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Interaction between the atmospheric boundary layer and a standalone wind turbine in Gansu—Part I: Field measurement 被引量:7

Interaction between the atmospheric boundary layer and a standalone wind turbine in Gansu—Part I: Field measurement
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摘要 Experiments and numerical simulations of the wake field behind a horizontal-axis wind turbine are carried out to investigate the interaction between the atmospheric boundary layer and a stand-alone wind turbine. The tested wind turbine(33 k W) has a rotor diameter of 14.8 m and hub height of 15.4 m. An anti-icing digital Sonic wind meter, an atmospheric pressure sensor, and a temperature and humidity sensor are installed in the upstream wind measurement mast. Wake velocity is measured by three US CSAT3 ultrasonic anemometers. To reflect the characteristics of the whole flow field, numerical simulations are performed through large eddy simulation(LES) and with the actuator line model. The experimental results show that the axial velocity deficit rate ranges from 32.18% to 63.22% at the three measuring points. Meanwhile, the time-frequency characteristics of the axial velocities at the left and right measuring points are different. Moreover, the average axial and lateral velocity deficit of the right measuring point is greater than that of the left measuring point. The turbulent kinetic energy(TKE) at the middle and right measuring points exhibit a periodic variation, and the vortex sheet-pass frequency is mostly similar to the rotational frequency of the rotor. However, this feature is not obvious for the left measuring point. Meanwhile, the power spectra of the vertical velocity fluctuation show the slope of-1, and those of lateral and axial velocity fluctuations show slopes of-1 and-5/3, respectively.However, the inertial subranges of axial velocity fluctuation at the left, middle, and right measuring points occur at 4, 7, and7 Hz, respectively. The above conclusion fully illustrates the asymmetry of the left and right measuring points. The experimental data and numerical simulation results collectively indicate that the wake is deflected to the right under the influence of lateral force. Therefore, wake asymmetry can be mainly attributed to the lateral force exerted by the wind turbine on the fluid.
出处 《Science China(Physics,Mechanics & Astronomy)》 SCIE EI CAS CSCD 2018年第9期45-58,共14页 中国科学:物理学、力学、天文学(英文版)
基金 supported by the National Basic Research Program of China(Grant No.2014CB046201) the National Natural Science Foundation of China(Grant Nos.51766009,51566011,51465033,and 51479114) the Thousand Talents Program(Grant No.NSFC-RCUK_EPSRC) the Platform Construction of Ocean Energy Comprehensive Supporting Service(2014)(Grant No.GHME2014ZC01) the High-tech Ship Research Projects Sponsored by MIITC Floating Support Platform Project(Grant No.201622) State Key Laboratory of Ocean Engineering at Shanghai Jiao Tong University
关键词 wind power atmospheric turbulence effects velocity measurements turbulent wakes large-eddy simulations 相互作用 汽轮机 风测量 边界层 大气 速度变化 大旋涡模拟 不对称现象
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