Rheological regimes in agitated granular media under shear
Olfa D'Angelo, Matthias Sperl, W. Till Kranz

TL;DR
This paper investigates the complex rheological behavior of agitated granular media, revealing that all flow regimes can be unified through two key dimensionless numbers, the Peclet number and shear-to-fluidization power ratio.
Contribution
It introduces a unified constitutive relation that captures all observed rheological regimes of agitated granular media using two dimensionless parameters.
Findings
All rheological regimes are delineated by Peclet number and shear-to-fluidization power ratio.
A single constitutive relation qualitatively and quantitatively describes the flow behaviors.
The study spans five orders of magnitude in shear rate, demonstrating broad applicability.
Abstract
Agitated granular media have a rich rheology: they exhibit Newtonian behavior at low shear rate and density, develop a yield stress at high density, and cross over to Bagnoldian shear thickening when sheared rapidly -- making them challenging to encompass in one theoretical framework. We measure the rheology of air-fluidized glass particles, spanning five orders of magnitude in shear rate. By comparing fluidization-induced to Brownian agitation, we show that all rheological regimes can be delineated by two dimensionless numbers -- the Peclet number, , and the ratio of shear-to-fluidization power, -- and propose a constitutive relation that captures all flow behaviors, qualitatively and quantitatively, in one unified framework.
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Taxonomy
TopicsGeotechnical and Geomechanical Engineering · Granular flow and fluidized beds · Hydraulic Fracturing and Reservoir Analysis
