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Aeolian saltation threshold: the effect of density ratio
Authors:JAMES D. IVERSEN  RONALD GREELEY  JOHN R. MARSHALL  JAMES B. POLLACK
Affiliation:Department of Aerospace Engineering, Iowa State University, Ames, IA 50011, U.S.A.;Department of Geology, Arizona State University, Tempe, AZ 85287, U.S.A.;NASA, Ames Research Center, Moffett Field, CA 94035, U.S.A.
Abstract:Saltation threshold data from three wind tunnels and from hydraulic flumes are presented to show that the dimensionless threshold friction speed for small particles is a continuous function of particle-to-fluid-density ratio. In addition, the dimensionless threshold speed is a function of the grain-friction Reynolds number and an interparticle force term. The variation with density ratio seems to be due to the relative energy with which particles impact other particles to initiate saltation.
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