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- W2007119736 abstract "Granular material convects in response to vertical vibrations of sufficient peak acceleration. Particles flow upward in the center of a container with rough, vertical walls and downward in a thin stream along the sides. Canting the side walls outward from the vertical beyond a transition angle reverses the sense of the flow and changes its shape: particles flow upward in a broad region above the walls and downward in the center. We have studied this transition experimentally and find evidence for two opposing mechanisms, net downward shear at a rough vertical wall and 'ratcheting' at an oblique wall, which combine to determine the effect of the boundaries on particle motion. The direction of convective flow is not solely a function of the external boundaries, however. Continuous vibration can induce internal shear bands at which the flow is always observed to move downward, in which case a competition between the internal shear and the shear at the external boundaries determines the overall pattern of convection." @default.
- W2007119736 created "2016-06-24" @default.
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- W2007119736 date "1997-05-01" @default.
- W2007119736 modified "2023-10-18" @default.
- W2007119736 title "External boundaries and internal shear bands in granular convection" @default.
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- W2007119736 doi "https://doi.org/10.1103/physreve.55.6016" @default.
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