Time-Resolved Studies of Stick-Slip Friction in Sheared Granular Layers

TL;DR

This study investigates the detailed dynamics of stick-slip friction in sheared granular layers using force measurements and imaging, revealing how particle properties and system parameters influence slip behavior and transitions to continuous sliding.

Contribution

It provides new insights into the velocity and stiffness dependence of granular stick-slip motion, including the transition to smooth sliding and microscopic rearrangements.

Findings

Stick-slip motion is nearly periodic over a wide parameter range.

A transition to continuous sliding occurs at a critical velocity Vc.

Microscopic rearrangements precede and follow slip events.

Abstract

Sensitive and fast force measurements are performed on sheared granular layers undergoing stick-slip motion, along with simultaneous imaging. A full study has been done for spherical particles with a +-20% size distribution. Stick-slip motion due to repetitive fluidization of the layer occurs for low driving velocities. Between major slip events, slight creep occurs that is variable from one event to the next. The effects of changing the stiffness k and velocity V of the driving system are studied in detail. The stick-slip motion is almost periodic for spherical particles over a wide range of parameters, but becomes irregular when k is large and V is relatively small. At larger V, the motion becomes smoother and is affected by the inertia of the upper plate bounding the layer. Measurements of the period T and amplitude A of the relative motion are presented as a function of V. At a critical value Vc, a transition to continuous sliding motion occurs that is discontinuous for k not too large. The time dependence of the instantaneous velocity of the upper plate and the frictional force produced by the granular layer are determined within individual slipping events. The force is a multi-valued function of the instantaneous velocity, with pronounced hysteresis and a sudden drop prior to resticking. Measurements of vertical displacement reveal a small dilation of the material (about one tenth of the mean particle size in a layer 20 particles deep) associated with each slip event. Finally, optical imaging reveals that localized microscopic rearrangements precede (and follow) each slip event. The behavior of smooth particles is contrasted with that of rough particles.