Model for steady state friction
- 10 April 1991
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 96 (B4) , 6121-6131
- https://doi.org/10.1029/90jb02536
Abstract
A model for dynamic steady state friction between two rough surfaces is developed in which the transfer of momentum from the horizontal to the vertical direction by collisions between asperities on opposing surfaces leads to a friction law which is independent of the detailed mechanism of energy dissipation. For nonfractal surfaces the model applies above a lower critical velocity which increases exponentially with smoothness. At high velocities there is velocity weakening and, as the smoothness of the surfaces increases, the velocity dependence rapidly approaches the experimentally observed logarithmic dependence, in agreement with phenomenological state variable friction laws. For fractallike surfaces the model applies over the whole velocity range above V = 0, showing velocity strengthening at low velocities and velocity weakening at high velocities, implying the existence of a stick‐sliplike instability.This publication has 29 references indexed in Scilit:
- Evidence for and implications of self-healing pulses of slip in earthquake rupturePhysics of the Earth and Planetary Interiors, 1990
- Properties of earthquakes generated by fault dynamicsPhysical Review Letters, 1989
- The critical slip distance for seismic faultingNature, 1988
- Time‐predictable recurrence model for large earthquakesGeophysical Research Letters, 1980
- Aging and strain softening model for episodic faultingTectonophysics, 1979
- Steady‐state seismic slip – A precise recurrence modelGeophysical Research Letters, 1977
- The role of asperity indentation and ploughing in rock friction — IInternational Journal of Rock Mechanics and Mining Sciences, 1976
- The mechanics of stick-slipTectonophysics, 1970
- Stick-Slip as a Mechanism for EarthquakesScience, 1966
- On the Mechanics of FaultingGeological Magazine, 1942