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contributor authorClark, Terry L.
contributor authorList, Roland
date accessioned2017-06-09T14:15:53Z
date available2017-06-09T14:15:53Z
date copyright1971/07/01
date issued1971
identifier issn0022-4928
identifier otherams-15980.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151712
description abstractA numerical experiment on falling particles arranged in zones, with slab symmetry, constant air density, and initially still air is performed whereby single-shed particles are treated by a Lagrangian method and the air motion by an Eulerian method. The results of this study of the zone's dynamics indicate that the zones fall considerably faster than their respective terminal velocity. This additional or convective velocity depends on loading and terminal speed. The spreading velocities, away from the axis of symmetry, appear to be dependent on terminal velocity such that a maximum occurs near the terminal velocity of 4 m sec?1. In all cases considered, the magnitude of the perturbation nonhydrostatic pressure gradient in the vertical is found to be an order of magnitude smaller than the perturbation hydrostatic pressure gradient.
publisherAmerican Meteorological Society
titleDynamics of a Falling Particle Zone
typeJournal Paper
journal volume28
journal issue5
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1971)028<0718:DOAFPZ>2.0.CO;2
journal fristpage718
journal lastpage727
treeJournal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 005
contenttypeFulltext


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