comparison of the actuator line model with fully resolved...
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Institute of Aerodynamics and Gas Dynamics
Comparison of the Actuator Line Model with
Fully Resolved Simulations in Complex
Environmental Conditions
Pascal Weihing, Christoph Schulz,
Thorsten Lutz, Ewald Krämer
• Wake Conference
2017
Complex Terrain
• Effects of orography:
• Inclination, yaw, local over-speed
• Roughness / forest
• Stratification
• Atmospheric turbulence
Offshore
• Atmospheric turbulence
• Stratification
• Coriolis force
• Yaw misalignment
• Wake turbine interaction
Challenges in modeling the flow around wind turbines
Motivation
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Non-uniform velocity distribution in the rotor plane unsteady aerodynamic effects
Accuracy of the ACL in such conditions?
[1]
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Numerical Modeling of Wind Turbines in FLOWer
Fully resolved rotor (FR)
• Boundary layer of the airfoil is resolved 𝑦+ ≈ 1
• Turbine components are separately meshed and integrated
using the overset grid technique
Detailed view into flow phenomena around the rotor
Accurate prediction of loads and power including unsteady
aerodynamic effects without need for further modeling
Disadvantages:
• Time consuming meshing
• High computational effort
Only suitable for simulation of wind farms to a limited extent
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• Effect of the blades on the flow modeled by a momentum source term
𝝏
𝝏𝒕𝑽
𝑾𝒅𝑽 + 𝑭 𝑺
⋅ 𝒏𝒅𝑺 = 𝑺 𝑾 𝒅𝑽𝑽
• Aerodynamic forces: 𝒇𝟐𝑫 =1
2𝜌𝑣𝑟𝑒𝑙
2 𝑐 𝑐𝑙 𝛼 𝒆𝑳, 𝑐𝑑 𝛼 𝒆𝒅
• Iterative calculation of the angle of attack
• Sampling of the velocity upstream of the AL point
• Gaussian smearing 𝑓 = 𝑓2𝐷⊗𝜂𝜖,3𝐷, 𝜂𝜖,3𝐷 =1
𝜖3𝜋3/2exp −
𝑑
𝜖
2
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The Actuator Line Method
Modeling of the rotor
𝜙 = tan−1𝑢𝐴𝐿
𝑣𝐴𝐿 + Ω𝑟 𝑢𝐴𝐿 = 𝑢𝑠𝑎𝑚𝑝 − 𝑢𝑖 d𝑠𝑎𝑚𝑝 𝛼 𝑐𝑎 , Γ Biot-Savart
iteration
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• Calculation of overall drag force using specified
𝑐𝐷 and area
• Break down into volume force increments
• Insert as momentum sink in Navier-Stokes
Equations
• Sinusoidal force to mimic bluff bodies:
𝐹𝑠𝑓 = 𝑘𝑓𝐹𝐷 sin2𝜋𝑆𝑟𝑈∞𝐿
𝑡
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The Actuator Line Method
Modeling of the nacelle
Nacelle wake:
FR ACL 𝑐𝐷 = 0.8 ACL 𝑐𝐷 = 0.8, sin
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• 5M wind turbine located in Alpha-Ventus, Germany
• Diameter 126m
• Hub height: 95m
• Tilt /Cone angle: 6°, -4°
• TSR: 8.5
• Total of 80M cells for FR, 42M cells for ACL, wake: Δ = 1𝑚3
• 100 ACL points, nacelle modeled by source term
• −180° < 𝛼 < 180° polars XFOIL/Viterna
• Higher order WENO scheme in the background mesh
Lower dissipation settings for ACL compared to FR
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caseOffshore
Investigated cases
Overset Meshing
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• 2.4M wind turbine located on an escarpment in Stötten, Germany
• Diameter 109m
• Hub height: 70m
• Tilt /Cone angle: 5°, -2°
• TSR: 6.64
• Total of 180M cells for FR, wake: Δ = 1𝑚3
• 100 ACL points, nacelle also meshed
• −180° < 𝛼 < 180° polars XFOIL/Viterna
• Higher order WENO scheme in the background mesh
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caseTerrain
Investigated cases
Part of the computational domain
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[3]
• WRF and LiDAR based LES simulations by
ForWind using PALM
• Almost neutral stratification
• Wind speed at hub height: 8 m/s
• Turbulence intensity: 4.5%
• Signal made periodic over 60s
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caseOffshore
Inflow Conditions
Velocity profile at the inlet
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• UAV and LiDAR measurements approximated by
• Steady power law profile 𝛼 = 0.14
• Synthetic turbulence by Mann model:
• 𝐿 = 40𝑚; Γ = 3.9; 𝛼𝜖2/3 = 0.035; 𝜎𝑢 = 0.9𝑚/𝑠
• Introduced as body forces with model of Troldborg [2]
• Velocity at hub height 11m/s
• Turbulence intensity ≈ 10%
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caseTerrain
Inflow Conditions
Velocity profile at the turbine
position (LiDAR □; UAV▲) [1]
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caseOffshore
• Linear loading over wide range
• Higher loads of ACL in the outer part
caseTerrain
• Higher loading in the mid part
of the rotor
• Good agreement of ACL and FR
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Loads
Results
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• AoA vs. Lift coefficient
• Unsteady aerodynamic effects
present in the inner and mid portion
• ACL predicts 2D polar as expected
• ACL shows higher lift at lower AoA
XFOIL polars inacurrate
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Unsteady aerodynamics caseOffshore
Results
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Vorticity contour for caseOffshore – FR
Results
• Tilt angle
Drivers of Instability:
+
• Shear +
larger scale
Turbulence
• High TSR
Effects:
• Vortex pairing
• Large scale motion
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Vorticity contour for caseOffshore – ACL
Results
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Instantaneous velocity field: caseTerrain
Investigation of a single wind turbine wake
Wake of the ACL rotor
Wake of the FR turbine
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[3]
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Vorticity contour for caseTerrain
Results
FR
ACL
Drivers of Instability:
+
• Shear +
high level
Turbulence
• Inclination
Effects:
• Quicker disordering
• More homogeneous
turbulence
• Upward deflection
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[3]
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Mean velocity profiles caseOffshore
Results
FR
ACL • “Linear” velocity deficit, with high induction
• Recovery process initiated by turbulent mixing with the surrounding flow
• Wake deflection in vertical direction
• Overall good agreement of ACL and FR
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Standard deviation of velocities caseOffshore
Results
• Higher standard deviation in the mid part of the wake by ACL
• Growing shear layer in the tip region yields higher standard deviation
• Mixing with high kinetic energy fluid from outside for x/R>4
FR
ACL
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Mean velocity profiles caseTerrain
Results
FR
ACL • “Bell”-shaped velocity deficit
• Higher velocity near the ground
• Turbine “footprint” blurred by high ambient turbulence level
• Slight over prediction of deficit by ACL
• Gaussian shaped velocity field for x/R>7
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Standard deviation of velocities caseTerrain
Results
• Higher turbulence levels compared to caseOffshore
• Fluctuations still present near the ground
• Peaks of the tip more pronounced in the horizontal plane
FR
ACL
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Velocity spectra caseOffshore
Results
FR
ACL
• Distinct 3P frequency peaks in the near wake, sharper for ACL
• In the farther wake ACL shows higher to amplitudes due to less dissipative scheme
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x/R=0.1 x/R=6
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Velocity spectra caseTerrain
Results
FR
ACL
• In the near wake the peaks of the ACL are smeared to neighboring frequencies
Vortices are disintegrated by high level of turbulence
• In the farther wake only slightly higher fluctuations in the higher frequencies by ACL
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x/R=0.1 x/R=7
• Comparison of ACL and FR for typical offshore and complex terrain case
• Unsteady aerodynamic effects present
• Wake development offshore determined by operational conditions, shear and large scale
turbulence
• Wake development in complex terrain dominated by inclination and high turbulence
• ACL predicts well:
• Wake instability
• Mean deficit
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Conclusions
• ACL depends on high quality polars
• Seems to over predict fluctuations in the near wake
[1] Schulz C, Hofsäß M, Anger J, Rautenberg A, Lutz T, Cheng P W and Bange J 2016 Journal of
Physics:
[2] Troldborg N, Sørensen J N, Mikkelsen R and Sørensen N N 2014 Wind Energy 17 657–669
[3] Schulz C 2017 Numerische Untersuchungen des Verhaltens von Windenergieanlagen im komplexen
Gelände
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References
phone +49 (0) 711 685-
fax +49 (0) 711 685-
University of Stuttgart
Thank you!
Pascal Weihing
69974
69974
Institut für Aerodynamik und Gasdynamik
Pfaffenwaldring 21
Institute of Aerodynamics and Gas Dynamics
University of Stuttgart 27
Instantaneous velocity field: caseOffshore
Results
Wake of the ACL rotor Wake of the FR turbine
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