Abstract
Granular packing is often characterized by a linear relationship between packing fraction and dimensionless shear rate. We examine this relationship in simple and complex heterogeneous flow geometries. At high inertial number , we observe that the packing fraction depends approximately linearly on and is seemingly independent of the geometry. However, at low the packing fraction varies nonlinearly with and this variation is dependent on the specific geometry and conditions. This response is analogous to the behavior of the stress ratio , where, at low , depends on the geometry of the system, an effect that is often attributed to nonlocal effects of the granular rheology. We demonstrate that, in steady isochoric flow geometries, the and responses are equivalent and may be determined locally from , even at low . However, in a more complex, nonisochoric geometry, such as a pseudo-two-dimensional hopper, this relationship is not recovered in dense regions. We show that during transient startup in a shear cell and follow a similar response to that seen in these nonisochoric flows. Hence we conclude that the observed discrepancy arises because the hopper is transient in a Lagrangian sense. The simple relationship seen in isochoric flows is insufficient in these more complex systems because of differences in the temporal evolution of the stress and packing fraction.
- Received 28 April 2021
- Accepted 24 June 2022
DOI:https://doi.org/10.1103/PhysRevFluids.7.074304
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