Jamming, Yielding, and Rheology during Submerged Granular Avalanche
Jamming transitions and the rheology of granular avalanches in fluids are investigated using experiments and numerical simulations. Simulations use the lattice-Boltzmann method coupled with the discrete element method, providing detailed stress and deformation data. Both simulations and experiments...
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Published in | arXiv.org |
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Main Authors | , , , , |
Format | Paper |
Language | English |
Published |
Ithaca
Cornell University Library, arXiv.org
25.08.2024
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Subjects | |
Online Access | Get full text |
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Summary: | Jamming transitions and the rheology of granular avalanches in fluids are investigated using experiments and numerical simulations. Simulations use the lattice-Boltzmann method coupled with the discrete element method, providing detailed stress and deformation data. Both simulations and experiments present a perfect match with each other in carefully conducted deposition experiments, validating the simulation method. We analyze transient rheological laws and jamming transitions using our recently introduced length-scale ratio \(G\). \(G\) serves as a unified metric for the pressure and shear rate capturing the dynamics of sheared fluid-granular systems. Two key transition points, \(G_{Y}\) and \(G_{0}\), categorize the material's state into solid-like, creeping, and fluid-like states. Yielding at \(G_{Y}\) marks the transition from solid-like to creeping, while \(G_{0}\) signifies the shift to the fluid-like state. The \(\mu-G\) relationship converges towards the equilibrium \(\mu_{eq}(G)\) after \(G>G_0\) showing the critical point where the established rheological laws for steady states apply during transient conditions. |
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ISSN: | 2331-8422 |