Page 167 - Wind Energy Handbook
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UNSTEADY FLOW – DYNAMIC INFLOW                                         141

                   400

                            Measurement
                            2D coefficients
                   300      3D coefficients
                  Aerodynamic power (kW)  200








                   100




                     0
                       0                                       10                                       20                                         30
                                              Wind speed (m/s)

             Figure 3.75  A Comparison of Measured and Snel’s Predicted Power Curves for a NOR-
             TANK 300 kW Turbine

               If the linear part of the static, two-dimensional, C l   Æ curve is extended beyond
             the stall then let ˜C l be the difference between the two curves. Then the correction
             to the two-dimensional curve to account for the rotational, three-dimensional,
                          2
             effects is 3(c=r) ˜C l .
                                                        2
                                                      c
                                                  þ 3                            (3:190)
                                        C l 3-D  ¼ C l 2-D  ˜C l
                                                      r
                                                                        ) lift coefficients
             Table 3.2 compares the measured static (C l 2-D  ) and rotating (C l 3-D
             with the calculated values for the rotating values using Snel’s correction of Equation
             (3.190). The correction is quite good and is very simple to apply. An example of the
             correction is given by Snel et al. (1993) and is shown in Figure 3.75.



             3.13    Unsteady flow – Dynamic inflow

             3.13.1  Introduction

             Natural winds are almost never steady in either strength or direction and so it is
             seldom that the conditions for the momentum theory apply. It takes a finite time for
             the wind to travel from far upwind of a rotor to far downwind and in that time
             wind conditions will change so an equilibrium state is never achieved. Even if the
             ‘average’ wind speed changes only slowly small-scale turbulence will cause a
             continuous unsteadiness in the velocities impinging on a rotor blade.
               Several approximate solutions offer themselves for the determination of the
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