The effect of interface movement and viscosity variation on the stability of a diffusive interface between aqueous and gaseous CO2
From MaRDI portal
Publication:2945297
DOI10.1063/1.4813072zbMath1320.76115OpenAlexW2079629266MaRDI QIDQ2945297
Bernard Meulenbroek, Hans Bruining, Rouhollah Farajzadeh
Publication date: 9 September 2015
Published in: Physics of Fluids (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1063/1.4813072
Related Items (2)
Hysteretic enhancement of carbon dioxide trapping in deep aquifers ⋮ Buoyancy-driven instabilities of partially miscible fluids in inclined porous media
Cites Work
- Unnamed Item
- An empirical theory for gravitationally unstable flow in porous media
- Theory of fluid flows through natural rocks
- Numerical simulation of density-driven natural convection in porous media with application for CO\(_{2}\) injection projects
- The stability of a fluid layer subjected to a step change in temperature: transient vs. frozen time analyses
- Non-modal growth of perturbations in density-driven convection in porous media
- On the Brinkman correction in unidirectional Hele-Shaw flows
- Onset of convection in anisotropic porous media subject to a rapid change in boundary conditions
- Wavelength selection of fingering instability inside Hele–Shaw cells
- Gravitational instability of miscible fluids in a Hele-Shaw cell
- Stability of miscible displacements in porous media: Rectilinear flow
- STABILITY OF A SATURATED POROUS LAYER SUBJECT TO A SUDDEN RISE IN SURFACE TEMPERATURE: COMPARISON BETWEEN THE LINEAR AND ENERGY METHODS
- Secondary convection in a Hele Shaw cell
- Shear stabilization of miscible displacement processes in porous media
- Miscible porous media displacements in the quarter five-spot configuration. Part 1. The homogeneous case
- Density-driven unstable flows of miscible fluids in a Hele-Shaw cell
- A calculation of the viscous force exerted by a flowing fluid on a dense swarm of particles
This page was built for publication: The effect of interface movement and viscosity variation on the stability of a diffusive interface between aqueous and gaseous CO2