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中国沙漠 ›› 2004, Vol. 24 ›› Issue (3): 268-273.

• 论文 • 上一篇    下一篇

不均匀沙起动理论及戈壁风蚀层形成动力学

慕青松, 苗天德, 马崇武   

  1. 兰州大学物理科学与技术学院力学系, 甘肃 兰州 730000
  • 收稿日期:2003-04-28 修回日期:2003-06-04 出版日期:2004-06-20 发布日期:2004-06-20
  • 作者简介:慕青松(1971-),男(汉族),甘肃省静宁县人,讲师,博士,主要研究方向为流体力学、岩土力学和风沙物理学。E-mail:qsmulz@sohu.com
  • 基金资助:
    国家自然科学基金资助项目(10172041); 教育部博士点基金资助项目(20020730020)资助

Threshold Velocity for Mix-sized Sand and Formation Dynamics of Gravel Surface

MU Qing-song, MIAO Tian-de, MA Chong-wu   

  1. Department of Mechanics, School of Physical Science and Technology, Lanzhou University, Lanzhou 730000, China
  • Received:2003-04-28 Revised:2003-06-04 Online:2004-06-20 Published:2004-06-20

摘要: 定义了不均匀沙有别于均匀沙的起动概念, 得出了不均匀沙中各粒径沙具有不同的流体起动风速, 且不等于对应粒径均匀沙流体起动风速的结论, 具体表现为: 不均匀沙中小粒径沙的流体起动风速大于相同粒径均匀沙的流体起动风速, 而其中大粒径沙的流体起动风速又小于相同粒径均匀沙的流体起动风速。然后应用不均匀沙起动风速理论, 讨论了戈壁风蚀层与环境风力之间动态平衡的建立过程。

关键词: 不均匀沙, 流体起动风速, 冲击起动风速

Abstract: Based on analyzing the initiation process of mix-sized sand by wind, a theory for the wind threshold of mix-sized sand is presented, which reveals that the threshold velocity of a large diameter in mix-sized sand is less than the threshold velocity of single-size sand having the same diameter, but the case to a small diameter in mix-sized sand is just converse. Then, using the threshold theory of mix-sized sand, we depict the formation of a gravel surface and the dynamical stabilization between turbulent wind and gravel surface.

Key words: mix-sized sand, fluid threshold velocity, impact threshold velocity

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