Abstract Entrainment of solid particles by gas jets discharged downwards through slotted nozzles into bubble-free beds of fluidized particles is considered. The gas flow in the jet is calculated for irrotational flow, using a correlation established previously for slot opening as a function of operating variables. The momentum boundary layer thickness and shear stress at the horizontal interface between jet and particles are then calculated by integral boundary layer analysis. The calculated shear stress distributions are consistent with measurements of the momentum of bed particles caused to saltate by the jet, and explain the dependence of particle movement on the various operating variables. The results provide a direct confirmation of a hypothesis due to Owen on the mechanism of saltation.
[1]
W. S. Chepil,et al.
DYNAMICS OF WIND EROSION: II. INITIATION OF SOIL MOVEMENT
,
1945
.
[2]
L. Massimilla,et al.
The structure of bubble-free gas fluidized beds of fine fluid cracking catalyst particles
,
1972
.
[3]
P. Saffman.
The lift on a small sphere in a slow shear flow
,
1965,
Journal of Fluid Mechanics.
[4]
H. Schlichting.
Boundary Layer Theory
,
1955
.
[5]
R. Bagnold,et al.
The Physics of Blown Sand and Desert Dunes
,
1941
.
[6]
S. Frankel.
Convergence rates of iterative treatments of partial differential equations
,
1950
.
[7]
P. R. Owen,et al.
Saltation of uniform grains in air
,
1964,
Journal of Fluid Mechanics.