Convective carbon dioxide dissolution in a closed porous medium at low pressure
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Publication:4685411
DOI10.1017/JFM.2018.622zbMath1415.76622arXiv1801.02537OpenAlexW2889172768WikidataQ129310044 ScholiaQ129310044MaRDI QIDQ4685411
Baole Wen, Li Zhang, Daria Akhbari, Marc Andre Hesse
Publication date: 8 October 2018
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://arxiv.org/abs/1801.02537
Related Items (4)
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Cites Work
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- Computational approaches to aspect-ratio-dependent upper bounds and heat flux in porous medium convection
- Convective mixing influenced by the capillary transition zone
- Stability of a fluid-saturated porous medium heated from below by forced convection.
- Spectral methods for incompressible viscous flow
- Onset of thermal convection in a porous layer with mixed boundary conditions
- Carbon dioxide dissolution in structural and stratigraphic traps
- Two-phase gravity currents in porous media
- Structure and stability of steady porous medium convection at large Rayleigh number
- Wall to wall optimal transport
- Onset of convection in anisotropic porous media subject to a rapid change in boundary conditions
- Bounds for heat transport in a porous layer
- High-Rayleigh-number convection in a fluid-saturated porous layer
- Transient solute transport with sorption in Poiseuille flow
- The impact of imperfect heat transfer on the convective instability of a thermal boundary layer in a porous media
- Inclined porous medium convection at large Rayleigh number
- Onset of buoyancy-driven convection in a liquid-saturated cylindrical porous layer supported by a gas layer
- Convective shutdown in a porous medium at high Rayleigh number
- Third‐order‐accurate semi‐implicit Runge–Kutta scheme for incompressible Navier–Stokes equations
- Convection Currents in a Porous Medium
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