Pages that link to "Item:Q2384222"
From MaRDI portal
The following pages link to Numerical simulation of double-diffusion driven convective flow and rock alteration in three-dimensional fluid-saturated geological fault zones (Q2384222):
Displaying 7 items.
- Effect of material anisotropy on the onset of convective flow in three-dimensional fluid-saturated faults (Q1402237) (← links)
- A double-layer reduced model for fault flow on slipping domains with an hybrid finite volume scheme (Q1632201) (← links)
- Double diffusion-driven convective instability of three-dimensional fluid-saturated geological fault zones heated from below (Q2457900) (← links)
- Computational simulation of chemical dissolution-front instability in fluid-saturated porous media under non-isothermal conditions (Q2952672) (← links)
- Numerical modelling of double diffusion driven reactive flow transport in deformable fluid‐saturated porous media with particular consideration of temperature‐dependent chemical reaction rates (Q4506301) (← links)
- Numerical simulation of the seismic wave propagation and fluid pressure in complex porous media at the mesoscopic scale (Q5885261) (← links)
- Effects of an internal cavity on heat transfer and mass transport in partially heated double corrugated domains (Q6494532) (← links)