Home > Publications database > Instabilities at frictional interfaces: Creep patches, nucleation, and rupture fronts |
Journal Article | FZJ-2015-03867 |
; ; ;
2013
APS
College Park, Md.
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Please use a persistent id in citations: http://hdl.handle.net/2128/8802 doi:10.1103/PhysRevE.88.060403
Abstract: The strength and stability of frictional interfaces, ranging from tribological systems to earthquake faults, are intimately related to the underlying spatially extended dynamics. Here we provide a comprehensive theoretical account, both analytic and numeric, of spatiotemporal interfacial dynamics in a realistic rate-and-state friction model, featuring both velocity-weakening and velocity-strengthening behaviors. Slowly extending, loading-rate-dependent creep patches undergo a linear instability at a critical nucleation size, which is nearly independent of interfacial history, initial stress conditions, and velocity-strengthening friction. Nonlinear propagating rupture fronts—the outcome of instability—depend sensitively on the stress state and velocity-strengthening friction. Rupture fronts span a wide range of propagation velocities and are related to steady-state-front solutions.
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