Dynamic instabilities of frictional sliding at a bimaterial interface

TL;DR

This paper performs a detailed 2D linear stability analysis of a deformable solid sliding on a rigid surface, revealing universal instabilities at small wave numbers and the stabilizing effects of rate-and-state friction models.

Contribution

It derives the linear stability spectrum considering elastodynamic effects and finite size, highlighting the interplay between destabilizing bi-material coupling and stabilizing frictional laws.

Findings

Homogeneous sliding is universally unstable at small wave numbers.

Instability modes propagate at nearly wave and shear wave speeds.

Finite-time regularized normal stress response promotes stability.

Abstract

We study the 2D linear stability analysis of a deformable solid of a finite height $H$, steadily sliding on top of a rigid solid within a generic rate-and-state friction type constitutive framework, fully accounting for elastodynamic effects. We derive the linear stability spectrum, quantifying the interplay between stabilization related to the frictional constitutive law and destabilization related both to the elastodynamic bi-material coupling between normal stress variations and interfacial slip, and to finite size effects. The stabilizing effects related to the frictional constitutive law include velocity-strengthening friction (i.e.~an increase in frictional resistance with increasing slip velocity, both instantaneous and under steady-state conditions) and a regularized response to normal stress variations. We first consider the small wave-number $k$ limit and demonstrate that homogeneous sliding in this case is universally unstable, independently of the details of the friction law. This universal instability is mediated by propagating waveguide-like modes, whose fastest growing mode is characterized by a wave-number satisfying $k H\!\sim\!{\cal O}(1)$ and by a growth rate that scales with $H^{-1}$. We then consider the limit $k H\!\to\!\infty$ and derive the stability phase diagram in this case. We show that the dominant instability mode travels at nearly the dilatational wave-speed in the opposite direction to the sliding direction. Instability modes which travel at nearly the shear wave-speed in the sliding direction also exist in some range of physical parameters. Finally, we show that a finite-time regularized response to normal stress variations, within the framework of generalized rate-and-state friction models, tends to promote stability.