Onset of sliding across scales: How the contact topography impacts frictional strength
Fabian Barras, Ramin Aghababaei, Jean-Fran\c{c}ois Molinari

TL;DR
This paper investigates how the topography of contact surfaces influences the initiation of frictional sliding across different scales, bridging atomistic microcontact failure mechanisms with macroscopic rupture dynamics.
Contribution
It introduces a coarse-grained cohesive law derived from atomistic simulations to unify micro- and macro-scale descriptions of frictional slip initiation.
Findings
Microcontact failure mode affects slip nucleation
Brittle vs. ductile failure impacts interface strength
Large-scale simulations reveal failure mechanism influence
Abstract
When two solids start rubbing together, frictional sliding initiates in the wake of slip fronts propagating along their surfaces in contact. This macroscopic rupture dynamics can be successfully mapped on the elastodynamics of a moving shear crack. However, this analogy breaks down during the nucleation process, which develops at the scale of surface asperities where microcontacts form. Recent atomistic simulations revealed how a characteristic junction size selects if the failure of microcontact junctions either arises by brittle fracture or by ductile yielding. This work aims at bridging these two complementary descriptions of the onset of frictional slip existing at different scales. We first present how the microcontacts failure observed in atomistic simulations can be conveniently "coarse-grained" using an equivalent cohesive law. Taking advantage of a scalable parallel…
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