Spatiotemporal Hierarchy of Slow Avalanches During Creep

TL;DR

This study uncovers the hierarchical spatio-temporal structure of thermal avalanches during creep in amorphous solids, revealing how local rearrangements promote long-range cascades and slow relaxation behaviors.

Contribution

It demonstrates the hierarchical organization of avalanches and the role of noise-mediated facilitation in slow relaxation, combining simulations and experiments.

Findings

Thermal avalanches form hierarchical, compact cascades.

Long-range facilitation links cascades, producing seismic-like correlations.

Experimental validation confirms the simulation-based framework.

Abstract

Far from equilibrium, amorphous solids exhibit structural relaxations that span a vast range of timescales such as physical aging and creep. Recently, it has been shown that such relaxations are driven by via intermittent, scale-free, yet anomalously slow cascades of local rearrangements, termed 'thermal avalanches.' Here, we investigate the spatio-temporal dynamics of these avalanches during logarithmic creep, using simulations of a model amorphous solid. By systematically disentangling mechanical and thermal activation events, we reveal that thermal avalanches have a hierarchical spatio-temporal structure: localized rearrangement events group into fast and compact cascades, which then promote the thermal activation of subsequent cascades via long-range, noise-mediated facilitation. This process results in heavy-tailed temporal correlations reminiscent of seismic activity. We validate these findings using experiments on slow relaxation of crumpled matter. Our work provides a framework for identifying noise-mediated correlations and elucidates the rich structural dynamics underlying slow relaxation of amorphous solids.