Natural convection in a shallow porous cavity - The Brinkman model
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Publication:581153
DOI10.1016/0017-9310(87)90005-6zbMath0626.76086OpenAlexW2037507708MaRDI QIDQ581153
Publication date: 1987
Published in: International Journal of Heat and Mass Transfer (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/0017-9310(87)90005-6
no-slip boundary conditionnatural convection problempetroleum reservoircavity with free upper surfacedifferentially heated sidewallsshallow porous rectangular cavity
Absolute and convective instability and stability in hydrodynamic stability (76E15) Flows in porous media; filtration; seepage (76S05) Free convection (76R10)
Related Items (6)
Forchheimer and Brinkman extended Darcy flow model of natural convection in a vertical cylindrical porous annulus ⋮ Conduction-radiation effect on natural convection flow in fluid-saturated non-Darcy porous medium enclosed by non-isothermal walls ⋮ Surface-radiation effect on natural convection flow in a fluid-saturated non-Darcy porous medium enclosed by non-isothermal walls ⋮ Non-Darcy effects on conjugate double-diffusive natural convection in a variable porous layer sandwiched by finite thickness walls ⋮ Thermoconvective flow in a saturated, isotropic, homogeneous porous medium using Brinkman’s model: numerical study ⋮ Finite element analysis of heat transfer by natural convection in porous media in vertical enclosures
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