How collective asperity detachments nucleate slip at frictional interfaces

Abstract

Sliding at a quasi-statically loaded frictional interface can occur via macroscopic slip events, which nucleate locally before propagating as rupture fronts very similar to fracture. We introduce a novel microscopic model of a frictional interface that includes asperity-level disorder, elastic interaction between local slip events, and inertia. For a perfectly flat and homogeneously loaded interface, we find that slip is nucleated by avalanches of asperity detachments of extension larger than a critical radius $A_c$ governed by a Griffith criterion. We find that after slip, the density of asperities at a local distance to yielding $x_{\sigma }$ presents a pseudo-gap $P(x_{\sigma })\sim (x_{\sigma }{)}^{\theta }$, where $\theta$ is a non-universal exponent that depends on the statistics of the disorder. This result makes a link between friction and the plasticity of amorphous materials where a pseudo-gap is also present. For friction, we find that a consequence is that stick-slip is an extremely slowly decaying finite size effect, while the slip nucleation radius $A_c$ diverges as a $\theta$-dependent power law of the system size. We discuss how these predictions can be tested experimentally.

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• Experimental evidence of seismic ruptures initiated by aseismic slip
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• Static Friction Coefficient Depends on the External Pressure and Block Shape due to Precursor Slip
• Scaling theory for the statistics of slip at frictional interfaces
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