Discontinuous Shear Thickening of Frictional Hard-Sphere Suspensions
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Abstract
Discontinuous shear thickening (DST) observed in many dense athermal suspensions has proven difficult to understand and to reproduce by numerical simulation. By introducing a numerical scheme including both relevant hydrodynamic interactions and granularlike contacts, we show that contact friction is essential for having DST. Above a critical volume fraction, we observe the existence of two states: a low viscosity, contactless (hence, frictionless) state, and a high viscosity frictional shear jammed state. These two states are separated by a critical shear stress, associated with a critical shear rate where DST occurs. The shear jammed state is reminiscent of the jamming phase of granular matter. Continuous…
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4Topics & keywords
Topics
Keywords
- Dilatant
- Jamming
- Shear (geology)
- Shear rate
- Volume fraction
- Shear stress
- Mechanics
- Materials science
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