Abstract
The evolution of granular shear flow is investigated as a function of height in a split-bottom Couette cell. Using particle tracking, magnetic-resonance imaging, and large-scale simulations, we find a transition in the nature of the shear as a characteristic height H* is exceeded. Below H* there is a central stationary core; above H* we observe the onset of additional axial shear associated with torsional failure. Radial and axial shear profiles are qualitatively different: the radial extent is wide and increases with height, while the axial width remains narrow and fixed. © 2006 The American Physical Society.
| Original language | English |
|---|---|
| Journal | Physical Review Letters |
| Volume | 96 |
| Issue number | 3 |
| DOIs | |
| State | Published - Jan 27 2006 |
| Externally published | Yes |
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