Bulletin of the American Physical Society
71st Annual Meeting of the APS Division of Fluid Dynamics
Volume 63, Number 13
Sunday–Tuesday, November 18–20, 2018; Atlanta, Georgia
Session G08: Multiphase Flows: Particle-Laden Flows I
10:35 AM–12:45 PM,
Monday, November 19, 2018
Georgia World Congress Center
Room: B213
Chair: Greg Voth, Wesleyan University
Abstract ID: BAPS.2018.DFD.G08.5
Abstract: G08.00005 : Dispersion of Rock- and Coal-Dust in Stratified Dust Layers*
11:27 AM–11:40 AM
Presenter:
Shuyue Lai
(Univ of Maryland-College Park)
Authors:
Shuyue Lai
(Univ of Maryland-College Park)
Ryan Houim
(University of Florida)
Elaine S Oran
(Univ of Maryland-College Park)
Numerical simulations of a shock wave passing over layered rock and coal investigated whether and how the presence of rock effects the entrainment of coal in an explosion. We use a multifluid granular flow model based on the Kinetic Theory for Granular Flow (KTGF) and account for multiple particle types with a binning approach. More specifically, we consider the dispersal of coal and rock dust under the action of a Mach 1.4 shock wave. The rock and coal particles have a density of 2680 kg/m3 and 1330 kg/m3, and a diameter of 15 μm and 30 μm, respectively. When a thin layer of rock dust is initially placed on top of a thicker layer of coal particles, entrainment of the coal dust behind the shock wave is suppressed. Increasing the thickness of the rock dust shows that only the top 2-3 mm of the rock is entrained, and particles in the bottom layer remain stationary or become slightly compacted. We also performed simulations in which coal dust was initially placed on top of the rock dust. This configuration does not suppress entrainment of the coal particles, and particles in the dispersed region are primarily coal particles. The results are explained on the basis of the forces on the particles.
*This work was supported by NIOSH Grant No. 200-2015-64091.
To cite this abstract, use the following reference: http://meetings.aps.org/link/BAPS.2018.DFD.G08.5
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