Experimental measurements of particle dynamics on the lower surface of a 3D Couette cell containing monodisperse spheres are reported. The average radial density and velocity profiles are similar to those previously measured within the bulk and on the lower surface of the 3D cell filled with mustard seeds. Observations of the evolution of particle velocities over time reveal distinct motion events, intervals where previously stationary particles move for a short duration before jamming again. The cross-correlation between the velocities of two particles at a given distance r from the moving wall reveals a characteristic lengthscale over which the particles are correlated. The autocorrelation of a single particle's velocity reveals a characteristic timescale τ which decreases with distance from the inner moving wall. This may be attributed to the increasing rarity at which the discrete motion events occur and the reduced duration of those events at large r. The relationship between the RMS azimuthal velocity fluctuations, δv θ (r), and average shear rate,γ(r), was found to be δv θ ∝γ α with α = 0.52 ± 0.04. These observations are compared with other recent experiments and with the modified hydrodynamic model recently introduced by Bocquet et al.
INTRODUCTIONThe detailed understanding of slow flow in dense granular systems has remained one of the central challenges in the field of granular materials [1]. While fast dilute granular flows are fluid-like and can be described well by granular kinetic theory [2][3][4], slow flows at high packing fraction preserve many of the complex properties of static granular packs and may be more accurately described as slow, plastic deformation of a metastable granular solid than flow of a fluid. Recent work by Howell and Behringer [5,6] showed that many of the intriguing properties of granular solids, such as the broad distribution of stresses and the presence of "force chains" which focus stresses along paths of many connected particles, play a crucial role. Direct visualization revealed that the flow is intermittant in time and that correlations, both in time and in space, exist [7]. These are seen as intervals over which one or more particles in a region become unjammed, move for a short time, and then become jammed again. Such properties of dense granular flow are reminiscent of behavior seen in glasses, dense colloidal suspensions, and foams [8]. Recent studies have been successful at relating stresses in stationary bead packs with those in glassy fluids [9], suggesting the two systems may also have similar flow properties for high packing fractions and low shearing rates. It is hoped that an understanding of dense granular flow will provide insight into the properties of static granular packs as well as the broader class of jammed systems.From previous work a number of unresolved fundamental questions about slow, dense granular shear flow emerge. Although videos and plots of particle trajectories suggest that particle velocities are correlated both in space and in time, the...