Flow regime transitions in dense non-Brownian suspensions: rheology, microstructural characterisation and constitutive modelling
arXiv:1409.1041 · doi:10.1103/PhysRevE.91.012201
Abstract
Shear flow of dense, non-Brownian suspensions is simulated using the discrete element method, taking particle contact and hydrodynamic lubrication into account. The resulting flow regimes are mapped in the parametric space of solid volume fraction, shear rate, fluid viscosity and particle stiffness. Below a critical volume fraction , the rheology is governed by the Stokes number, which distinguishes between viscous and inertial flow regimes. Above , a quasistatic regime exists for low and moderate shear rates. At very high shear rates, the dependence is lost and soft particle rheology is explored. The transitions between rheological regimes are associated with the evolving contribution of lubrication to the suspension stress. Transitions in microscopic phenomena such as inter-particle force distribution, fabric and correlation length are found to correspond to those in the macroscopic flow. Motivated by the bulk rheology, a constitutive model is proposed combining a viscous pressure term with a dry granular model presented by Chialvo, Sun and Sundaresan [Phys. Rev. E. \textbf{85}, 021305 (2012)]. The model is shown to successfully capture the flow regime transitions.
References in corpus (13)
- On dense granular flows
- A constitutive law for dense granular flows
- Rheophysics of dense granular materials : Discrete simulation of plane shear flows
- Discontinuous Shear Thickening of Frictional Hard-Sphere Suspensions
- Shear thickening, frictionless and frictional rheologies in non-Brownian suspensions
- Bridging the rheology of granular flows in three regimes
- Transition from viscous to inertial regime in dense suspensions
- Microscopic mechanism for the shear-thickening of non-Brownian suspensions
- Microfluidic rheology of soft colloids above and below jamming
- Flow of wet granular materials
- Shear thickening and migration in granular suspensions
- Thinning or thickening? Multiple rheological regimes in dense suspensions of soft particles
- Long Range Correlation in Granular Shear Flow II: Theoretical Implications
Cited by in corpus (18)
- Hydrodynamic and contact contributions to shear thickening in colloidal suspensions
- The physics of sediment transport initiation, cessation, and entrainment across aeolian and fluvial environments
- A mechanical erosion model for two-phase mass flows
- Shear thickening regimes of dense non-Brownian suspensions
- The physics of dense suspensions
- The influence of surface roughness on the rheology of immersed and dry frictional spheres
- Local Rheology Relation with Variable Yield Stress Ratio across Dry, Wet, Dense, and Dilute Granular Flows
- Merging fluid and solid granular behavior
- Two-scale evolution during shear reversal in dense suspensions
- Viscous-inertial transition in dense granular suspension
- Universal friction law at granular solid-gas transition explains scaling of sediment transport load with excess fluid shear stress
- Force transmission and the order parameter of shear thickening
- The non-monotonic shear-thinning flow of two strongly cohesive concentrated suspensions
- Basal force fluctuations and granular rheology: Linking macroscopic descriptions of granular flows to bed forces with implications for monitoring signals
- Extended -rheology for dense suspensions at oscillatory shear flows
- Shear thickening of suspensions of dimeric particles
- Non-monotonic constitutive curves and shear banding in dry and wet granular flows
- Linking particle properties to paste extrusion flow characteristics using discrete element simulations