Why Do Granular Materials Stiffen with Shear Rate? A Test of Novel Stress-Based Statistics
arXiv:0810.4891 · doi:10.1103/PhysRevLett.101.268301
Abstract
Recent experiments exhibit a rate-dependence for granular shear such that the stress grows linearly in the logarithm of the shear rate, \dotγ. Assuming a generalized activated process mechanism, we show that these observations are consistent with a recent proposal for a stress-based statistical ensemble. By contrast, predictions for rate-dependence using conventional energy-based statistical mechanics to describe activated processes, predicts a rate dependence that of (\ln (\dotγ))^{1/2}.
4 pages, 4 figures
References in corpus (2)
Cited by in corpus (7)
- The Statistical Physics of Athermal Materials
- Intermittent relaxation and avalanches in extremely persistent active matter
- Equivalence of fluctuation-dissipation and Edwards' temperature in cyclically sheared granular systems
- Friction and the oscillatory motion of granular flows
- The role of microscopic friction in statistics and scaling laws of avalanches
- Jamming is a first-order transition with quenched disorder in amorphous materials sheared by cyclic quasistatic deformations
- Dense bidisperse suspensions under non-homogenous shear