1. The transition in the sedimentation pattern of a particle cloud.
- Author
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Noh, Y. and Fernando, H. J. S.
- Subjects
- *
VORTEX motion , *PARTICLES - Abstract
Experiments were carried out to study the sedimentation of a two-dimensional particle cloud. When a large number of particles (glass beads) of uniform size are released from a two-dimensional opening into a column of fresh water, the mixture initially descends as a thermal; however, after some time, the particles start settling individually, thus leaving the parent fluid behind. For a given type of particle, the critical depth zc at which this transition occurs, measured from a virtual origin, was found to change as zcws/ν∼(Q/νws)α, with α[bar_over_tilde:_approx._equal_to]0.3, where ws is the terminal velocity of a single particle, ν is the kinematic viscosity, and Q is the total buoyancy of the released particles per unit length. The descending velocity and the spatial growth of the particle cloud were found to depend on its sedimentation characteristics. [ABSTRACT FROM AUTHOR]
- Published
- 1993
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