Double-diffusive convection instability in a vertical porous enclosure
From MaRDI portal
Publication:4224548
DOI10.1017/S0022112098001591zbMath0927.76033OpenAlexW2133664191MaRDI QIDQ4224548
E. Bilgen, P. Vasseur, Mahmoud Mamou
Publication date: 17 January 1999
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/s0022112098001591
variational formulationlinear stability analysisbuoyancy forcesthermal effectsoscillatory instabilityLewis numberstationary instabilitynormalized porosityenclosure aspect ratiosolutal effects
Flows in porous media; filtration; seepage (76S05) Finite difference methods applied to problems in fluid mechanics (76M20) Finite element methods applied to problems in fluid mechanics (76M10) Convection in hydrodynamic stability (76E06)
Related Items
Numerical simulation of double-diffusion driven convective flow and rock alteration in three-dimensional fluid-saturated geological fault zones ⋮ Fixed-flux Rayleigh–Bénard convection in doubly periodic domains: generation of large-scale shear ⋮ Magnetic field effect on Soret driving free convection in an inclined porous cavity saturated by a conducting binary mixture ⋮ Convection of a binary fluid in a shallow porous cavity heated and salted from the sides ⋮ Double diffusion-driven convective instability of three-dimensional fluid-saturated geological fault zones heated from below ⋮ Double diffusion natural convection in a rectangular enclosure filled with binary fluid saturated porous media: The effect of lateral aspect ratio ⋮ Stability analysis of thermosolutal convection in a vertical packed porous enclosure ⋮ Natural convection in a trapezoidal enclosure filled with a porous medium ⋮ Lumped-system analysis of a cavity with triangular porous layers ⋮ The Soret effect on convection in a horizontal porous domain under cross temperature and concentration gradients ⋮ Parallel computation of natural convection in trapezoidal porous enclosures ⋮ Numerical modelling of double diffusion driven reactive flow transport in deformable fluid‐saturated porous media with particular consideration of temperature‐dependent chemical reaction rates ⋮ Near-onset dynamics in natural doubly diffusive convection