Network of recurrent events for the Olami-Feder-Christensen model

Tiago P. Peixoto and Jörn Davidsen
Phys. Rev. E 77, 066107 – Published 10 June 2008

Abstract

We numerically study the dynamics of a discrete spring-block model introduced by Olami, Feder, and Christensen (OFC) to mimic earthquakes and investigate to what extent this simple model is able to reproduce the observed spatiotemporal clustering of seismicity. Following a recently proposed method to characterize such clustering by networks of recurrent events [J. Davidsen, P. Grassberger, and M. Paczuski, Geophys. Res. Lett. 33, L11304 (2006)], we find that for synthetic catalogs generated by the OFC model these networks have many nontrivial statistical properties. This includes characteristic degree distributions, very similar to what has been observed for real seismicity. There are, however, also significant differences between the OFC model and earthquake catalogs, indicating that this simple model is insufficient to account for certain aspects of the spatiotemporal clustering of seismicity.

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  • Received 10 March 2008

DOI:https://doi.org/10.1103/PhysRevE.77.066107

©2008 American Physical Society

Authors & Affiliations

Tiago P. Peixoto*

  • Instituto de Física, Universidade de São Paulo, Caixa Postal 66318, 05315-970, São Paulo, Brazil

Jörn Davidsen

  • Complexity Science Group, Department of Physics & Astronomy, University of Calgary, Calgary, Alberta, Canada T2N 1N4

  • *tpeixoto@if.usp.br
  • davidsen@phas.ucalgary.ca

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Vol. 77, Iss. 6 — June 2008

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