Finite element modeling of dynamic frictional rupture with rate and state friction

TL;DR

This paper uses finite element modeling to analyze how finite size effects influence rate and state frictional behavior, revealing transient steady states, stress concentrations, and long-term stability differences between velocity weakening and strengthening laws.

Contribution

It introduces finite element simulations for finite size systems with rate and state friction, highlighting boundary effects and long-term stability, which are less explored compared to infinite domain models.

Findings

Transient steady states occur before wave reflections return.

Velocity weakening friction is unstable over long times, leading to acceleration.

Velocity weakening-strengthening friction reaches a stable steady state.

Abstract

Numerous laboratory experiments have demonstrated the dependence of the friction coefficient on the interfacial slip rate and the contact history, a behavior generically called rate and state friction. Although numerical models have been widely used for analyzing rate and state friction, in general they consider infinite elastic domains surrounding the sliding interface and rely on boundary integral formulations. Much less work has been dedicated to modeling finite size systems to account for interactions with boundaries. This paper investigates rate and state frictional interfaces in the context of finite size systems with the finite element method in explicit dynamics. We investigate the long term behavior of the sliding interface for two different friction laws: a velocity weakening law, for which the friction monotonously decreases with increasing sliding velocity, and a velocity weakening-strengthening law, for which the friction coefficient first decreases but then increases above a critical velocity. We show that for both friction laws at finite times, that is before wave reflections from the boundaries come back to the sliding interface, a temporary steady state sliding is reached, with a well-defined stress drop at the interface. This stress drop gives rise to a stress concentration and leads to an analogy between friction and fracture. However, at longer times, that is after multiple wave reflections, the stress drop is essentially zero, resulting in losing the analogy with fracture mechanics. Finally, the simulations reveal that velocity weakening is unstable at long time scales, as it results in an acceleration of the sliding blocks. On the other hand, velocity weakening-strengthening reaches a steady state sliding configuration.