论文标题
大气边界层偏航风力涡轮机下游的反向旋转涡流的产生和衰减
Generation and decay of counter-rotating vortices downstream of yawed wind turbines in the atmospheric boundary layer
论文作者
论文摘要
需要对控制由偏航风力涡轮机产生的反旋转涡流对(CVP)产生和衰减的主要机制的定量理解,以充分实现偏视风电场功率最大化和调节的潜力。来自湍流大气边界层中的偏航风力涡轮机的大型涡模拟(LES)的观测以及飞机尾随涡流文献的概念为脱落涡流和循环的模型提供了模型。该模型是通过分析涡度传输方程的简化形式的分析整合形成的。基于涡流粘度方法,它使用边界层摩擦速度作为速度尺度和涡度分布的宽度本身作为长度尺度。与广泛使用的Jensen模型用于风电场中的尾流不足演化一样,我们的分析表达式不需要昂贵的微分方程数值整合。预测的最大涡度和总循环的下游衰减与LES结果非常吻合。我们还表明,涡度长度刻度随下游距离线性增长,并找到了最大涡度衰减的几个功率定律。这些结果支持以下观点:CVP的衰减主要取消通过交叉扩散在尾流对称线处的涡度逐渐取消。
A quantitative understanding of the dominant mechanisms that govern the generation and decay of the counter-rotating vortex pair (CVP) produced by yawed wind turbines is needed to fully realize the potential of yawing for wind farm power maximization and regulation. Observations from large eddy simulations (LES) of yawed wind turbines in the turbulent atmospheric boundary layer and concepts from the airplane trailing vortex literature inform a model for the shed vorticity and circulation. The model is formed through analytical integration of simplified forms of the vorticity transport equation. Based on an eddy viscosity approach, it uses the boundary layer friction velocity as the velocity scale and the width of the vorticity distribution itself as the length scale. As with the widely used Jensen model for wake deficit evolution in wind farms, our analytical expressions do not require costly numerical integration of differential equations. The predicted downstream decay of maximum vorticity and total circulation agree well with LES results. We also show that the vorticity length scale grows linearly with downstream distance and find several power laws for the decay of maximum vorticity. These results support the notion that the decay of the CVP is dominated by gradual cancellation of the vorticity at the line of symmetry of the wake through cross-diffusion.