| 风沙流和净风场中瞬时水平风速廓线特征比较 |
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| 引用本文： | 高咏晴,亢力强,张军杰,邹学勇,张春来,程宏.风沙流和净风场中瞬时水平风速廓线特征比较[J].中国沙漠,2017,37(1):48-56. |
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| 作者姓名： | 高咏晴 亢力强 张军杰 邹学勇 张春来 程宏 |
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| 作者单位： | 北京师范大学 地表过程与资源生态国家重点实验室/防沙治沙教育部工程研究中心, 北京 100875 |
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| 基金项目： | 国家自然科学基金项目（41330746，41271020） |
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| 摘 要： | 为进一步认识风沙流和净风场中瞬时水平风速廓线特征的异同，在风洞中分别对风沙流和净风场中瞬时水平风速廓线进行了测量，风速采集时间间隔缩短至0.01s，分析了风沙流和净风场中瞬时水平风速、瞬时摩阻风速和瞬时空气动力学粗糙度的变化特征。结果表明：相同来流条件下，风沙流中水平风速脉动强度高于净风场，风沙流中瞬时摩阻风速、瞬时空气动力学粗糙度以及它们的脉动幅度均大于净风场；风沙流和净风场中瞬时摩阻风速概率密度分布均可以表示为正态分布，但其正态分布的特征值却存在一定差别；净风场中瞬时空气动力学粗糙度的概率密度分布表现出单调递减分布，而风沙流中瞬时空气动力学粗糙度的概率密度分布呈现出单峰分布。因此，在相同主流风速下风沙流和净风场中瞬时水平风速廓线特征有明显差别。
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| 关 键 词： | 瞬时水平风速 摩阻风速 空气动力学粗糙度 风沙流 |
| 收稿时间： | 2015-09-10 |
| 修稿时间： | 2015-09-24 |
Comparison of Instantaneous Horizontal Wind Velocity Profile in Aeolian Sand Transport and Clean Air |
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| Gao Yongqing,Kang Liqiang,Zhang Junjie,Zou Xueyong,Zhang Chunlai,Cheng Hong.Comparison of Instantaneous Horizontal Wind Velocity Profile in Aeolian Sand Transport and Clean Air[J].Journal of Desert Research,2017,37(1):48-56. |
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| Authors: | Gao Yongqing Kang Liqiang Zhang Junjie Zou Xueyong Zhang Chunlai Cheng Hong |
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| Institution: | State Key Laboratory of Earth Surface Processes and Resource Ecology/MOE Engineering Center of Desertification and Blown-sand Control, Beijing Normal University, Beijing 100875, China |
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| Abstract: | In order to further understand the instantaneous horizontal wind velocity profile characteristics in aeolian sand transport and clean air, the instantaneous horizontal wind velocity profiles were measured in wind tunnel with sampling time interval of 0.01 s. The characteristics of instantaneous horizontal wind velocity, instantaneous friction velocity and instantaneous aerodynamic roughness in aeolian sand transport and clear air are analyzed. The results show that in the same free-stream wind velocity, the horizontal wind velocity fluctuation intensity in windblown sand movement is stronger than that in clear air. The instantaneous friction velocity, instantaneous aerodynamic roughness and their fluctuation in aeolian sand transport are more than that in clear air. The probability density distribution of instantaneous friction velocity both in aeolian sand transport and clear air obeys the normal distribution, while their eigenvalue is different. The probability density distribution of instantaneous aerodynamic roughness in clear air shows a monotone decreasing distribution, while in aeolian sand transport, a single peak appears in the probability density distribution of instantaneous aerodynamic roughness. Therefore, in the same free-stream wind velocity, the characteristics of instantaneous horizontal wind velocity profile in aeolian sand transport and clean air show an obvious distinction. |
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| Keywords: | instantaneous horizontal wind velocity friction velocity aerodynamic roughness aeolian sand transport |
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