Non-monotonic Dynamics in the Onset of Frictional Slip

The transition from static to dynamic friction is often described as a fracture instability. However, studies on slow sliding processes aimed at understanding frictional instabilities and earthquakes report slow friction transients that are usually explained by empirical rate-and-state formulations....

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Bibliographic Details
Main Authors: Bonn, D. (Author), Farain, K. (Author)
Format: Article
Language:English
Published: Springer 2022
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Online Access:View Fulltext in Publisher
Description
Summary:The transition from static to dynamic friction is often described as a fracture instability. However, studies on slow sliding processes aimed at understanding frictional instabilities and earthquakes report slow friction transients that are usually explained by empirical rate-and-state formulations. We perform very slow (∼ nm/s) macroscopic-scale sliding experiments and show that the onset of frictional slip is governed by continuous non-monotonic dynamics originating from a competition between contact aging and shear-induced rejuvenation. This allows to describe both our non-monotonic dynamics and the simpler rate-and-state transients with a single evolution equation. © 2022, The Author(s).
ISBN:10238883 (ISSN)
DOI:10.1007/s11249-022-01598-z