Abstract
Saltating particle concentration variations in the windsand flux on the desertified area have been analyzed. Vertical profiles of the particle concentrations are constructed. Exponential approximations of the saltating particle concentration height profiles have been proposed. For the upper layer of the saltation the relation between the wind velocity and the logarithmic concentration gradient has been received and for the lower layer of the saltation the statistical characteristics of the logarithmic concentration gradient variations have been determined.
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