ArticleProceedings of the National Academy of Sciences of the United States of America2014
Slow slip and the transition from fast to slow fronts in the rupture of frictional interfaces.
Article in Proceedings of the National Academy of Sciences of the United States of America, 2014. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 10 papers.
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Who cites it
10 citing papers in PubMed.
- Static friction coefficient depends on the external pressure and block shape due to precursor slip.Scientific reports · 2023Article
- Creep fronts and complexity in laboratory earthquake sequences illuminate delayed earthquake triggering.Nature communications · 2022Article
- How collective asperity detachments nucleate slip at frictional interfaces.Proceedings of the National Academy of Sciences of the United States of America · 2019Article
- Frictional weakening of slip interfaces.Science advances · 2019Article
- Nature of the high-speed rupture of the two-dimensional Burridge-Knopoff model of earthquakes.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2018Article
- Evolution of real contact area under shear and the value of static friction of soft materials.Proceedings of the National Academy of Sciences of the United States of America · 2018Article
- Evidence of friction reduction in laterally graded materials.Beilstein journal of nanotechnology · 2018Article
- Creep to inertia dominated stick-slip behavior in sliding friction modulated by tilted non-uniform loading.Scientific reports · 2016Article
- Onset of frictional sliding of rubber-glass contact under dry and lubricated conditions.Scientific reports · 2016Article
- Velocity-strengthening friction significantly affects interfacial dynamics, strength and dissipation.Scientific reports · 2015Article
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Authors and funding
6 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The failure of the population of microjunctions forming the frictional interface between two solids is central to fields ranging from biomechanics to seismology. This failure is mediated by the propagation along the interface of various types of rupture fronts, covering a wide range of velocities. Among them are the so-called slow fronts, which are recently discovered fronts much slower than the materials' sound speeds. Despite intense modeling activity, the mechanisms underlying slow fronts remain elusive. Here, we introduce a multiscale model capable of reproducing both the transition from fast to slow fronts in a single rupture event and the short-time slip dynamics observed in recent experiments. We identify slow slip immediately following the arrest of a fast front as a phenomenon sufficient for the front to propagate further at a much slower pace. Whether slow fronts are actually observed is controlled both by the interfacial stresses and by the width of the local distribution of forces among microjunctions. Our results show that slow fronts are qualitatively different from faster fronts. Because the transition from fast to slow fronts is potentially as generic as slow slip, we anticipate that it might occur in the wide range of systems in which slow slip has been reported, including seismic faults.
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