Aranson IS, Tsimring LS. Continuum theory of partially fluidized granular flows.
PHYSICAL REVIEW E 2002;
65:061303. [PMID:
12188712 DOI:
10.1103/physreve.65.061303]
[Citation(s) in RCA: 127] [Impact Index Per Article: 5.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/19/2001] [Revised: 01/18/2002] [Indexed: 11/07/2022]
Abstract
A continuum theory of partially fluidized granular flows is developed. The theory is based on a combination of the equations for the flow velocity and shear stresses coupled with the order-parameter equation which describes the transition between the flowing and static components of the granular system. We apply this theory to several important granular problems: avalanche flow in deep and shallow inclined layers, rotating drums, and shear granular flows between two plates. We carry out quantitative comparisons between the theory and experiment.
Collapse