Diffusion, mixing, and segregation in confined granular flows
Alexander M. Fry, Paul B. Umbanhowar, Julio M. Ottino and, Richard M. Lueptow

TL;DR
This study uses simulations and continuum modeling to explore how pressure influences diffusion and segregation in confined granular flows, revealing conditions that promote mixing or segregation.
Contribution
It introduces a pressure-dependent continuum model that accurately predicts segregation and diffusion behaviors in bidisperse granular flows.
Findings
Diffusion is independent of overburden pressure.
Segregation rate decreases with increasing pressure.
High pressure can suppress segregation, promoting mixing.
Abstract
Discrete element method simulations of confined bidisperse granular shear flows elucidate the balance between diffusion and segregation that can lead to either mixed or segregated states, depending on confining pressure. Results indicate that the collisional diffusion is essentially independent of overburden pressure. Because the rate of segregation diminishes with overburden pressure, the tendency for particles to segregate weakens relative to the re-mixing of particles due to collisional diffusion as the overburden pressure increases. Using a continuum approach that includes a pressure dependent segregation velocity and a pressure independent diffusion coefficient, the interplay between diffusion and segregation is accurately predicted for both size and density bidisperse mixtures over a wide range of flow conditions when compared to simulation results. Additional simulations with…
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Taxonomy
TopicsGranular flow and fluidized beds · Landslides and related hazards · Rock Mechanics and Modeling
