State-variable friction for the Burridge-Knopoff model

Ian Clancy and David Corcoran
Phys. Rev. E 80, 016113 – Published 20 July 2009

Abstract

This work shows the relationship of the state variable rock-friction law proposed by Dieterich to the Carlson and Langer friction law commonly used in the Burridge-Knopoff (BK) model of earthquakes. Further to this, the Dieterich law is modified to allow slip rates of zero magnitude yielding a three parameter friction law that is included in the BK system. Dynamic phases of small scale and large scale events are found with a transition surface in the parameter space. Near this transition surface the event size distribution follows a power law with an exponent that varies as the transition is approached contrasting with the invariant exponent observed using the Carlson and Langer friction. This variability of the power-law exponent is consistent with the range of exponents measured in real earthquake systems and is more selective than the range observed in the Olami-Feder-Christensen model.

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  • Received 11 December 2008

DOI:https://doi.org/10.1103/PhysRevE.80.016113

©2009 American Physical Society

Authors & Affiliations

Ian Clancy* and David Corcoran

  • Department of Physics, University of Limerick, Ireland

  • *ian.clancy@ul.ie
  • david.corcoran@ul.ie

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Vol. 80, Iss. 1 — July 2009

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