Abstract
We probe the rheology of weakly vibrated granular flows as function of flow rate, vibration strength, and pressure by performing experiments in a vertically vibrated split-bottom shear cell. For slow flows, we establish the existence of a vibration-dominated granular flow regime, where the driving stresses smoothly vanish as the driving rate is diminished. We distinguish three qualitatively different vibration-dominated rheologies, most strikingly a regime where the shear stresses no longer are proportional to the pressure.
Original language | English |
---|---|
Article number | 012202 |
Journal | Physical Review E - Statistical, Nonlinear, and Soft Matter Physics |
Volume | 89 |
Issue number | 1 |
DOIs | |
Publication status | Published - 15 Jan 2014 |
Externally published | Yes |