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@ARTICLE{BarSinai:173406,
author = {Bar-Sinai, Yohai and Spatschek, Robert and Brener, Efim and
Bouchbinder, Eran},
title = {{O}n the velocity-strengthening behavior of dry friction},
journal = {Journal of geophysical research / Solid earth},
volume = {119},
number = {3},
issn = {2169-9313},
address = {Hoboken, NJ},
publisher = {Wiley},
reportid = {FZJ-2014-06816},
pages = {1738 - 1748},
year = {2014},
abstract = {The onset of frictional instabilities, e.g., earthquakes
nucleation, is intimately related to velocity-weakening
friction, in which the frictional resistance of interfaces
decreases with increasing slip velocity. While this
frictional response has been studied extensively, less
attention has been given to steady state
velocity-strengthening friction, in spite of its potential
importance for various aspects of frictional phenomena such
as the propagation speed of interfacial rupture fronts and
the amount of stored energy released by them. In this note
we suggest that a crossover from steady state
velocity-weakening friction at small slip velocities to
steady state velocity-strengthening friction at higher
velocities might be a generic feature of dry friction. We
further argue that while thermally activated rheology
naturally gives rise to logarithmic steady state
velocity-strengthening friction, a crossover to
stronger-than-logarithmic strengthening might take place at
higher slip velocities, possibly accompanied by a change in
the dominant dissipation mechanism. We sketch a few physical
mechanisms that may account for the crossover to
stronger-than-logarithmic steady state velocity
strengthening and compile a rather extensive set of
experimental data available in the literature, lending
support to these ideas.},
cin = {PGI-2},
ddc = {550},
cid = {I:(DE-Juel1)PGI-2-20110106},
pnm = {424 - Exploratory materials and phenomena (POF2-424)},
pid = {G:(DE-HGF)POF2-424},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000336844700012},
doi = {10.1002/2013JB010586},
url = {https://juser.fz-juelich.de/record/173406},
}