Measurements of the Yield Stress in Frictionless Granular Systems

TL;DR

This study uses molecular dynamics simulations to investigate whether frictionless granular systems can be characterized by a single static yield shear stress, revealing size-dependent discontinuities that vanish in the infinite system limit.

Contribution

The paper demonstrates that in the large system limit, frictionless granular materials are characterized by a single static yield shear stress, resolving previous ambiguities about shear initiation and maintenance.

Findings

Discontinuity in shear velocity at finite sizes diminishes as system size increases.

In the infinite system limit, a single static yield shear stress characterizes the system.

Short-time shear response depends on packing fraction and velocity profile shape.

Abstract

We perform extensive molecular dynamics simulations of 2D frictionless granular materials to determine whether these systems can be characterized by a single static yield shear stress. We consider boundary-driven planar shear at constant volume and either constant shear force or constant shear velocity. Under steady flow conditions, these two ensembles give similar results for the average shear stress versus shear velocity. However, near jamming it is possible that the shear stress required to initiate shear flow can differ substantially from the shear stress required to maintain flow. We perform several measurements of the shear stress near the initiation and cessation of flow. At fixed shear velocity, we measure the average shear stress $\Sigma_{yv}$ in the limit of zero shear velocity. At fixed shear force, we measure the minimum shear stress $\Sigma_{yf}$ required to maintain steady flow at long times. We find that in finite-size systems $\Sigma_{yf} > \Sigma_{yv}$, which implies that there is a jump discontinuity in the shear velocity from zero to a finite value when these systems begin flowing at constant shear force. However, our simulations show that the difference $\Sigma_{yf} - \Sigma_{yv}$, and thus the discontinuity in the shear velocity, tend to zero in the infinite system size limit. Thus, our results indicate that in the large system limit, frictionless granular systems are characterized by a single static yield shear stress. We also monitor the short-time response of these systems to applied shear and show that the packing fraction of the system and shape of the velocity profile can strongly influence whether or not the shear stress at short times overshoots the long-time average value.