Dynamics of fault motion in a stochastic spring-slider model with varying neighboring interactions and time-delayed coupling

• Published in: Nonlinear dynamics 2017-03, Vol.87 (4), p.2563-2575
• Main Authors: Kostić, Srđan, Vasović, Nebojša, Franović, Igor, Todorović, Kristina, Klinshov, Vladimir, Nekorkin, Vladimir
• Format: Article
• Language: English
• Subjects: Automotive Engineering; Bifurcations; Classical Mechanics; Control; Coupling; Dynamic tests; Dynamical Systems; Dynamics; Earthquakes; Engineering; Friction; Hopf bifurcation; Mathematical models; Mechanical Engineering; Noise; Nonlinear dynamics; Original Paper; Oscillations; Qualitative analysis; Seismic analysis; Seismic stability; Stability analysis; Stochastic systems; Vibration
• ISSN: 0924-090X; 1573-269X
• DOI: 10.1007/s11071-016-3211-5

We examine dynamics of a fault motion by analyzing behavior of a spring-slider model composed of 100 blocks where each block is coupled to a varying number of 2 K neighboring units (1  ≤  2 K   ≤   N , N = 100 ). Dynamics of such model is studied under the effect of delayed interaction, variable coupling strength and random seismic noise. The qualitative analysis of stability and bifurcations is carried out by deriving an approximate deterministic mean-field model, which is demonstrated to accurately capture the dynamics of the original stochastic system. The primary effect concerns the direct supercritical Andronov–Hopf bifurcation, which underlies transition from equilibrium state to periodic oscillations under the variation of coupling delay. Nevertheless, the impact of delayed interactions is shown to depend on the coupling strength and the friction force. In particular, for loosely coupled blocks and low values of friction, observed system does not exhibit any bifurcation, regardless of the assumed noise amplitude in the expected range of values. It is also suggested that a group of blocks with the largest displacements, which exhibit nearly regular periodic oscillations analogous to coseismic motion for system parameters just above the bifurcation curve, can be treated as a representative of an earthquake hypocenter. In this case, the distribution of event magnitudes, defined as a natural logarithm of a sum of squared displacements, is found to correspond well to periodic (characteristic) earthquake model.