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TURBULENCE IN WIND TURBINE WAKE: EFFECT OF ATMOSPHERIC FORCINGS

机译:涡轮风中的湍流:大气强迫的影响

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Large eddy simulation (LES) is used as a tool to understand the near-wake effects of large 5-MW, 3-blade horizontal-axis wind turbines (WT) in convective atmospheric boundary layer (ABL). The simulations are performed for two inline WT separated by distance of 2.5D (D is diameter of the rotor) in unstable ABL so that the downstream WT is operated under the wake of the upstream WT. The flow characteristics are analyzed in the wake regions behind WT to understand the flow physics. Tip and root vortices undergo vortex merging due to instability. Turbulent mixing layer that develops in the wake region is stronger for the downstream WT. The rate of growth/decay of the mean velocity and turbulence is much higher for WT2 than WT1. The time evolution of the wake of WT1 and WT2 revealed additional wake induced shear that contributes to faster turbulence diffusion which results in shrinking of the shear layer (in height) downstream. The average power output of WT2 is 40% lower than WT1 during unstable stratified atmospheric conditions.
机译:大型涡流仿真(LES)用作理解大型5-MW,3叶水平轴风力涡轮机(WT)在对流大气边界层(ABL)中的近醒来的效果的工具。在不稳定的ABL中,通过2.5D(D是转子的直径)分开的两个内联WT进行模拟,使得下游WT在上游WT之后操作。在WT后面的唤醒区域中分析流动特性以了解流物理学。提示和根涡流由于不稳定而经过涡旋合并。在唤醒区域中发育的湍流混合层对于下游wt较强。对于WT1而言,平均速度和湍流的生长/衰减率远高于WT1。 WT1和WT2次唤醒的时间演变揭示了额外的XEAR诱导的剪切,这有助于更快的湍流扩散,这导致下游的剪切层(高度)收缩。在不稳定的分层大气条件下,WT2的平均功率输出比WT1低40%。

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    《》|2014年|V06BT07A069.1-V06BT07A069.9|共9页
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