From Elasticity to Hypoplasticity: Dynamics of Granular Solids
arXiv:0706.1354 · doi:10.1103/PhysRevLett.99.105501
Abstract
"Granular elasticity," useful for calculating static stress distributions in granular media, is generalized by including the effects of slowly moving, deformed grains. The result is a hydrodynamic theory for granular solids that agrees well with models from soil mechanics.
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Cited by in corpus (14)
- Granular Solid Hydrodynamics
- Well-posed continuum equations for granular flow with compressibility and -rheology
- Anisotropic nonlinear elasticity in a spherical bead pack: influence of the fabric anisotropy
- Granular Solid Hydrodynamics (GSH): a broad-ranged macroscopic theory of granular media
- Applying GSH to a Wide Range of Experiments in Granular Media
- Granular Gas: Vibrating Walls, Two-Peak Distribution and Hydrodynamics
- An Expression for the Granular Elastic Energy
- Period tripling causes rotating spirals in agitated wet granular layers
- Why Granular Media Are Thermal, and Quite Normal, After All
- Similarities between GSH, Hypoplasticity and KCR
- Proportional Paths, Barodesy, and Granular Solid Hydrodynamics
- Shock Wave Response of Porous Materials: From Plasticity to Elasticity
- Temperatures in Grains and Plasma
- Granular Solid Hydrodynamics (GSH): from Quasi-Static Motion to Rapid Dense Flow