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Effects of Thermal Stability and Incoming Boundary-Layer Flow Characteristics on Wind-Turbine Wakes: A Wind-Tunnel Study

机译:热稳定性和传入边界层流动特性对风力涡轮机尾流的影响:风洞研究

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Wind-tunnel experiments were carried out to study turbulence statistics in the wake of a model wind turbine placed in a boundary-layer flow under both neutral and stably stratified conditions. High-resolution velocity and temperature measurements, obtained using a customized triple wire (cross-wire and cold wire) anemometer, were used to characterize the mean velocity, turbulence intensity, turbulent fluxes, and spectra at different locations in the wake. The effect of the wake on the turbulence statistics is found to extend as far as 20 rotor diameters downwind of the turbine. The velocity deficit has a nearly axisymmetric shape, which can be approximated by a Gaussian distribution and a power-law decay with distance. This decay in the near-wake region is found to be faster in the stable case. Turbulence intensity distribution is clearly non-axisymmetric due to the non-uniform distribution of the incoming velocity in the boundary layer. In the neutral case, the maximum turbulence intensity is located above the hub height, around the rotor tip location and at a distance of about 4–5.5 rotor diameters, which are common separations between wind turbines in wind farms. The enhancement of turbulence intensity is associated with strong shear and turbulent kinetic energy production in that region. In the stable case, the stronger shear in the incoming flow leads to a slightly stronger and larger region of enhanced turbulence intensity, which extends between 3 and 6 rotor diameters downwind of the turbine location. Power spectra of the streamwise and vertical velocities show a strong signature of the turbine blade tip vortices at the top tip height up to a distance of about 1–2 rotor diameters. This spectral signature is stronger in the vertical velocity component. At longer downwind distances, tip vortices are not evident and the von Kármán formulation agrees well with the measured velocity spectra.
机译:进行风洞实验以研究在中性和稳定分层条件下将模型风轮机置于边界层流中后的湍流统计。使用定制的三线制(交叉线和冷线)风速仪获得的高分辨率速度和温度测量值用于表征尾流中不同位置的平均速度,湍流强度,湍流和光谱。发现尾流对湍流统计的影响一直延伸到涡轮顺风向20处。速度赤字具有近似轴对称的形状,可以通过高斯分布和幂律随距离的衰减来近似。在稳定的情况下,发现近苏醒区的这种衰减更快。由于边界层中入射速度的不均匀分布,湍流强度分布显然是非轴对称的。在中性情况下,最大湍流强度位于轮毂高度上方,围绕转子尖端位置,并且距转子直径约4–5.5,这是风电场中风力涡轮机之间的常见间距。湍流强度的增加与该区域的强剪切和湍动能的产生有关。在稳定的情况下,进入流中的较强剪切力会导致湍流强度稍强一些和更大一些,该区域会在涡轮机位置顺风方向的3到6个转子直径之间延伸。流向和垂直速度的功率谱显示出涡轮叶片尖端涡旋在顶部尖端高度直至转子直径约为1-2的距离时具有强烈的特征。该频谱特征在垂直速度分量上更强。在较长的顺风距离处,尖端涡旋不明显,冯·卡尔曼公式与测得的速度谱吻合得很好。

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