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Granular Matter: How Structure Determines Response Far From Equilibrium

Subject Area Statistical Physics, Nonlinear Dynamics, Complex Systems, Soft and Fluid Matter, Biological Physics
Term from 2017 to 2022
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 335058789
 
Final Report Year 2023

Final Report Abstract

Fluidized granular media are pervasive in nature and industry. Avalanches, land slides and the transport of agricultural grains or construction sand are examples of processes that would benefit from a detailed understanding of the granular flow behavior. Despite its importance, a comprehensive granular rheology had been missing so far. In this project, I developed the Granular Integration Through Transients (GITT) formalism and validated it by dedicated experiments in a state of the art commercial rheometer. In a nutshell, granular rheology is captured by a few time scales: (i) Newtonian behavior is observed when the shear rate is slow compared to the structural relaxation rate. Shear thinning and in the Taylor-Couette geometry, shear banding, is found for higher shear rates until shear heating dominates over fluidization and the rheology follows Bagnold scaling. Promising initial results for a compatible description of the jamming transition and for the use in continuum simulations pave the way for future work. In summary, it is indeed the structure in form of the structural relaxation rate that largely determines graular rheology. Including finer details, GITT can also explain the empirical µ(I)-law valid in the Bagnold regime and make quantitative predictions for difficult to measure quantities like the granular temperature.

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