋮ Onset of thermohaline convection in a rectangular porous cavity in the presence of vertical vibration ⋮ Stability analysis of thermosolutal convection in a vertical packed porous enclosure ⋮ Double-diffusive Marangoni convection in a rectangular cavity: Onset of convection ⋮ Thermoconvective instabilities in an inclined porous channel heated from below ⋮ Unstable mixed convection in a heated inclined porous channel ⋮ Settling-driven instability in two-component stably stratified Hele-Shaw flows
Cites Work
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- Numerical study of double-diffusive natural convection in a porous cavity using the Darcy-Brinkman formulation
- On natural convection in vertical porous enclosures due to opposing fluxes of heat and mass prescribed at the vertical walls
- Convection induced by inclined thermal and solutal gradients in a shallow horizontal layer of a porous medium
- Onset of a Double-Diffusive Convective Regime in a Rectangular Porous Cavity
- Double diffusion in a vertical fluid layer: Onset of the convective regime
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