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The influence of wind velocity on the size distributions of aerosols generated by the wind erosion of soils

Gillette, Dale A., Blifford, Irving H., Fryrear, D. W.·1974·Journal of Geophysical Research

Abstract

The relationship of the relative size distribution of soil wind erosion aerosols to wind velocity was examined in field measurements and wind tunnel simulations. The ratio of sedimentation velocity to friction velocity ((vertical momentum flux/air density)1/2) at which aerosol particles were significantly affected by settling was larger than 0.12 and smaller than 0.68. The shapes of the size distributions of soil wind erosion aerosols (2 μm < r < 10 μm) were fairly constant with wind speed. This result is evidence that the dominant mechanism of aerosol production by soil erosion is sandblasting of the soil surface.

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Metadata

Authors
Gillette, D. A., Blifford, I. H., & Fryrear, D. W.
Venue
Journal of Geophysical Research
Published
1974-09-20
Volume
79
Issue
27
Pages
4068-4075
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2045469990
Cited by
281
References
0
FWCI
10.05
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: The influence of wind velocity on the size distributions of aerosols generated by the wind erosion of soils. https://app.cochat.ai/papers/10.1029/jc079i027p04068
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Gillette, D. A., Blifford, I. H., & Fryrear, D. W. (1974). The influence of wind velocity on the size distributions of aerosols generated by the wind erosion of soils. Journal of Geophysical Research. https://doi.org/10.1029/jc079i027p04068

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

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.