4.5 Article

Non-steady wind turbine response to daytime atmospheric turbulence

Publisher

ROYAL SOC
DOI: 10.1098/rsta.2016.0103

Keywords

field experiment; atmospheric turbulence; large-eddy simulation; actuator line methodology

Funding

  1. US Department of Energy's Office of Energy Efficiency and Renewable Energy (EERE)
  2. Penn State Applied Research Laboratory
  3. Penn State Cyber Science Institute (CSI)
  4. Penn State Institutes of Energy and the Environment (PSIEE)
  5. Penn State Departments of Aerospace Engineering, and Mechanical and Nuclear Engineering

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Relevant to drivetrain bearing fatigue failures, we analyse non-steady wind turbine responses from interactions between energy-dominant daytime atmospheric turbulence eddies and the rotating blades of a GE 1.5MW wind turbine using a unique dataset from a GE field experiment and computer simulation. Time-resolved local velocity data were collected at the leading and trailing edges of an instrumented blade together with generator power, revolutions per minute, pitch and yaw. Wind velocity and temperature were measured upwind on a meteorological tower. The stability state and other atmospheric conditions during the field experiment were replicated with a large-eddy simulation in which was embedded a GE 1.5MW wind turbine rotor modelled with an advanced actuator line method. Both datasets identify three important response time scales: advective passage of energy-dominant eddies (approximate to 25-50 s), blade rotation (once per revolution (1P), approximate to 3 s) and sub-1P scale (< 1 s) response to internal eddy structure. Large-amplitude short-time ramp-like and oscillatory load fluctuations result in response to temporal changes in velocity vector inclination in the aerofoil plane, modulated by eddy passage at longer time scales. Generator power responds strongly to large-eddy wind modulations. We show that internal dynamics of the blade boundary layer near the trailing edge is temporally modulated by the non-steady external flow that was measured at the leading edge, as well as blade-generated turbulence motions. This article is part of the themed issue 'Wind energy in complex terrains'.

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