Abstract
The underlying physics of nonlocal granular flow within quasistatic, cohesive, split-bottom cells have been investigated. The evolution of macroscopic quantities, e.g., nonlocal granular fluidity, with respect to cohesiveness has been analyzed by coupling microscopic-level discrete element method (DEM) simulations with a coarse-graining procedure. As a result, tentative constitutive relations for wet granular flows have been uncovered and discussed.
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