Onset of Darcy–Bénard convection in a horizontal layer of dual-permeability medium with isothermal boundaries
From MaRDI portal
Publication:5115432
DOI10.1017/jfm.2020.462zbMath1460.76741OpenAlexW3044439629MaRDI QIDQ5115432
Publication date: 13 August 2020
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/jfm.2020.462
Related Items (1)
Cites Work
- A representation of the equations of multicomponent multiphase seepage
- Convection with local thermal non-equilibrium and microfluidic effects
- The onset of convection in a bidisperse porous medium
- On thermal equation for flow in porous media
- Onset of Darcy-Bénard convection using a thermal non-equilibrium model
- Basic concepts in the theory of seepage of homogeneous liquids in fissured rocks [strata]
- Onset of convection in a layered porous medium heated from below
- Dispersion effects on thermal convection in porous media
- Horizontally isotropic bidispersive thermal convection
- Convection in Porous Media
- Horizontally isotropic double porosity convection
- On the principle of exchange of stabilities
- Convection Currents in a Porous Medium
- Unnamed Item
This page was built for publication: Onset of Darcy–Bénard convection in a horizontal layer of dual-permeability medium with isothermal boundaries