Phase boundaries and desynchronization in the single-defect Olami-Feder-Christensen model: Toward understanding earthquake power laws

We investigate the emergence of self-organized criticality (SOC) in the single-defect Olami-Feder-Christensen (OFC) model by quantifying the ordered phase and deriving theoretical phase boundaries. Using both square and honeycomb lattices, we analytically obtain expressions for the ordered-SOC transition boundary and the characteristic period, validating them against numerical simulations. The results show that while synchronization alone governs the transition to the ordered phase, the onset of SOC requires desynchronization triggered by supercritical toppling energies exceeding a certain threshold. These findings characterize the threshold-dependent nature of desynchronization under minimal inhomogeneity, providing a fundamental perspective that clarifies the mechanisms observed in the original OFC model.

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Publication Details

Journal
Physical review. E
Published
2026-02-18
DOI
https://doi.org/10.1103/7c3x-j5xf
Primary Topic
High-pressure geophysics and materials
Type
article
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article

Phase boundaries and desynchronization in the single-defect Olami-Feder-Christensen model: Toward understanding earthquake power laws

Nobuki Kame
Physical review. E
High-pressure geophysics and materials
article

Phase boundaries and desynchronization in the single-defect Olami-Feder-Christensen model: Toward understanding earthquake power laws

Nobuki Kame
article en

Abstract

We investigate the emergence of self-organized criticality (SOC) in the single-defect Olami-Feder-Christensen (OFC) model by quantifying the ordered phase and deriving theoretical phase boundaries. Using both square and honeycomb lattices, we analytically obtain expressions for the ordered-SOC transition boundary and the characteristic period, validating them against numerical simulations. The results show that while synchronization alone governs the transition to the ordered phase, the onset of SOC requires desynchronization triggered by supercritical toppling energies exceeding a certain threshold. These findings characterize the threshold-dependent nature of desynchronization under minimal inhomogeneity, providing a fundamental perspective that clarifies the mechanisms observed in the original OFC model.

Physical review. EVol. 113(3)
The University of Tokyo (JP)
Climate action
Openalex Percentile: Top 65%
High-pressure geophysics and materials
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