Open AccessDust resuspension without saltation
Author(s) -
Loosmore Gwen A.,
Hunt James R.
Publication year - 2000
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2000jd900271
Subject(s) - abrasion (mechanical) , flux (metallurgy) , atmospheric sciences , entrainment (biomusicology) , shear velocity , environmental science , atmosphere (unit) , mechanics , wind speed , physics , meteorology , turbulence , materials science , rhythm , acoustics , metallurgy , composite material
Wind resuspension (or entrainment) provides a source of dust and contaminants for the atmosphere. Conventional wind erosion models parameterize dust resuspension flux with a threshold velocity or with a horizontal abrasion flux; in the absence of abrasion the models assume dust flux is transient only. Our experiments with an uncrusted, fine material at relative humidities exceeding 40% show a long‐term steady dust flux in the absence of abrasion, which fits the approximate form: F d = 3.6( u * ) 3 , where F d is the dust flux (in μg/m 2 s), and u * is the friction velocity (in m/s). These fluxes are generally too small to be significant sources of dust in most models of dust emission. However, they provide a potential route to transport contaminants into the atmosphere. In addition, dust release is substantial during the initial transient phase. Comparison with field data suggests that the particle friction Reynolds number may prove a better parameter than u * for correlating fluxes and understanding the potential for abrasion.