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Investigations of flow field around two-dimensional simplified models with wind tunnel experiments

机译:用风洞实验研究二维简化模型周围的流场

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The effect of topographic features on wind velocity and turbulence intensity was evaluated by conducting wind tunnel experiments with Particle Image Velocimetry (PIV) system. In this study, to simulate the natural wind characteristics, the active turbulence grids and boundary layer generation frame were installed in the wind tunnel. The mean wind velocity, the velocity vector diagram and the turbulence intensity around the two-dimensional single simplified models were investigated. As a result, the flow was separated at the simplified model tip in all cases of models, and the countercurrent flow field was generated at the downstream side. Moreover, the clockwise circulation flow also moved to the upstream side in the case of large radius R. RX was followed by the name given the radius value of X. For the mainstream turbulence intensity, the ranges of high turbulence intensity were z/H < 2.8 for R1 model, z/H < 2.6 for R3 model, z/H < 2.5 for R6 model, z/H < 2.4 for R11 model, z/H < 2.2 for R20 model, z/H < 2.0 for R23 model, z/H < 1.9 for R25 model in the vertical direction. The quantitative measurement results of this paper provided a database for the validation of the wind velocity distributions of atmospheric turbulent flow in the hill and mountain regions. (C) 2019 Elsevier Ltd. All rights reserved.
机译:通过使用粒子图像测速(PIV)系统进行风洞实验,评估了地形特征对风速和湍流强度的影响。在这项研究中,为了模拟自然风特征,在风洞中安装了主动湍流网格和边界层生成框架。研究了二维单一简化模型周围的平均风速,速度矢量图和湍流强度。结果,在所有模型情况下,流在简化模型尖端处被分离,并且在下游侧产生了逆流流场。此外,在大半径R的情况下,顺时针循环流也移至上游侧。RX后面是给定半径X的名称。对于主流湍流强度,高湍流强度的范围为z / H < R1型号为2.8,R3型号为z / H <2.6,R6型号为z / H <2.5,R11型号为z / H <2.4,R20型号为z / H <2.2,R23型号为z / H <2.0对于R25模型,z / H <1.9在垂直方向上。本文的定量测量结果为验证丘陵和山区大气湍流的风速分布提供了一个数据库。 (C)2019 Elsevier Ltd.保留所有权利。

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