AIP Conference Proceedings 2009
DOI: 10.1063/1.3179976
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Rheological Transitions in Two- and Three-Dimensional Granular Media

Abstract: The planar shearing of dense systems of bidisperse as well as polydisperse, non-cohesive, hard, round, dissipative and frictional particles is simulated in two and three dimensions using Contact Dynamics. The system is sheared by smooth, frictional walls at constant shear velocities, subject to a constant normal force. Depending on the shear velocity, the system behavior belongs to one of the three different regimes (from high to low shear velocities): a) a fluid like state with almost homogeneous shearing, b)… Show more

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Cited by 3 publications
(5 citation statements)
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“…Our system size analysis shows a discontinuous transition from regime B to regime C, at V BC ≃0.10 and a continuous transition between regimes A and B completed at V AB ≃0.50 [19][20][21]. V BC and V AB are system size independent.…”
Section: B Shear Regimes and Strain Localizationmentioning
confidence: 98%
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“…Our system size analysis shows a discontinuous transition from regime B to regime C, at V BC ≃0.10 and a continuous transition between regimes A and B completed at V AB ≃0.50 [19][20][21]. V BC and V AB are system size independent.…”
Section: B Shear Regimes and Strain Localizationmentioning
confidence: 98%
“…However, with rough walls the homogeneous shear regime persists down to very low velocities, in spite of increasing fluctuations. The smooth walls of our system, allowing for slip and rotation at the walls, are responsible for the more complex behavior [19][20][21].…”
Section: B Shear Regimes and Strain Localizationmentioning
confidence: 99%
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“…The latter parameter can be determined e.g. from simple shear simulations [14] and it was found to be µ w ≃0.12. The result of numerical minimization at different aspect ra- tios match prefectly the simulation data as shown on Fig.…”
Section: Complex Shear Band Structuresmentioning
confidence: 99%