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Measurement and simulation of sand saltation movement under fluctuating wind in a natural field environment

机译:自然场环境下风沙波动下沙盐运动的测量与模拟

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Extensive research on the near surface movement of sand particles has focused on wind tunnel experiments, theoretical analysis, and numerical simulation of sand saltation under ideal and controllable conditions. Most field observations are results on the average rate of sand transport over some hours or the whole day. However, researchers found recently that the effect of turbulent characteristics of near surface wind in real atmospheric boundary layers on the sand transport rate was obvious. The turbulent characteristics would cause a significant discrepancy between field observation and simulation of sand transport rate. In this work, a field experiment in a real-time system was designed to synchronously measure physical quantities, such as fluctuating wind velocity in the near surface region, sand transport intensity, temperature, and humidity, with the frequency of 1 Hz, at two points on a homogeneous flat sand surface located in the Minqin area, which is between the edges of the Badain Jaran Desert and the Tengger Desert. The relationship between the saltation events and some physical properties, such as the fluctuating wind velocity, temperature, and humidity, was studied. On the basis of the field observation results, a numerical model was developed to simulate sand movement under the fluctuating wind. The overall features of the experimental measurements were reproduced by simulation.
机译:沙粒近表面运动的广泛研究集中在理想条件和可控条件下的风洞实验,理论分析和沙盐形成的数值模拟。大部分现场观察都是在几个小时或一整天的平均砂传输速率的结果。但是,研究人员最近发现,在实际大气边界层中近地表风的湍流特征对砂的输运速度的影响是显而易见的。湍流特征将导致实地观测与沙运速率模拟之间的显着差异。在这项工作中,设计了一个实时系统中的野外实验来同步测量物理量,例如在近地表区域中风速的波动,砂子的输送强度,温度和湿度(频率为1 Hz)在两个点位于民勤地区的均质平坦砂土表面上,位于巴丹吉林沙漠和腾格里沙漠的边缘之间。研究了盐分事件与某些物理特性(例如风速,温度和湿度的波动)之间的关系。根据实地观测结果,建立了数值模型来模拟风沙在动荡下的运动。通过模拟再现了实验测量的总体特征。

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