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The Role of Fabric in Frictional Properties of Phyllosilicate-Rich Tectonic Faults
Published on: November 6, 2021
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A phase-plane analysis of localized frictional waves
T Putelat1, J H P Dawes2, A R Champneys1
1Department of Engineering Mathematics, University of Bristol, Bristol BS8 1UB, UK.
Summary
Sliding interfaces generate traveling waves, relevant to earthquakes and mechanical systems. A new model explains these waves using a spinodal friction law, revealing diverse wave behaviors.
Area of Science:
- Physics
- Mechanical Engineering
- Geophysics
Background:
- Sliding frictional interfaces generate traveling waves across various scales.
- These waves are relevant to phenomena like earthquake ground motion and mechanical brake performance.
Purpose of the Study:
- To propose an explanation for the origin of traveling waves at sliding interfaces.
- To study an idealized mechanical model of a shear-stressed elastic plate in frictional contact.
Main Methods:
- Constructed a nonlinear wave equation for plate deformation.
- Coupled the wave equation to a spinodal rate-and-state friction law.
- Employed analytical and numerical bifurcation analysis to study model solutions.
Main Results:
- The model sustains diverse solutions: periodic stick-slip wave trains, isolated slip/stick pulses, and detachment/attachment fronts.
- A two-parameter state diagram organizes these complex wave states.
- The spinodal friction law is crucial for capturing the full range of wave types.
Conclusions:
- The proposed model provides a framework for understanding traveling waves at frictional interfaces.
- The spinodal friction law offers a more comprehensive description than traditional Coulomb friction models.
- The study highlights the rich dynamics of wave generation in sliding systems.
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