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中国沙漠 ›› 2011, Vol. 31 ›› Issue (3): 583-587.

• 国家重点基础研究发展规划 • 上一篇    下一篇

非均匀沙的跃移计算

樊 莉, 武生智   

  1. 兰州大学 西部灾害与环境力学教育部重点实验室/土木工程与力学学院, 甘肃 兰州 730000
  • 收稿日期:2010-12-01 修回日期:2011-03-01 出版日期:2011-05-20 发布日期:2011-05-20

Numerical Computation of Nonuniform Grains Saltation

FAN Li, WU Sheng-zhi   

  1. Key Laboratory of the Ministry of Education for Mechanics on Disaster and Environment in Western China; School of Civil Engineering and Mechanics, Lanzhou University, Lanzhou 730000, China
  • Received:2010-12-01 Revised:2011-03-01 Online:2011-05-20 Published:2011-05-20

摘要: 为研究更加接近实际情况的风沙运动,并为实验研究提供一些理论分析和数值资料,本研究用数值计算的方法模拟了几种不同粒径分布方式相应的风沙跃移运动。分别计算了沙粒为单一粒径,以及粒径数学期望为该值时的伪随机分布和均匀分布共7种情况下的风沙跃移运动。计算结果表明,对于相同风速,气流对单一粒径组成的均匀沙的携带能力较弱,而对由多粒径组成的非均匀沙的携带能力较强。同时,因沙粒粒径组成的改变导致当跃移运动达到饱和时,风沙流饱和层的高度和沙粒的跃移长度、高度均有所变化。

关键词: 非均匀沙, 粒径分布, 输沙量

Abstract: Most of aeolian physics researches focus on field observation of wind blown sand and numerical simulation for saltation of sand grains with the uniform diameter size. Therefore, the numerical study for nonuniform sand grains seems very necessary. In this paper, computational method is employed to simulate saltation movement of sand grains with various diameters. We analyzed the saltation movement of sand particles with seven different particle size distributions respectively. The results show that the air flow has more powerful transporting ability for nonuniform particles than that for uniform particles at the same wind velocity when the average grain diameters are identical. Meanwhile, when saltation movement comes to steady state there exist different saltation heights and lengths including related saturated saltation layer thicknesses for different particle size distributions.

Key words: nonuniform sand grain, particle size distribution, mass flux

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