International audienceA pure and incompressible material is confined between two plates such that it is heated from below and cooled from above. When its melting temperature is comprised between these two imposed temperatures, an interface separating liquid and solid phases appears. Depending on the initial conditions, freezing or melting occurs until the interface eventually converges towards a stationary state. This evolution is studied numerically in a two-dimensional configuration using a phase-field method coupled with the Navier-Stokes equations. Varying the control parameters of the model, we exhibit two types of equilibria: diffusive and convective. In the latter case, Rayleigh-Bénard convection in the liquid phase shapes the solid-...
International audienceThe presence of a magma ocean may have characterized the beginning of terrestr...
The stability of a shear flow imposed along a diffusive interface that separates two miscible liquid...
The two-dimensional motion of a fluid confined between two long horizontal planes, heated and salted...
International audienceWe study the evolution of a melting front between the solid and liquid phases ...
International audienceSolid-state convection can take place in the rocky or icy mantles of planetary...
On the basis of the phase-field approach we investigate the simultaneous diffusive and convective ev...
When a horizontal layer of fluid is cooled and solidified from the top, a cellular form of natural c...
We numerically study the melting process of a solid layer heated from below such that a liquid melt ...
International audienceWe report an idealized numerical study of a melting and freezing solid adjacen...
A numerical investigation of transient natural convective heat transfer with coupled phase change is...
We develop a phase-field model for the solidification of a pure material that includes convection in...
The paper presents the results of the study of the models of convective instability near its thresho...
A thin layer of a single-component Boussinesq fluid, contained between two rigid horizontal plates o...
The motion of the freezing front between a dendritic crystal and a supercooled liquid is studied usi...
International audienceThe presence of a magma ocean may have characterized the beginning of terrestr...
The stability of a shear flow imposed along a diffusive interface that separates two miscible liquid...
The two-dimensional motion of a fluid confined between two long horizontal planes, heated and salted...
International audienceWe study the evolution of a melting front between the solid and liquid phases ...
International audienceSolid-state convection can take place in the rocky or icy mantles of planetary...
On the basis of the phase-field approach we investigate the simultaneous diffusive and convective ev...
When a horizontal layer of fluid is cooled and solidified from the top, a cellular form of natural c...
We numerically study the melting process of a solid layer heated from below such that a liquid melt ...
International audienceWe report an idealized numerical study of a melting and freezing solid adjacen...
A numerical investigation of transient natural convective heat transfer with coupled phase change is...
We develop a phase-field model for the solidification of a pure material that includes convection in...
The paper presents the results of the study of the models of convective instability near its thresho...
A thin layer of a single-component Boussinesq fluid, contained between two rigid horizontal plates o...
The motion of the freezing front between a dendritic crystal and a supercooled liquid is studied usi...
International audienceThe presence of a magma ocean may have characterized the beginning of terrestr...
The stability of a shear flow imposed along a diffusive interface that separates two miscible liquid...
The two-dimensional motion of a fluid confined between two long horizontal planes, heated and salted...