Thermoconvective flow in a saturated, isotropic, homogeneous porous medium using Brinkman’s model: numerical study
DOI10.1108/09615539810220298zbMath0962.76582OpenAlexW1979284083MaRDI QIDQ4700929
H. S. Takhar, V. Ramachandra Prasad, O. Anwar Beg, V. M. Soundalgekar
Publication date: 12 June 2001
Published in: International Journal of Numerical Methods for Heat & Fluid Flow (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1108/09615539810220298
parametric investigationviscous incompressible fluidboundary layerviscous dissipationvertical flat plateconvective flownon-Darcy porous mediumdouble shooting Runge-Kutta-Merson schemefinite difference implicit Keller box methodwall heat transfer rate
Flows in porous media; filtration; seepage (76S05) Finite difference methods applied to problems in fluid mechanics (76M20) Free convection (76R10)
Related Items (2)
Cites Work
- Natural convection in a shallow porous cavity - The Brinkman model
- A boundary-layer analysis for natural convection in vertical porous enclosures - Use of the Brinkman-extended Darcy model
- The Brinkman model for boundary layer regime in a rectangular cavity with uniform heat flux from the side
- Mixed convection of an incompressible viscous fluid in a porous medium past a hot vertical plate
- The boundary correction for the Rayleigh-Darcy problem: limitations of the Brinkman equation
- Analysis of the Brinkman equation as a model for flow in porous media
- Free convection in a saturated porous medium beyond the similarity solution
- Slow flow through stationary random beds and suspensions of spheres
- A calculation of the viscous force exerted by a flowing fluid on a dense swarm of particles
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