Strain is the controlling variable for the transition from a sedimented bed to a suspended state in dense non-Brownian suspensions, captured by a volume-fraction-dependent model that unifies steady and oscillatory shear.
Transport layer structure in intense bed- load
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From Sedimentation to Suspension: Critical Strain as a Predictor of Particle Resuspension Thresholds
Strain is the controlling variable for the transition from a sedimented bed to a suspended state in dense non-Brownian suspensions, captured by a volume-fraction-dependent model that unifies steady and oscillatory shear.