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中国沙漠 ›› 2020, Vol. 40 ›› Issue (3): 127-134.DOI: 10.7522/j.issn.1000-694X.2019.00102

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风沙流中跃移沙粒冲击速度和角度联合概率分布风洞实验

肖锋军1, 董治宝1, 郭烈锦2, 王跃社2, 李德标3   

  1. 1. 陕西师范大学 地理科学与旅游学院, 陕西 西安 710119;
    2. 西安交通大学 动力工程多相流国家重点实验室, 陕西 西安 710049;
    3. 西安特种设备检验检测院, 陕西 西安 710065
  • 收稿日期:2019-10-01 修回日期:2019-11-13 出版日期:2020-05-20 发布日期:2020-06-09
  • 作者简介:肖锋军(1984-),男,陕西西安人,博士,讲师,主要从事风沙物理学研究。E-mail:xiaofengjun@snnu.edu.cn
  • 基金资助:
    国家自然科学基金项目(41601002);中国博士后科学基金项目(2017M623115);陕西省自然科学基金项目(2018JQ4010)和中央高校基本科研基金项目(GK201903077)

Experimental study on the joint probability distribution of impacting speed and angle of saltating sand grains in a wind tunnel

Xiao Fengjun1, Dong Zhibao1, Guo Liejin2, Wang Yueshe2, Li Debiao3   

  1. 1. School of Geography and Tourism, Shaanxi Normal University, Xi'an 710119, China;
    2. State Key Laboratory of Multiphase Flow in Power Engineering, Xi'an Jiaotong University, Xi'an 710049, China;
    3. Xi'an Special Equipment Inspection Institute, Xi'an 710065, China
  • Received:2019-10-01 Revised:2019-11-13 Online:2020-05-20 Published:2020-06-09

摘要: 近地表跃移沙粒速度和角度概率分布是连接风沙运动宏观研究和微观研究的桥梁,对沙粒跃移轨迹和输沙率分布有很大影响。但是,目前跃移沙粒冲击速度概率分布和角度概率分布之间的关系还不明确。使用相位多普勒粒子分析仪(PDPA)测量了风洞沙床面1 mm高度处的跃移沙粒速度,通过分析各冲击速度对应的冲击角度的概率分布研究了沙粒冲击速度和角度的联合概率分布。结果表明:沙粒冲击速度概率分布可用对数正态函数描述,冲击角度概率分布可用指数函数描述;各冲击速度对应的冲击角度都符合指数函数分布,且其衰减速度随冲击速度增加而加快。这表明,冲击速度概率分布和冲击角度概率分布之间具有很强的相关性。最后分别给出了沙粒冲击速度和角度的独立假设概率分布和条件联合概率分布。

关键词: 输沙率, 跃移运动, 沙粒速度, 联合概率分布

Abstract: The velocity distribution of saltating sand grains is the bridge between macroscopic and microscopic aeolian research, which largely affects the saltating trajectory and mass flux profile. However, the relation between probability distribution of impacting speed and that of impacting angle remains unclear. In this paper, velocity of saltating sand grains in wind-blown sand located at 0.001 m above the sand bed was measured using a phase Doppler particle analyzer in a wind tunnel. The joint probability distribution of impacting speed and angle is studied by analyzing the probability distribution of impacting angle under each impacting speed. The results show that the probability distribution of impacting speed can be expressed as a lognormal function, while that of impacting angle follows an exponential function. The probability distribution of impacting angle conditioned for each impacting speed also follows an exponential function, whose slope becomes steeper with increasing impacting speed. This implies that the probability distributions of impacting speed and impacting angle are strongly dependent on each other. In the end, we present functions to describe the independent and conditional joint probability distributions of the impacting speed and angle of saltating sand grains.

Key words: saltating movement, sand speed, joint probability distribution, sand mass flux

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