Transient and non-Darcian effects on natural convection flow in a vertical channel partially filled with porous medium: analysis with Forchheimer-Brinkman extended Darcy model

DOI10.1016/J.IJHEATMASSTRANSFER.2010.11.011zbMath1223.80008OpenAlexW2013094943MaRDI QIDQ631150

Atul Kumar Singh, Ajay Kumar Singh, Pratibha Agnihotri, N. P. Singh

Publication date: 22 March 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.2010.11.011

zbMATH Keywords

porous mediumnatural convectionvertical channeltransient and non-Darcian effects

Mathematics Subject Classification ID

Flows in porous media; filtration; seepage (76S05) Free convection (76R10)

Related Items (6)

Effects of viscous and darcy dissipation on fully developed natural convection flow in a composite channel partially filled with porous material: Homotopy perturbation method (HPM) ⋮ New benchmark solutions for transient natural convection in partially porous annuli ⋮ Buoyancy induced convection in a porous cavity with partially thermally active sidewalls ⋮ Analysis of heat flux bifurcation inside porous media incorporating inertial and dispersion effects -- an exact solution ⋮ Unsteady hydromagnetic convective flow in a vertical channel using Darcy-Brinkman-Forchheimer extended model with heat generation/absorption: analysis with asymmetric heating/cooling of the channel walls ⋮ Hydromagnetic convection flow in a porous medium bounded between vertical wavy wall and parallel flat wall: analysis using Darcy-Brinkman-Forchheimer model

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• Convection in Porous Media
• A model for the boundary condition of a porous material. Part 2
• A model for the boundary condition of a porous material. Part 1

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