DUMONT, Denis; SOULARD, Pierre; SALEZ, Thomas; RAPHAEL, Elie; DAMMAN, Pascal

Metadatos

Mostrar el registro completo del ítem

Licencia de uso del documento

DUMONT, Denis
Laboratoire Interfaces et Fluides Complexes [Mons] [LIFC]

SOULARD, Pierre
Gulliver (UMR 7083)

SALEZ, Thomas
Laboratoire Ondes et Matière d'Aquitaine [LOMA]

Idioma

Article de revue

Este ítem está publicado en

Physical Review Letters. 2020-11-10, vol. 125, p. 208002

American Physical Society

Resumen en inglés

Gravity-driven flows of granular matter are involved in a wide variety of situations, ranging from industrial processes to geophysical phenomena, such as avalanches or landslides. These flows are characterized by the coexistence of solid and fluid phases, whose stability is directly related to the erosion and sedimentation occurring at the solid-fluid interface. To describe these mechanisms, we build a microscopic model involving friction, geometry, and a nonlocal cooperativity emerging from the propagation of collisions. This new picture enables us to obtain a detailed description of the exchanges between the fluid and solid phases. The model predicts a phase diagram including erosion, sedimentation, and stationary-flow regimes, in quantitative agreement with experiments and discrete-element-method simulations.< Leer menos

Orígen

Importado de Hal

Centros de investigación

Laboratoire Ondes et Matière d'Aquitaine (LOMA) - UMR 5798