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Interaction between the atmospheric boundary layer and a standalone wind turbine in Gansu-Part I: Field measurement
Li, DeShun2,3,4; Guo, Tao2; Li, YinRan2,3,4; Hu, JinSen2; Zheng, Zhi2,3,4; Li, Ye5,6,7; Di, YuJia5; Hu, WenRui1; Li, RenNian2,3,4
刊名SCIENCE CHINA-PHYSICS MECHANICS & ASTRONOMY
2018-09
卷号61期号:9
关键词wind power atmospheric turbulence effects velocity measurements turbulent wakes large-eddy simulations
ISSN号1674-7348
DOI10.1007/s11433-018-9219-y
英文摘要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 kW) 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, and 7 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.
资助项目High-tech Ship Research Projects - MIITC Floating Support Platform Project[201622]
WOS研究方向Physics
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:000437173700008
状态已发表
内容类型期刊论文
源URL[http://119.78.100.223/handle/2XXMBERH/32503]  
专题能源与动力工程学院
通讯作者Li, Ye; Hu, WenRui; Li, RenNian
作者单位1.Chinese Acad Sci, Inst Mech, Beijing 100080, Peoples R China
2.Lanzhou Univ Technol, Sch Energy & Power Engn, Lanzhou 730050, Gansu, Peoples R China
3.Gansu Prov Technol Ctr Wind Turbines, Lanzhou 730050, Gansu, Peoples R China
4.Key Lab Fluid Machinery & Syst, Lanzhou 730050, Gansu, Peoples R China
5.Shanghai Jiao Tong Univ, Sch Naval Architecture Ocean & Civil Engn, Shanghai 200240, Peoples R China
6.Shanghai Jiao Tong Univ, Sch Naval Architecture Ocean & Civil Engn, State Key Lab Ocean Engn, Shanghai 200240, Peoples R China
7.Shanghai Jiao Tong Univ, Collaborat Innovat Ctr Adv Ship & Deep Sea Explor, Shanghai 200240, Peoples R China
推荐引用方式
GB/T 7714
Li, DeShun,Guo, Tao,Li, YinRan,et al. Interaction between the atmospheric boundary layer and a standalone wind turbine in Gansu-Part I: Field measurement[J]. SCIENCE CHINA-PHYSICS MECHANICS & ASTRONOMY,2018,61(9).
APA Li, DeShun.,Guo, Tao.,Li, YinRan.,Hu, JinSen.,Zheng, Zhi.,...&Li, RenNian.(2018).Interaction between the atmospheric boundary layer and a standalone wind turbine in Gansu-Part I: Field measurement.SCIENCE CHINA-PHYSICS MECHANICS & ASTRONOMY,61(9).
MLA Li, DeShun,et al."Interaction between the atmospheric boundary layer and a standalone wind turbine in Gansu-Part I: Field measurement".SCIENCE CHINA-PHYSICS MECHANICS & ASTRONOMY 61.9(2018).
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