供稿: 岳高伟;蔺海晓;贾慧娜 | 时间: 2018-12-25 | 次数: |
作者单位:河南理工大学土木工程学院
摘要:针对风沙运动中沙粒旋转这一风沙灾害的重要因素,建立风-沙-温度相互耦合作用的描述风沙运动发展过程的数学模型,数值模拟了风沙运动中沙粒旋转角速度的变化及分布规律.定量分析表明:不同高度处沙粒旋转角速度的分布概率服从单峰非对称分布,峰值呈尖点,且沙粒下旋旋转角速度约400 r/s时沙粒概率密度最大;旋转沙粒起跳后开始上升及快要落地阶段,其旋转速度变化较大.同时,Magnus效应对沙粒平均跃移轨迹、输沙率等风沙运动宏观因素均有显著影响.
基金:河南省重点学科项目(504906);国家自然科学基金项目(51074064);河南理工大学博士基金项目(648376);
DOI:10.16186/j.cnki.1673-9787.2011.05.004
分类号:P425.55
Abstract:Spinning of sands is an important factor in wind-blown sand casualty, so a theoretical model is suggested in this paper to mathematically describe the effect of spinning of sands on the evolution of a wind-blown sand movement, which is considered the coupling interaction among the wind flow, saltating sands, and temperature.The numerical results show that at different height the distribution probabilities of angular speed of sands is single-peaked and asymmetric in wind-blown sand movement, and when the distribution probabilities reaches the maximal value, sands are downward spinning and angular speed reaches 400 r/s.When rotational sands lift-off and will fall the ground, variation of sands angular speed sands are more obvious.Meanwhile, Magnus effect apparently influence the trajectories of saltating sands, the transport rate of sand, and so on.