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Transient and stationary behavior of the Olami-Feder-Christensen earthquake model

Felix Wissel·Barbara Drossel
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Abstract

Using long-term computer simulations and mean-field like arguments, we investigate the transient time and the properties of the stationary state of the Olami-Feder-Christensen earthquake model as function of the coupling parameter $α$ and the system size $N$. The most important findings are that the transient time diverges nonanalytically when $α$ approaches zero, and that the avalanche-size distribution will not approach a power law with increasing system size.

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BibTeXRIS

Felix Wissel, Barbara Drossel. 2006-08-15. Transient and stationary behavior of the Olami-Feder-Christensen earthquake model. https://doi.org/10.1103/physreve.74.066109

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