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Programme des sessions > Recherche par auteur > Cochet-Escartin Olivier

Negative avalanches and anomalous dilation in a granular fault
Adèle Douin  1, *@  , Eliot Saurety  1@  , Olivier Cochet-Escartin  2@  , Osvanny Ramos  3@  
1 : Institut Lumière Matière [Villeurbanne]
Université Claude Bernard Lyon 1, Centre National de la Recherche Scientifique
2 : Institut Lumière Matière [Villeurbanne]  (ILM)  -  Site web
Université Claude Bernard Lyon 1, Centre National de la Recherche Scientifique, Centre National de la Recherche Scientifique : UMR5306
UMR5306 CNRS Université Claude Bernard Lyon 1 Domaine Scientifique de La Doua Bâtiment Kastler, 10 rue Ada Byron 69622 Villeurbanne CEDEX, Franc -  France
3 : Institut Lumière Matière  (ILM)  -  Site web
CNRS : UMR5306, Université Claude Bernard - Lyon I (UCBL)
UMR5306 CNRS Université Claude Bernard Lyon 1 Domaine Scientifique de La Doua Bâtiment Kastler, 10 rue Ada Byron 69622 Villeurbanne CEDEX, Franc -  France
* : Auteur correspondant

When slowly shearing a granular system, we expect a slow accumulation of mechanical energy and a global dilation, interrupted by sudden avalanche-like events of energy release and a contraction of the structure. However, in the case of a compressed medium, we report a much richer behavior of the avalanches, including all four possible combinations between sudden contraction or sudden dilation with abrupt energy release or abrupt energy accumulation. Modifications in the stress network, captured by photoelasticity, can help us understand the four scenarios, particularly the totally counterintuitive one of sudden energy accumulation and dilation, that usually liberates a large amount of acoustic energy. Decoding it in the context of earthquakes: a large quake may not result in a relaxation of the fault, but in a more charged configuration, more likely to trigger other extreme events.


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