From shear bands to earthquakes in a model granular material with contact aging
E. A. Jagla

TL;DR
This study uses molecular dynamics simulations to explore how contact aging in a granular material leads to a transition from uniform flow to shear banding and earthquake-like stick-slip behavior, revealing a unified framework for diverse deformation regimes.
Contribution
It introduces a model incorporating contact aging that reproduces a reentrant flow curve and connects uniform deformation, shear banding, and seismic phenomena.
Findings
Flow curve becomes reentrant with aging.
Shear bands form at intermediate strain rates.
Stick-slip behavior emerges at very low strain rates.
Abstract
We perform molecular dynamics simulations of homogeneous athermal systems of poly-disperse soft discs under shear. For purely repulsive interactions between particles, and under a confining external pressure, a monotonous flow curve (strain rate vs. stress) starting at a critical yield stress is obtained, with deformation distributing uniformly in the system, on average. Then we add a short range attractive contribution to the interaction potential that increases its intensity as particles remain in contact for a progressively longer time, mimicking an aging effect into the system. In this case the flow curve acquires a reentrant behavior, namely, a region of negative slope. Within this region the deformation is seen to localize in a shear band with a well defined width that decreases as the global strain rate does. At very low strain rates the shear band becomes very thin and…
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Taxonomy
TopicsGranular flow and fluidized beds · earthquake and tectonic studies · High-pressure geophysics and materials
