Mean-field description of plastic flow in amorphous solids

Abstract

Failure and flow of amorphous materials are central to various phenomena including earthquakes and landslides. There is accumulating evidence that the yielding transition between a flowing and an arrested phase is a critical phenomenon, but the associated exponents are not understood, even at a mean-field level where the validity of popular models is debated. Here we solve a mean-field model that captures the broad distribution of the mechanical noise generated by plasticity, whose behavior is related to biased Lévy flights near an absorbing boundary. We compute the exponent $\theta$ characterising the density of shear transformation $P(x)\sim x^{\theta }$, where $x$ is the stress increment beyond which they yield. We find that after an isotropic thermal quench, $\theta =1/2$. However, $\theta$ depends continuously on the applied shear stress, this dependence is not monotonic, and its value at the yield stress is not universal. The model rationalizes previously unexplained observations, and captures reasonably well the value of exponents in three dimensions. Values of exponents in four dimensions are accurately predicted. These results support that it is the true mean-field model that applies in large dimension, and raise fundamental questions on the nature of the yielding transition.

10 pages, 7 figures

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• Yield Stress Materials in Soft Condensed Matter
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• A random critical point separates brittle and ductile yielding transitions in amorphous materials
• Driving rate dependence of avalanche statistics and shapes at the yielding transition
• A direct link between active matter and sheared granular systems
• Elastic avalanches reveal marginal behaviour in amorphous solids
• How collective asperity detachments nucleate slip at frictional interfaces