% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{Brener:859605,
author = {Brener, Efim A. and Aldam, Michael and Barras, Fabian and
Molinari, Jean-François and Bouchbinder, Eran},
title = {{U}nstable {S}lip {P}ulses and {E}arthquake {N}ucleation as
a {N}onequilibrium {F}irst-{O}rder {P}hase {T}ransition},
journal = {Physical review letters},
volume = {121},
number = {23},
issn = {1079-7114},
address = {College Park, Md.},
publisher = {APS},
reportid = {FZJ-2019-00454},
pages = {234302},
year = {2018},
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.},
cin = {PGI-2},
ddc = {530},
cid = {I:(DE-Juel1)PGI-2-20110106},
pnm = {144 - Controlling Collective States (POF3-144)},
pid = {G:(DE-HGF)POF3-144},
typ = {PUB:(DE-HGF)16},
pubmed = {pmid:30576171},
UT = {WOS:000452683000010},
doi = {10.1103/PhysRevLett.121.234302},
url = {https://juser.fz-juelich.de/record/859605},
}