SLOW DENSE GRANULAR FLOWS AS A SELF-INDUCED PROCESS

DOI10.1142/S0219525901000358zbMath1046.74015OpenAlexW2028561608MaRDI QIDQ4425295

Stéphane Le Dizès, Y. Forterre, Olivier Pouliquen

Publication date: 2001

Published in: Advances in Complex Systems (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1142/s0219525901000358

zbMATH Keywords

frictionshear flowstress fluctuation

Mathematics Subject Classification ID

Granularity (74E20) Granular flows (76T25)

Related Items (6)

Comparison of the compressible class of models and non-local models with the discrete element method for steady fully developed flow of cohesionless granular materials through a vertical channel ⋮ Extended kinetic theory for granular flow in a vertical chute ⋮ Experimental evidence of the kinematic Cosserat effect in dense granular flows ⋮ Different shear regimes in the dense granular flow in a vertical channel ⋮ Nonlinear elasto-plastic model for dense granular flow ⋮ A non-local rheology for dense granular flows

Cites Work

• Scales and kinetics of granular flows
• Surface flow of granular materials: model and experiments in heap formation
• Kinetic theories for granular flow: inelastic particles in Couette flow and slightly inelastic particles in a general flowfield
• Scaling laws in granular flows down rough inclined planes
• Analyses of slow high-concentration flows of granular materials

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