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Steady state saltation in air

UNGAR, J. E., HAFF, P. K.·1987·Sedimentology

Abstract

Coupled equations of motion for steady state saltation over an infinite plane are derived and solved for a simplified model of the grain‐surface impact process. Experimentally observed features of the wind velocity profile in saltation are qualitatively reproduced, including a diminution of the sub‐saltation layer mean wind speed, as the friction speed increases. In this model the surface impact velocity of the saltating grains remains relatively constant over a wide range of free‐stream shear stresses, and the grain mass flux increases with friction speed uf* less rapidly than uf3.

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Crossref · 10.1111/j.1365-3091.1987.tb00778.x

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Metadata

Authors
UNGAR, J. E., & HAFF, P. K.
Venue
Sedimentology
Publisher
Wiley
Published
1987-04
Volume
34
Issue
2
Pages
289-299
ISSN
  • 0037-0746 (ISSN-L)
  • 1365-3091
OpenAlex
W2028903105
Cited by
412
References
0
FWCI
11.02
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Steady state saltation in air. https://app.cochat.ai/papers/10.1111/j.1365-3091.1987.tb00778.x
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UNGAR, J. E., & HAFF, P. K. (1987). Steady state saltation in air. Sedimentology. https://doi.org/10.1111/j.1365-3091.1987.tb00778.x

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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