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台灣風場特性與離岸風電技術 - 蔡原祥 助理教授

learnenergy
November 22, 2019

台灣風場特性與離岸風電技術 - 蔡原祥 助理教授

台灣風場特性與離岸風電技術 - 蔡原祥 助理教授

learnenergy

November 22, 2019
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  1. 1 Yuan-Shiang Tsai, Ph.D. 2019/11/22 National Kaohsiung University of Science

    and Technology 台灣風場特性與離岸風電技術 成功大學能源講堂
  2. Outlines ◼ Wind features in Taiwan ◼ Wind measurements ◼

    In terms of power generation and wind turbine safety ◼ Turbulence effects ◼ Extreme winds 2
  3. Wind energy in Taiwan Strait 3 ◼ Potential wind energy

    Shallow water (5-20m) Deep water (20-50m) Potential 9 GW 48 GW feasible 1.2 GW 5 GW From ITRI (2007) ⚫ Taiwan Strait is one of the best sites for wind energy development
  4. Wind patterns in Taiwan 4 Typhoon ◼ Diurnal variation ◆

    Sea-land (land-sea) breeze ◆ Mesoscale and extension for hundred kilometers ◼ Typhoons ◆ Extreme wind conditions ◆ Mesoscale and extension for hundred kilometers Northeast monsoon Southwest monsoon ◼ Seasonal variations ◆ Northeast trade wind ◆ Southwest trade wind ◆ Very large-scale and extension for thousands of kilometers H Winter L Summer
  5. Funnel effect 5 ⚫ Wind speed is increased when passing

    a contract section wind h v1 v2 ◼ Venturi effect ◼ Wind passes a valley
  6. Distribution of wind direction 6 Mar. - May Jun.- Aug.

    Sep. – Nov. Dec.- Feb. Annual ◼ Wind rose offshore of Jhonghua ⚫ Majority of the wind energy from northeast monsoons
  7. Wind-speed variations 7 Typhoons sea-land/land-sea breeze Southwest monsoon ◼ NE

    wind in dominance ◼ SW wind in dominance ⚫ Observed at Yongan Taoyuan ⚫ Dry and cold winds Cold fronts ⚫ Warm and humidity winds abrupt wind increase ⚫ Observed At Singda Harbour
  8. 8 Various scales in winds ✓ Typhoon Wind power Diurnal

    cycle Synoptic scales Turbulence, gusts Spectral gap Time scale Without significant wind energy ◼ Spectrum of Von der Hoven (1956)
  9. Conventional measurements 10 ⚫ Accurate measurements after calibration ⚫ Difficult

    to construct over 100 m ⚫ Not easy to maintain ◼ Meteorological mast cup anemometer wind vane Taiwan generations Corp. IEC 61400-12-1 propeller anemometer Ultrasonic anemometer PTH sensor
  10. 11 ⚫ Easily to measure a greater height (for example

    between 40- 200m) with self-defined different levels ⚫ Ease of installation and maintenance Lidar measurement ◼ Leosphere WindCube v2 200 m 40 m 50 m 60 m 80 m 100 m 120 m 140 m 160 m 180 m
  11. 12 Principle of Lidar measurement Aerosols V fo fo +2f

     Radial velocity • Assuming aerosols moving with wind =   : Doppler frequency shift ◼ Lidar (Light Detect and Ranging )
  12. Wind studies using Lidar 13 ◼ Observation at intertidal zone,

    Hanbour, Changhua 13 ⚫ SW wind measurement (P2) ⚫ NE wind measurement (P1) Observation sites 600 m P1 P2
  13. A wind turbine under wind action Wind Foundation Tower Hub

    Nacelle Blade Rotation Pitch Yaw Waves & currents Power generation Upper part Structural safety Lower part Integration Hub height
  14. Inside the nacelle 17 ◼ Power generator and mechanical components

    Lynn (2012) ⚫ Very import devices to control the wind turbine and power performance, however, installed behind the rotor
  15. Power performance 18 Wind velocity (m/s) Generated power (KW) ◼

    Wind-speed distribution ◼ Power output curves • Wind-Speed distribution • Wind shear (boundary layer) • Turbulence • Wind veer • Inflow direction (horizontal & vertical) ◼ Factors to affect power output Weibull distribution
  16. 19 Verification of power curve ◼ Single point measurement 2-4D

    D: diameter of rotor Hub height Electric power (kW) Hub height wind speed (m/s) IEC 61400-12-1 ◼ Observed power curve ⚫ Wind speed & direction ⚫ Pressure ⚫ Temperature ⚫ Humidity
  17. 20 Size growth of wind turbines 2020 ◼ GE 12

    MW future wind turbine power generation effective power generation =  () = () : power coefficient
  18. As becoming large-scale wind turbines 21 ◼ Importance of wind-speed

    profile (wind shear) ⚫ Wind power estimation ⚫ Wind turbine design- need to know wind loading from the wind shear Approx. 200 m Mean wind profile Wake turbulence turbulence ⚫ Wakes- influence the power generation behind
  19. 22 Formulation of the boundary layer ◼ Logarithmic law (neutral

    stability) () = ∗ : surface roughness length ∗ : friction velocity () ( ) = ( ) ◼ Power law : power exponent  =0.14 for a flat terrain, 0.11 over the sea ◼ Both profiles are used for international standards IEC for wind turbine designs ⚫ for the surface layer approximately below 100 m
  20. Jet-like profiles 23 ◼ Observed at Hanbour using the Lidar

    ⚫ NE wind ⚫ SW wind ⚫ Sometimes different from conventional profiles
  21. Wakes in the wind farm 24 Horns Rev Offshore Wind

    Farm, Denmark (http://i.imgur.com/qruVcnu.jpg /)
  22. 25 Wake measurements ◼ Observations nearby Gaomei Wetland, Taichung ◼

    Wind-speed profiles ◼ Wind-direction profiles
  23. 27 Intermittency of wind ◼ Significant fluctuations in natural atmospheric

    airflow Turbulence intensity I=U  /U ◼ Pitch control ◼ Decrease of power generation abrupt wind increase
  24. 28 Outputs varying with wind fluctuations ◼ NERL 5 MW

    reference wind turbine dynamic behaviour wind speed (m/s) Gen power (kw) Gen toque (N/m) Pitch (deg) Lackner (2009)
  25. IEC international standard ◼ IEC 61400-1, wind turbine classes 29

    Vr: the reference wind speed averaged over 10 minute ◼ Turbulence standard deviation (NTM model) ◼ Turbulence intensity (NTM model)
  26. To have better control 30 upwind downwind wind wind ⚫

    Following the wind passively ⚫ Flexible material ⚫ However, strong turbulence effect ◼ Upwind and downwind wind turbine
  27. Nacelle wind Lidar 31 ◼ Development of nacelle wind Lidar

    FREA ( https://www.aist.go.jp/fukus hima/en/unit/WPT_e.html) ◼ Prototype
  28. 34 Impact of typhoon ◼ Typhoon Dujuan (2015) observed at

    Hsingda Harbour ⚫ Wind direction ⚫ Wind speed approaching leaving ⚫ Wind direction rotation 180o in a day , depending on the typhoon moving speed. ⚫ Have to carefully consider yaw control
  29. 36 Typhoon wind-speed profile ⚫ Power law Typhoon approaching Typhoon

    leaving =0.18 =0.24 ⚫ Log law 100 m Significant Coriolis effect Surface friction effect Tsai, Miau, Yu, and Chang (2019), Boundary Layer Meteorology
  30. Waves induced by wind 38 ⚫ Wave patterns over the

    sea are highly correlated to winds NW wind SW wind NW wind SW wind Typhoon ◼ Buoy observation Typhoon
  31. 39 Structural safety ⚫ Parameters over the sea under typhoon

    conditions are not fully understood. (NCREE 2018)
  32. Summary 40 ◼ Long-term observations are needed. ◼ Required to

    validate the consistency of wind and wave characteristics between Europe experiences and Taiwan. ◼ Aware of typhoon wind effect on offshore wind farm.