A sidewall friction driven ordering transition in granular channel flows: Implications for granular rheology

Abstract

We report a transition from a disordered state to an ordered state in the flow of nearly mono-disperse granular matter flowing in an inclined channel with a bumpy base, in discrete element method simulations. For low particle-sidewall friction coefficients, the particles are disordered and the Bagnold velocity profile is obtained. However, for high sidewall friction, an ordered state is obtained, characterized by a layering of the particles and hexagonal packing of the particles in each layer. The extent of ordering, quantified by the local bond-orientational order parameter, varies in the cross- section of the channel, with the highest ordering near the side walls. The flow transition significantly affects the local rheology: the effective friction coefficient is lower, and the packing fraction is higher, in the ordered state compared to the disordered state. A simple model, incorporating the extent of local ordering, is shown to describe the rheology of the system.

5 pages and 6 figures

References in corpus (4)

• Crystallization of a quasi-two-dimensional granular fluid
• A Microscopic Description of the Granular Fluidity Field in Nonlocal Flow Modeling
• Hysteresis and competition between disorder and crystallization in sheared and vibrated granular flow
• Fast decay of the velocity autocorrelation function in dense shear flow of inelastic hard spheres