Wall stresses in granular Couette flows of mono-sized particles and binarymixtures

Citation
A. Karion et Ml. Hunt, Wall stresses in granular Couette flows of mono-sized particles and binarymixtures, POWD TECH, 109(1-3), 2000, pp. 145-163
Citations number
26
Categorie Soggetti
Chemical Engineering
Journal title
POWDER TECHNOLOGY
ISSN journal
00325910 → ACNP
Volume
109
Issue
1-3
Year of publication
2000
Pages
145 - 163
Database
ISI
SICI code
0032-5910(20000403)109:1-3<145:WSIGCF>2.0.ZU;2-1
Abstract
Granular shear flows are studied in a gravity-free Couette geometry using a two-dimensional discrete element computer simulation. Upper and lower boun ding walls are flat and frictional and move in opposing directions, while t he right and left boundaries are periodic. Mono-size flows are examined at various concentrations and three different gap widths. Flows of binary mixt ures with diameter ratios of 2, 5, and 10 are investigated as well. Mixture solid fraction ratios of small to large particles range from 0.4 to 5, wit h a constant overall solid fraction of 0.75 in two dimensions. Normal and s hear stresses on the bounding walls are measured for various flow condition s. Both normal and shear stresses increase with solid fraction in same-size flows, and show a dependence on the wall spacing at low concentrations. Sa me-size particle flows show the existence of a critical wall solid fraction at which the granular temperature, strain rate, and stresses increase sudd enly. Stresses in mixture flows with low solid fraction ratios of small to large particles are higher than for the mono-size system. For a fixed overa ll solid fraction of 0.75, mixture flow stresses also increase with diamete r ratio of large to small particles. The ratio of shear to normal stress de creases with solid fraction in same-size flows. For mixture flows with cons tant overall solid fraction, the ratio increases with solid fraction ratio for size ratios of 5 and 10; it remains relatively constant in flows with a size ratio of only 2. (C) 2000 Elsevier Science S.A. All rights reserved.