沟谷坡面风沙起动规律研究

THE INITIATION THRESHOLDS OF BLOWN SAND OVER THE SLOPE

  • 摘要: 根据坡面风沙受力情况,以滚动模式建立了坡面风沙起动的风速公式. 计算分析了相同风向条件下不同坡度风沙的起动风速和相同坡度条件下不同风向风沙的起动风速,并与平面风沙起动计算风速和实测风速进行了比较. 计算分析表明,在风向一定时,坡面风沙更容易起动,风沙起动速率随着坡度的变陡而变小. 在坡度一定时,风沙起动风速受到风向的影响很大,起动风速随风力与水平面垂线夹角的增大而增大. 与平面相比,当风力与水平面垂线夹角小于90o时,坡面风沙起动流速比平面为小. 在当风力与水平面垂线夹角大于90o时,起动风速比平面为大. 当坡面为平面时,风沙起动公式与平面拜格诺起动公式完全一致.

     

    Abstract: Based on the force acting on the wind-blown sedimentover the slope, a formula for the threshold velocity isderived. The threshold wind velocity for different slope angles in thesame wind direction andfor different wind directionsat same slope angle are calculated. They are compared with the threshold wind velocityat 0o slope angle. The results show that in the same wind direction, thethreshold wind velocity over a slope is smaller thanthat on a plane. The threshold wind velocity on a slopevaries with the wind direction. When the slope angle is zero,the formula is identical to the Bagnold formula.

     

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