Hauptseite > Publikationsdatenbank > Unstable Slip Pulses and Earthquake Nucleation as a Nonequilibrium First-Order Phase Transition |
Journal Article | FZJ-2019-00454 |
; ; ; ;
2018
APS
College Park, Md.
This record in other databases:
Please use a persistent id in citations: http://hdl.handle.net/2128/21264 doi:10.1103/PhysRevLett.121.234302
Abstract: The onset of rapid slip along initially quiescent frictional interfaces, the process of “earthquake nucleation,” and dissipative spatiotemporal slippage dynamics play important roles in a broad range of physical systems. Here we first show that interfaces described by generic friction laws feature stress-dependent steady-state slip pulse solutions, which are unstable in the quasi-1D approximation of thin elastic bodies. We propose that such unstable slip pulses of linear size L∗ and characteristic amplitude are “critical nuclei” for rapid slip in a nonequilibrium analogy to equilibrium first-order phase transitions and quantitatively support this idea by dynamical calculations. We then perform 2D numerical calculations that indicate that the nucleation length L∗ exists also in 2D and that the existence of a fracture mechanics Griffith-like length LG<L∗ gives rise to a richer phase diagram that features also sustained slip pulses.
![]() |
The record appears in these collections: |