Olami-Feder-Christensen model

In physics, in the area of dynamical systems, the Olami-Feder-Christensen model is an example of self-organized criticality where local exchange dynamics are not conservative.

Additional recommended knowledge

Safe Weighing Range Ensures Accurate Results

Recognize and detect the effects of electrostatic charges on your balance

Weighing the right way

References

• Christensen, K. and Olami, Z. (1992). "Variation of the Gutenberg-Richter b values and nontrivial temporal correlations in a spring-block model for earthquakes". Journal of Geophysical Research B 97: 8729–8735.

• Grassberger, P. (1994). "Efficient large-scale simulations of a uniformly driven system". Physical Review E 49: 2436–2444. doi:10.1103/PhysRevE.49.2436.

• Lise, S. and Paczuski, M. (2001). "Self-organized criticality and universality in a nonconservative earthquake model". Physical Review E 63: 036111. doi:10.1103/PhysRevE.63.036111.

• Lise, S. and Paczuski, M. (2001). "Scaling in a nonconservative earthquake model of self-organized criticality". Physical Review E 64: 046111. doi:10.1103/PhysRevE.64.046111.

• Olami, Z., Feder, H. J. S. and Christensen, K. (1992). "Self-organized criticality in a continuous, nonconservative cellular automaton modeling earthquakes". Physical Review Letters 68: 1244–1247. doi:10.1103/PhysRevLett.68.1244.