Avalanches can increase stored energy in a granular fault
Abstract
Slowly sheared granular materials generally store mechanical energy and dilate between abrupt failures that release energy and compact the material. Here, simultaneous measurements of torque, layer thickness, acoustic emission, and photoelastic force networks reveal all four combinations of energy release or storage with contraction or dilation in a compressed granular fault. Most strikingly, some avalanches both dilate the layer and increase the elastic energy transmitted to the resisting boundary. These events reorganize force chains beyond the shear band and produce a distinct acoustic response. The results show that an avalanche need not relax a driven disordered material; it can instead redistribute stress into a more highly loaded configuration, a mechanism with potential relevance to the physics of both laboratory and natural faults.
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BibTeX
@misc{douin2026avalanches,
title = {{Avalanches can increase stored energy in a granular fault}},
author = {A. Douin and E. Saurety and V. Levy dit Vehel and L. Combe and L. Vanel and O. Cochet-Escartin and O. Ramos},
howpublished = {arXiv},
year = {2026},
month = sep,
doi = {10.48550/arxiv.2609.14406},
eprint = {2609.14406},
archivePrefix = {arXiv},
url = {https://arxiv.org/abs/2609.14406},
}
RIS
TY - UNPB
TI - Avalanches can increase stored energy in a granular fault
AU - A. Douin
AU - E. Saurety
AU - V. Levy dit Vehel
AU - L. Combe
AU - L. Vanel
AU - O. Cochet-Escartin
AU - O. Ramos
PY - 2026
DA - 2026/09/13
PB - arXiv
DO - 10.48550/arxiv.2609.14406
UR - https://arxiv.org/abs/2609.14406
AB - Slowly sheared granular materials generally store mechanical energy and dilate between abrupt failures that release energy and compact the material. Here, simultaneous measurements of torque, layer thickness, acoustic emission, and photoelastic force networks reveal all four combinations of energy release or storage with contraction or dilation in a compressed granular fault. Most strikingly, some avalanches both dilate the layer and increase the elastic energy transmitted to the resisting boundary. These events reorganize force chains beyond the shear band and produce a distinct acoustic response. The results show that an avalanche need not relax a driven disordered material; it can instead redistribute stress into a more highly loaded configuration, a mechanism with potential relevance to the physics of both laboratory and natural faults.
ER -