2002
DOI: 10.1103/physrevlett.89.204302
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Preavalanche Instabilities in a Granular Pile

Abstract: We investigate numerically the transition between static equilibrium and dynamic surface flow of a 2D cohesionless granular system driven by a continuous gravity loading. This transition is characterized by intermittent local dynamic rearrangements and can be described by an order parameter defined as the density of critical contacts, e.g. contacts where the friction is fully mobilized.Analysis of the spatial correlations of critical contacts shows the occurence of "fluidized" clusters which exhibit a power-la… Show more

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Cited by 97 publications
(109 citation statements)
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“…One can wonder if these collapse events are directly or indirectly related to the pre-avalanche precursors which have been previously studied [5][6][7][8][9]. Kabla et al…”
Section: Discussionmentioning
confidence: 99%
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“…One can wonder if these collapse events are directly or indirectly related to the pre-avalanche precursors which have been previously studied [5][6][7][8][9]. Kabla et al…”
Section: Discussionmentioning
confidence: 99%
“…Note that even if the solid volume fraction is used as a control parameter it reflects only partially the complexity of the granular microstructure from which originate the local mechanisms responsible for the micro-failures described in [5][6][7][8][9]. Other quantities should be more relevant than the solid volume fraction as for instance the dilatancy angle [12,23] or the mean coordination number.…”
Section: Conclusion and Prospectsmentioning
confidence: 99%
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“…In CD, an iterative algorithm based on nonlinear Gauss-Seidel iterations is used to determine the contact forces and particle velocities simultaneously at all potential contacts. The CD method has been extensively employed for the simulation of granular materials in 2D and 3D [55][56][57][58][59][60][61][62][63][64][65][66][67][68][69][70][71][72].…”
Section: Bonded Cell Modelmentioning
confidence: 99%
“…Important non equilibrium effects of structurally disordered granular systems, beside the slow relaxation to equilibrium [12,22,23], are : bistability and hysteresis [24,25,26] as the result of a memory effect due to the internal history dependence of systems out of equilibrium and the lack of an unique metastable state [2] ; and a jerky response to the external driving force with impulselike events (local rearrangements of grains or avalanches), as the result of the exploration of local minimal energy configurations [27,28]. A related important question is whether a diverging length-scale exists on the jammed side of the transition [29].…”
Section: Introductionmentioning
confidence: 99%