Phase Separation in a Normal Fluid Mixture
Viscoelastic Phase Separation
Phase Separation of Colloidal Suspensions
Numerical Simulations of Viscoelastic Phase Separation
Micro-Phase Separation in Diblock Copolymer
Interplay between Wetting and Phase Separation
Phase Separation under External Fields
Dynamic Control of the Smectic Membranes
Colloidal ‘Atom’
Colloidal Gel Network
Electrophoretic Separation of Charged Particles
Aggregation of Charged Colloidal Systems
Surface-Assisted Monodomain Formation of a Lyotropic Liquid Crystal
Shear-Induced Topological Transitions in a Membrane System
Spontaneous Onion-Structure Formation
Self-Organization in Phase Separation of a Lyotropic Liquid Crystal
We demonstrate by numerical simulations that spinodal decomposition of fluid mixtures is strongly dependent upon their “fluidity,” which characterizes the relative importance of the two relevant transport mechanisms, hydrodynamic flow and diffusion. Thus, it may not be “universal,” at least in two dimensions. For a high fluidity, we find “spontaneous double phase separation.” We confirm that this unusual phenomenon is caused by the following mechanism: High fluidity causes rapid geometrical coarsening of domains due to a hydrodynamic process, which is too fast for diffusion to follow. This brings the system out of equilibrium and induces secondary phase separation.