Buoyant flow in a vertical fluid saturated porous annulus: the Brinkman model
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Publication:533274
DOI10.1016/J.IJHEATMASSTRANSFER.2010.11.014zbMath1211.80033OpenAlexW2049874718MaRDI QIDQ533274
Ioan Pop, Eugenia Rossi di Schio, Michele Celli
Publication date: 2 May 2011
Published in: International Journal of Heat and Mass Transfer (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/j.ijheatmasstransfer.2010.11.014
Related Items (4)
Steady fully developed non-Darcian mixed convection flow in an annulus partially filled with porous material ⋮ Buoyancy induced convection in a porous cavity with partially thermally active sidewalls ⋮ Mixed convection flow in a vertical tube filled with porous material with time-periodic boundary condition: steady-periodic regime ⋮ Analysis of entropy generation and energy transport of Cu-water nanoliquid in a tilted vertical porous annulus
Cites Work
- Natural convection in a vertical porous annulus
- Porous media convection between vertical walls: continuum of solutions from capped to open ends
- Unstably stratified Darcy flow with impressed horizontal temperature gradient, viscous dissipation and asymmetric thermal boundary conditions
- The onset of convection in a porous layer induced by viscous dissipation: A linear stability analysis
- Stability analysis of dual adiabatic flows in a horizontal porous layer
- Maximum density effects on natural convection in a vertical annulus filled with a non-Darcy porous medium
- Onset of convection in a permeable medium between vertical coaxial cylinders
- Convection in Porous Media
- The drag on a cloud of spherical particles in low Reynolds number flow
- Slow flow through stationary random beds and suspensions of spheres
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