Aeolian abrasion and modes of fine particle production from natural red dune sands: an experimental study

Article


Bullard, Joanna E., McTainsh, Grant H. and Pudmenzky, Christa. 2004. "Aeolian abrasion and modes of fine particle production from natural red dune sands: an experimental study." Sedimentology. 51 (5), pp. 1103-1125. https://doi.org/10.1111/j.1365-3091.2004.00662.x
Article Title

Aeolian abrasion and modes of fine particle production from natural red dune sands: an experimental study

ERA Journal ID1860
Article CategoryArticle
AuthorsBullard, Joanna E. (Author), McTainsh, Grant H. (Author) and Pudmenzky, Christa (Author)
Journal TitleSedimentology
Journal Citation51 (5), pp. 1103-1125
Number of Pages23
Year2004
Place of PublicationOxford, United Kingdom
ISSN0037-0746
1365-3091
Digital Object Identifier (DOI)https://doi.org/10.1111/j.1365-3091.2004.00662.x
Abstract

A series of experiments was conducted to determine the potential for aeolian abrasion of natural dune sands to produce fine particles (< 125 µm) by (1) the release of resident fines; (2) spalling, chipping and breakage of particles; and (3) the removal of grain surface coatings. Parent samples were obtained from the surfaces of four active continental dunes and abraded using a glass 'test
tube' chamber for up to 120h. The fine particles produced by this abrasion process were trapped at varying time intervals and subject to detailed particle-size analyses using a Coulter Multisizer. The abrasion of untreated parent
samples produced fine particles in one of two main size classes, <10 µm and >50 µm, but when the parent sample was sieved to exclude particles <250 µm, relatively more material in the range 10–50 µm was produced. For unsieved
parent samples, the size range associated with the dominant mode varied according to the length of the abrasion time. The coarsest mode (>63 µm) was dominant during the first 16 h of abrasion, then became less significant and is
thought to be associated with the release of resident fines into suspension. The finest mode (<10 µm) was absent or very weak during the first 16h of abrasion, then became more significant and, in some instances, dominated the
distribution as abrasion continued. Removal of grain surface coatings is the main source of fine material <10 µm, and this may be a significant source of fine material in areas where sands are dominated by subrounded and rounded
particles. By comparison with previous studies of aeolian particle abrasion, these natural dune sands produced very low quantities of fine material (by weight), but their spatial extent makes them potentially a significant source of dust-sized particles at the global scale.

Keywordsaeolian abrasion; dune sands; fine particle production; grain characteristics
ANZSRC Field of Research 2020370999. Physical geography and environmental geoscience not elsewhere classified
410605. Soil physics
410601. Land capability and soil productivity
Public Notes

© 2004 International Association of Sedimentologists.
Permanent restricted access to published version due to publisher copyright policy.

Byline AffiliationsLoughborough University, United Kingdom
Griffith University
Institution of OriginUniversity of Southern Queensland
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