Abstract
The viscosity of a dense suspension has contributions from hydrodynamics and particle interactions, both of which depend upon the flow-induced arrangement of particles into fragile structures. Here, we study the response of nearly hard sphere suspensions to oscillatory shear using simulations and experiments in the athermal, non-inertial limit. Three distinct regimes are observed as a function of the strain amplitude gamma(0). For gamma(0) <10(-1), initially non-contacting particles remain separated and the suspension behaves similarly to a Newtonian fluid, with the shear stress proportional to the strain rate, and the normal stresses close to zero. For gamma(0) > 10(1), the microstructure becomes well-established at the beginning of each shear cycle and the rheology is quasi-Newtonian: the shear stress varies with the rate, but flow-induced structures lead to non-zero normal stresses. At intermediate gamma(0), particle-particle contacts break and reform across entire oscillatory cycles, and we probe a non-linear regime that reveals the fragility of the material. Guided by these features, we further show that oscillatory shear may serve as a diagnostic tool to isolate specific stress contributions in dense suspensions, and more generally in those materials whose rheology has contributions with both hydrodynamic and non-hydrodynamic origin.
Original language | English |
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Pages (from-to) | 3664-3674 |
Number of pages | 11 |
Journal | Soft Matter |
Volume | 13 |
Issue number | 19 |
Early online date | 28 Apr 2017 |
DOIs | |
Publication status | Published - 21 May 2017 |
Keywords / Materials (for Non-textual outputs)
- NON-BROWNIAN SUSPENSIONS
- SHEARED SUSPENSIONS
- GRANULAR-MATERIALS
- SELF-DIFFUSION
- MODEL
- FLOW
- RHEOMETERS
- DYNAMICS
- SEQUENCE
- SOLIDS