Forchheimer and Brinkman extended Darcy flow model of natural convection in a vertical cylindrical porous annulus
From MaRDI portal
Publication:1914321
DOI10.1007/BF01176815zbMath0866.76087OpenAlexW2328349311MaRDI QIDQ1914321
Publication date: 20 July 1997
Published in: Acta Mechanica (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1007/bf01176815
Lua error in Module:PublicationMSCList at line 37: attempt to index local 'msc_result' (a nil value).
Related Items (8)
A lattice Boltzmann model for axisymmetric thermal flows through porous media ⋮ 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 ⋮ New benchmark solutions for transient natural convection in partially porous annuli ⋮ 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 ⋮ Numerical study of natural convection in a vertical porous annulus with discrete heating ⋮ Local and average heat transfer in the thermally developing region of an asymmetrically heated channel ⋮ Hydromagnetic convection flow in a porous medium bounded between vertical wavy wall and parallel flat wall: analysis using Darcy-Brinkman-Forchheimer model ⋮ Maximum density effects on natural convection in a vertical annulus filled with a non-Darcy porous medium
Cites Work
- Natural convection in a shallow porous cavity - The Brinkman model
- Natural convection in a vertical porous annulus
- A boundary-layer analysis for natural convection in vertical porous enclosures - Use of the Brinkman-extended Darcy model
- Axisymmetric free convection at small Rayleigh number in porous cavities
- A numerical study of the applicability of the Boussinesq approximation for a fluid-saturated porous medium
- The departure from Darcy flow in natural convection in a vertical porous layer
- A calculation of the viscous force exerted by a flowing fluid on a dense swarm of particles
This page was built for publication: Forchheimer and Brinkman extended Darcy flow model of natural convection in a vertical cylindrical porous annulus
