DPTM simulation of aeolian sand ripple

作者：Zheng XiaoJing^*; Bo TianLi; Xie Li

来源：Science in China - Series G: Physics Mechanics and Astronomy , 2008, 51(3): 328-336.

DOI：10.1007/s11433-008-0020-y

• wind-blown sand flux
• aeolian sand ripple
• discrete particle tracing method (DPTM)
• mixed-particle-size
• creep

Aeolian sand ripple and its time evolution are simulated by the discrete particle tracing method (DPTM) presented in this paper. The difference between this method and the current methods is that the former can consider the three main factors relevant to the formation of natural aeolian sand ripples, which are the wind-blown sand flux above the sand bed formed by lots of sand particles with different diameters, the particle-bed collision and after it the rebound and ejection of sand particles in the sand bed, the saltation of high-speed sand particles and the creep of low-speed sand particles, respectively. The simulated aeolian sand ripple is close to the natural sand ripple not only in basic shape and characteristic, particle size segregation and stratigraphy, but also in formation stages. In addition, three important speeds can be obtained by this method, which are the propagation speed of the saturated aeolian sand ripple and the critical frictional wind speeds of emergence and disappearance of sand ripple.

• 出版日期2008-3
• 单位兰州大学