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中文核心期刊

基于改进NSRFG方法的三维山丘绕流风场大涡模拟

LARGE EDDY SIMULATION OF THE WIND FIELD AROUND A THREE-DIMENSIONAL HILL BASED ON AN IMPROVED NSRFG METHOD

  • 摘要: 准确地合成满足大气湍流边界层风场特征的大涡模拟入流脉动风场是当前研究山区地形绕流风场特征的关键问题. 本文在NSRFG(Narrowband Synthesis Random Flow Generation)方法的基础上, 通过对空间调谐因子γj进行空间相关性修正, 同时引入时间尺度修正系数τ0和谱能量修正系数λj, 提出了一种改进的大涡模拟入流脉动合成方法——INSRFG(Improved NSRFG), 并采用该方法进行了三维山丘绕流风场大涡模拟研究, 通过与风洞试验结果及B类风场规范风剖面的对比分析, 验证了改进方法的有效性. 结果表明, 与NSRFG方法相比, 改进后的INSRFG方法模拟得到的脉动风速场, 能更好地满足脉动风速功率谱、时间相关性和空间相关性等湍流风场的基本特征; 在三维山丘绕流风场方面, 基于INSRFG方法模拟得到的山丘的平均和脉动风场, 与风洞试验结果具有更好的一致性, 特别是在流动较为复杂的山丘背风面, 其与风洞试验结果之间的相对误差更小; 与NSRFG方法相比, INSRFG方法模拟得到的山丘周围的流场结构分布更加合理, 特别是在山丘背风面, 能够更好地重现山丘流场结构的多尺度性.

     

    Abstract: The accurate synthesis of the inflow turbulence conditions that satisfy the characteristics of prescribed atmospheric turbulent boundary layer wind fields for large eddy simulation (LES) is the key issue in current research for accurately simulating the feature of the wind flow filed around hilly terrain. Based on the NSRFG (Narrowband Synthesis Random Flow Generation) method, an improved NSRFG (INSRFG) method was put forward by improving the spatial tuning factor γj, introducing the time scale correction factor τ0 and the spectral energy correction coefficient λi. The NSRFG method and INSRFG method were used to generate the inflow turbulence conditions for LES to study the applicability of these two methods within the wind field of hilly terrain. Through comparison of the LES results with those of wind tunnel test and the Category B wind field specifications, the effectiveness of the aforementioned two methods in simulating flow fields around 3D hill was investigated. Compared to the NSRFG method, the turbulence wind filed on the inlet surface obtained through the INSRFG method can better satisfy the requirements of the characteristics of the turbulence wind fields, such as the fluctuating wind speed power spectrum, spatial correlation, and temporal correlation. In comparison with the NSRFG method, the simulated mean and fluctuating wind profiles around the three-dimensional (3D) hill by INSRFG exhibits better consistency with the experimental data. Particularly, relative errors between INSRFG simulation and wind tunnel test are smaller on the leeward side of the hill with complex flow patterns. In addition, the variation characteristic of the flow filed structure around the 3D hill is more reasonable, especially on the leeward side of the hill where the multi-scale flow field structure can be better reproduced by the INSRFG method.

     

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