Page 173 - Wind Energy Handbook
P. 173

UNSTEADY FLOW – DYNAMIC INFLOW                                         147


             the acceleration is independent of yaw angle. The mean acceleration is zero and so
             there is no coupling between the cases.
               The relationship between accelerations and force coefficients is therefore
                                  2             32     3
                                   16              @a 0
                                         0    0           2     3
                                  6  3ð         76  @ô 7
                                  6             76     7     C T
                                  6     32      76     7  6     7
                                  6  0        0  76  @a c  7  ¼ 4  C my 5       (3:207a)
                                  6             76     7
                                  6     45ð     76  @ô 7
                                  4             54     5
                                             32    @a s     C mz  D
                                    0    0
                                             45ð    @ô

                                               @a
                                          [M]      ¼fCg D                       (3:207b)
                                               @ô
             The complete equation of motion combines Equation (3.207) and the steady yaw
             Equation (3.188). The combination is achieved by adding the corresponding force
             coefficients, which means that both equations must be inverted.

                                       @a       1
                                  [M]      þ [L] fag¼fCg D þfCg S                (3:208)
                                       @ô
             The right-hand side of Equation (3.208) can also be determined from blade element
             theory and will be a time-dependent function of the inflow factor. The blade forces
             will vary in a manner determined by the time-varying velocity of the oncoming
             wind and consequent dynamic structural deflections of the necessarily elastic rotor.
             Equation (3.208) applies to the whole rotor disc and the blade element forces need
             to be integrated along the blade lengths.
               Numerical solutions to Equation (3.208) require a procedure for dealing with
             first-order differential equations and the tried and tested fourth-order Runge-Kutta
             method is recommended. Starting with a steady-state solution the progress in time
             of the induced velocity as an unsteady flow passes through the rotor can be tracked.
             However, non-dimensionalizing with respect to wind speed is not very useful if
             wind speed is changing dynamically and it is common to work directly in terms of
             induced velocity rather than flow factors.
               Equation (3.208) really applies to the whole rotor and the only spatial variation of
             the induced velocity and acceleration that is permitted is as defined in Equations
             (3.182) and (3.202). However, a relaxation of the strict approach has been adopted
             by several workers (see, for example, Schepers and Snel, 1995) where the induced
             velocities are determined for separate annular rings, as described in Section 3.10.8.
             The added mass term for an annular ring can be taken as a proportion of the whole
             added mass according to the appropriate acceleration distribution, Equations
             (3.198), (3.204) and (3.206).
               Figure 3.76 shows measured and calculated flap-wise (out of the rotor plane)
             blade root bending moments for the Tjæreborg turbine caused by a pitch change
             from 0:0708 to 3:7168 with the reversed change 30 seconds later. The turbine was not
             in yaw and the wind speed was 8.7 m=s. The calculated results were made
             according to the equilibrium wake method and with a differential equation method
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