Grain size and transport characteristics of non-uniform sand in aeolian saltation

Size frequency distributions of sediment particles in a wind tunnel containing a bed of non-uniform sand are investigated by re-interpreting existing experimental data using particle-size analysis. Each particle sample is classified into one of eight groups according to its size grading. The analysi...

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Bibliographic Details
Published in:Geomorphology (Amsterdam, Netherlands) Netherlands), 2008-08, Vol.100 (3), p.484-493
Main Authors: Li, Z.S., Feng, D.J., Wu, S.L., Borthwick, A.G.L., Ni, J.R.
Format: Article
Language:English
Subjects:
Aeolian transport
Earth sciences
Earth, ocean, space
Exact sciences and technology
Frequency distribution
Geomorphology, landform evolution
Marine and continental quaternary
Particle size
Sediment mass flux
Surficial geology
Wind erosion
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Summary:Size frequency distributions of sediment particles in a wind tunnel containing a bed of non-uniform sand are investigated by re-interpreting existing experimental data using particle-size analysis. Each particle sample is classified into one of eight groups according to its size grading. The analysis reveals that the modal shape of the particle-size frequency distributions of the saltating sand at different elevations or longitudinal distances is similar to that of the mixed sand in the bed once the boundary layer is fully developed. The standard deviation of the grain-size frequency distribution increases with increasing elevation above the bed then stays constant, whereas its skewness decreases. The mean grain size decays exponentially with elevation. The aeolian sand mass flux is determined for each size grading at different vertical and horizontal measurement locations. The vertical profile of aeolian horizontal mass flux depends on the size grading. The distribution of the sand transport rate according to the mean grain size in each grading fits the normal distribution. A parameter w i is defined to reflect the likelihood of saltation for sand particles of the i-th size grading, and the mean sand size corresponding to the maximum value of w i is found to be 0.2 mm. In addition, wind velocity strongly influences the magnitudes of the particle-size distribution and the sand mass flux distribution in both vertical and longitudinal directions.
ISSN:0169-555X
1872-695X
DOI:10.1016/j.geomorph.2008.01.016