A prediction method for the size distribution of saltating particles above a mixed‐size bed

Abstract

In aeolian saltation, the sand bed is a mixture of sand particle with a wide range of particle sizes. Generally, the particle size distribution (PSD) of saltating particles is ignored by previous aeolian transport models, which will result in differences between predictions and observations. To better understand the saltation process, a prediction method of the PSD of saltating particles was proposed in this article. The probability of contact between incident sand and bed sand was introduced into the particle‐bed collision process. An artificial PSD of the incident saltating particles was set as the initial condition. A stochastic particle‐bed collision model considering contact probability was then used in each iteration step to calculate a new PSD of saltating particles. Finally, the PSD of saltating particles can be determined when aeolian saltation reaches a steady state (saltation is in a steady state when its primary characteristics, such as horizontal mass flux and the concentration of saltating particles, remain approximately constant over time and distance). Meanwhile, according to the experimental results, a calculation formula for the contact parameter n is given, which characterizes the shielding effect of particles on each other. That is, if soil PSD and friction velocity were given, the PSD of saltating particles can be determined. Our results do not depend on the initial conditions, and the predicted results are consistent with the experimental results. It indicated that our method can be used to determine the PSD of saltating particles. © 2020 John Wiley & Sons, Ltd.

Characterization of Wind‐Blown Sand With Near‐Wall Motions and Turbulence: From Grain‐Scale Distributions to Sediment Transport

“…At present, the limitations of experimental measurements and numerical simulation make it impossible to accurately describe the movement behavior of particles, either considering only the two‐dimensional movement (Liu & Bo, 2020; Rumpel, 1985), or ignoring the influence of particle motions very close to the wall (Dong et al., 2004; Willetts & Rice, 1986) and turbulence (Bo et al., 2017; Fu et al., 2014). Here, we simulate aeolian saltation in a turbulent boundary layer using RANS/LES and the three‐dimensional stochastic particle‐bed collision model.…”