Stability of natural convection in superposed fluid and porous layers: Equivalence of the one- and two-domain approaches
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Publication:1007988
DOI10.1016/j.ijheatmasstransfer.2008.07.045zbMath1156.80330OpenAlexW1964916313MaRDI QIDQ1007988
Publication date: 24 March 2009
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.2008.07.045
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Cites Work
- Linear stability of natural convection in superposed fluid and porous layers: influence of the interfacial modelling
- Stability of natural convection in superposed fluid and porous layers: Influence of the interfacial jump boundary condition
- The boundary correction for the Rayleigh-Darcy problem: limitations of the Brinkman equation
- Onset of convection in a fluid layer overlying a layer of a porous medium
- Penetrative convection in a superposed porous-mediumfluid layer via internal heating
- Local instant formulation of two-phase flow
- A calculation of the viscous force exerted by a flowing fluid on a dense swarm of particles
- Stability analysis of double-diffusive convection in superposed fluid and porous layers using a one-equation model.
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