Abstract
This Letter introduces unexpected diffusion properties in dense granular flows and shows that they result from the development of partially jammed clusters of grains, or granular vortices. Transverse diffusion coefficients and average vortex sizes are systematically measured in simulated plane shear flows at differing inertial numbers revealing (i) a strong deviation from the expected scaling involving the grain size and shear rate and (ii) an increase in average vortex size at low , following but limited by the system size. A general scaling is introduced that captures all the measurements and highlights the key role of vortex size. This leads to establishing a scaling for the diffusivity in dense granular flow as involving the geometric average of shear time and inertial time as the relevant time scale. Analysis of grain trajectories is further evidence that this diffusion process arises from a vortex-driven random walk.
- Received 23 May 2017
DOI:https://doi.org/10.1103/PhysRevLett.119.178001
© 2017 American Physical Society