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Frozen barrier evolution in saturated porous media
Sheshukov A., Egorov A.
A numerical model capable of simulating the freezing of aqueous solution flow in saturated porous
Influence of internal grids on particle motion in the fluidized bed reactor
Solovev S., Soloveva O., Sheshukov E.
© 2019 Published under licence by IOP Publishing Ltd. A fluidized bed reactor designed
Stability analysis of traveling wave solution for gravity-driven flow
Egorov A., Dautov R., Nieber J., Sheshukov A.
A linear stability analysis was performed for three models of flow in unsaturated porous media
Stability analysis of gravity-driven infiltrating flow
Egorov A., Dautov R., Nieber J., Sheshukov A.
flow with a generalized nonequilibrium capillary pressure-saturation relation. With this nonequilibrium
Non-equilibrium model for gravity-driven fingering in water repellent soils: Formulation and 2D simulations
Nieber J., Sheshukov A., Egorov A., Dautov R.
The instability of infiltrating flow is studied using the mass balance equation coupled with a
Simulation of two-dimensional gravity-driven unstable flow
Dautov R., Egorov A., Nieber J., Sheshukov A.
] are described. These equations account for mechanism of dynamic capillary pressure via a first order relaxation
Stability analysis of traveling wave solution for gravity-driven flow
Egorov A., Dautov R., Nieber J., Sheshukov A.
A linear stability analysis was performed for three models of flow in unsaturated porous media
Stability analysis of gravity-driven infiltrating flow
Egorov A., Dautov R., Nieber J., Sheshukov A.
flow with a generalized nonequilibrium capillary pressure-saturation relation. With this nonequilibrium
Non-equilibrium model for gravity-driven fingering in water repellent soils: Formulation and 2D simulations
Nieber J., Sheshukov A., Egorov A., Dautov R.
The instability of infiltrating flow is studied using the mass balance equation coupled with a
Simulation of two-dimensional gravity-driven unstable flow
Dautov R., Egorov A., Nieber J., Sheshukov A.
] are described. These equations account for mechanism of dynamic capillary pressure via a first order relaxation

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