Page 272 - Wind Energy Handbook
P. 272

246                        DESIGN LOADS FOR HORIZONTAL-AXIS WIND TURBINES


               1
              0.9    r = 0m
              0.8                                  Integral length scale, L = 73.5 m
              Normalized correlation functions  0.6  r = 10 m  Speed of rotation = 30 r.p.m.
              0.7
                                                     Mean wind speed = 8 m/s
              0.5
              0.4
                     r = 20 m
              0.3
                     Smooth curves are autocorrelation functions
              0.2
                     Bulletted curve is cross correlation function for r 1  = 10 m and r 2  = 20 m
              0.1
               0
                0            1            2            3            4            5
                                          Number of rotor revolutions
          Figure 5.18 Normalized Autocorrelation and Cross Correlation Functions for Along-wind
          Wind Fluctuations for Points on a Rotating Blade at Different Radii



              1.4                                          r = 20 m
             Rotationally sampled power spectral density function, R(r,n)  0.8 1  Integral length scale, L = 73.5 m
              1.2

                            Mean wind speed = 8 m/s
                          Speed of rotation = 30 r.p.m.


              0.6


              0.4
              0.2
                                                   r = 0 m
                                                                             r = 10 m
                                         r = 20 m
               0
               0.001           0.01             0.1              1               10
                                        Frequency, n (Hz, logarithmic scale)
          Figure 5.19 Rotationally Sampled Power Spectra of Longitudinal Wind Speed Fluctuations
          at Different Radii



          which arises from the aliasing effect described above. Figure 5.20 is a repeat of
          Figure 5.19, but with a logarithmic scale used on both axes.
            It is instructive to consider how the various input parameters affect the shift of
                                                        o
                                               o
                                                          s
          energy to the rotational frequency. As k (r, ô) ¼ k (~ s, 0) decreases monotonically
                                               u        u
          with increasing s, Equation (5.36) indicates that the depths of the troughs in this
          function – and hence the transfer of energy to the rotational frequency – increases
   267   268   269   270   271   272   273   274   275   276   277