Sand Emission Rate Study in Wind Tunnel by Particle Image Velocimetry
Sand emission rate is important parameter in study aeolian sand movement, wind erosion and dust prediction model. Wind tunnel experiments were carried out to measure the sand emission rate along the windstream by Particle Image Velocimetry. The results suggest that the sand emission rate exponential increase rapidly with increasing wind speed. We divide sand particle into two parts: one is upward movement sand grains; the other is downward movement sand grains. The numbers of these two kinds’ particles exponential decrease with increasing height. Sand emission rate and sand fall rate increases with the fetch length.
Wind tunnel Sand flow Sand emission rate Fetch length
Xiaohui Lv Lei Guo Ning Huang
Key Laboratory of Mechanics on Disaster and Environment in Western China,The Ministry of Education of China,Lanzhou,730000
国际会议
西安
英文
973-979
2011-08-17(万方平台首次上网日期,不代表论文的发表时间)