Jamming, Yielding, and Rheology during Submerged Granular Avalanche

Fuente: arXiv
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Hauptverfasser: Ge, Zhuan, Man, Teng, Hill, Kimberly M., Wang, Yujie, Galindo-Torres, Sergio Andres
Format: Preprint
Veröffentlicht: 2024
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author Ge, Zhuan
Man, Teng
Hill, Kimberly M.
Wang, Yujie
Galindo-Torres, Sergio Andres
author_facet Ge, Zhuan
Man, Teng
Hill, Kimberly M.
Wang, Yujie
Galindo-Torres, Sergio Andres
contents 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 $μ-G$ relationship converges towards the equilibrium $μ_{eq}(G)$ after $G>G_0$ showing the critical point where the established rheological laws for steady states apply during transient conditions.
format Preprint
id arxiv_https___arxiv_org_abs_2408_13730
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Jamming, Yielding, and Rheology during Submerged Granular Avalanche
Ge, Zhuan
Man, Teng
Hill, Kimberly M.
Wang, Yujie
Galindo-Torres, Sergio Andres
Soft Condensed Matter
Geophysics
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 $μ-G$ relationship converges towards the equilibrium $μ_{eq}(G)$ after $G>G_0$ showing the critical point where the established rheological laws for steady states apply during transient conditions.
title Jamming, Yielding, and Rheology during Submerged Granular Avalanche
topic Soft Condensed Matter
Geophysics
url https://arxiv.org/abs/2408.13730