Natural convection and the evolution of a reactive porous medium
From MaRDI portal
Publication:3097849
DOI10.1017/S0022112010006269zbMath1225.76266OpenAlexW1973196599MaRDI QIDQ3097849
No author found.
Publication date: 10 November 2011
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/s0022112010006269
Flows in porous media; filtration; seepage (76S05) Free convection (76R10) Reaction effects in flows (76V05) Convection in hydrodynamic stability (76E06)
Related Items (4)
Effects of hydrodynamic dispersion on the stability of buoyancy-driven porous media convection in the presence of first order chemical reaction ⋮ Substrate degradation in high-Rayleigh-number reactive convection ⋮ Thermosolutal convection in an evolving soluble porous medium ⋮ Dissolution-driven porous-medium convection in the presence of chemical reaction
Cites Work
- Finite amplitude convection in a two-component fluid saturated porous layer
- On numerical stability analysis of double-diffusive convection in confined enclosures
- Stability of an acid front moving through porous rock
- The effect of temperature-dependent solubility on the onset of thermosolutal convection in a horizontal porous layer
- Geological Fluid Dynamics
- Reactive Infiltration Instabilities
- A new oscillatory instability in a mushy layer during the solidification of binary alloys
- On gravity-driven flow through a reacting porous rock
- Convection in Porous Media
- Thermosolutal bifurcation phenomena in porous enclosures subject to vertical temperature and concentration gradients
- Dissolution-driven convection in a reactive porous medium
- Gravity-driven reacting flows in a confined porous aquifer
- Chemical Instabilities. II. Chemical Surface Reactions and Hydrodynamic Instability
- Convection Currents in a Porous Medium
This page was built for publication: Natural convection and the evolution of a reactive porous medium