首页> 外文期刊>Boundary-layer Meteorology >Comparison Between Large-Eddy Simulation and Reynolds-Averaged Navier-Stokes Computations for the MUST Field Experiment. Part II: Effects of Incident Wind Angle Deviation on the Mean Flow and Plume Dispersion
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Comparison Between Large-Eddy Simulation and Reynolds-Averaged Navier-Stokes Computations for the MUST Field Experiment. Part II: Effects of Incident Wind Angle Deviation on the Mean Flow and Plume Dispersion

机译:MUST现场实验的大涡模拟与雷诺平均Navier-Stokes计算之间的比较。第二部分:风向角偏差对平均流量和羽流弥散的影响

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Large-eddy simulations (LES) and Reynolds-averaged Navier-Stokes (RANS) computations of pollutant dispersion are reported for the Mock Urban Setting Test (MUST) field experiment flow. In particular we address the effects of incident wind angle deviation on the mean velocity and on the mean concentration fields. Both computational fluid dynamical methods are assessed by comparing the simulation results with experimental field data. The comparative analysis proposes to relate the plume deflection with the flow channelling effects. The results show that the plume deflection angle varies with the altitude. As the ground is approached the plume is shown to be almost aligned with the street canyon direction and independent of the incident wind directions considered. At higher altitudes well above the obstacles, the plume direction is aligned with the mean wind direction as in dispersion over flat terrain. The near-ground plume deflection is the consequence of a strong channelling effect in the region near the ground. The mean concentration profiles predicted by LES and RANS are both in good qualitative agreement with experimental data but exhibit discrepancies that can be partly explained by the influence of small incident wind angle deviation effects. Compared to RANS, LES predicts a higher channelling and thus a higher deflection of the plume. Results on the fluctuating intensity of the concentration obtained from LES show a satisfactory agreement with experiments. This information is not available from RANS for which only the mean concentration modelling is considered.
机译:针对模拟城市环境测试(MUST)现场实验流程,报告了污染物扩散的大涡模拟(LES)和雷诺平均Navier-Stokes(RANS)计算。特别地,我们解决了入射风角偏差对平均速度和平均浓度场的影响。通过将模拟结果与实验现场数据进行比较,可以评估这两种计算流体动力学方法。比较分析建议将羽流挠度与流道效应联系起来。结果表明,羽流偏转角随海拔高度而变化。当接近地面时,羽流显示与街道峡谷方向几乎对齐,并且与所考虑的入射风向无关。在高于障碍物的更高海拔处,羽流方向与平均风向一致,就像在平坦地形上的散布一样。近地面羽流偏斜是在靠近地面的区域中强烈的窜水效应的结果。 LES和RANS预测的平均浓度分布与实验数据在质量上都吻合,但是显示出差异,这可以部分归因于较小的入射风角偏差效应的影响。与RANS相比,LES预测出较高的窜流,因此羽状流的挠度较高。从LES获得的浓度波动强度的结果与实验表明令人满意。从仅考虑平均浓度建模的RANS无法获得此信息。

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