Self-Organized Phase Segregation In a Driven Flow of Dissimilar Particles Mixtures
Physics and Astronomy
Self-organized patterns in an immiscible fluid mixture of dissimilar particles driven from a source at the bottom are examined as a function of hydrostatic pressure bias by a Monte Carlo computer simulation. As the upward pressure bias competes with sedimentation due to gravity, a multi-phase system emerges: a dissociating solid phase from the source is separated from a migrating gas phase towards the top by an interface of mixed (bicontinuous) phase. Scaling of solid-to-gas phase with the altitude is nonuniversal and depends on both the range of the height/depth and the magnitude of the pressure bias. Onset of phase separation and layering is pronounced at low bias range.
International Journal of Modern Physics C
Pandey, R. B.,
Cueva-Parra, L. A.
(2003). Self-Organized Phase Segregation In a Driven Flow of Dissimilar Particles Mixtures. International Journal of Modern Physics C, 14(7), 955-962.
Available at: https://aquila.usm.edu/fac_pubs/3191