Final report for WP4.3: Enhancement of design methods ... - Upwind
Final report for WP4.3: Enhancement of design methods ... - Upwind
Final report for WP4.3: Enhancement of design methods ... - Upwind
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UPWIND WP4: Offshore Support Structures and Foundations<br />
While no dedicated scientific research on FOWT-specific blade <strong>design</strong> has been published yet, the work package<br />
“Offshore Blades” <strong>of</strong> the European KIC (Knowledge & Innovation Community) InnoEnergy research project<br />
Offwindtech, led by University <strong>of</strong> Stuttgart and started beginning <strong>of</strong> 2011, will address this issue.<br />
8.2 Hydrodynamic theories<br />
In order to take proper account <strong>of</strong> the influence <strong>of</strong> a floating body on the surrounding fluid, potential flow theory<br />
must be used. This is particularly important <strong>for</strong> floating wind turbine support structure <strong>design</strong>s which have large<br />
diameters and experience significant motion. In potential flow theory the fluid is considered to be incompressible,<br />
inviscid and surface tension effects are neglected. The flow is irrotational and so the velocity <strong>of</strong> the fluid<br />
( ) at a certain point in a Cartesian coordinate system fixed in space and instant (t) is given by:<br />
The total velocity potential ( ) satisfies the Laplace equation in all fluid domain:<br />
and also at the boundary conditions at the air and solid interfaces that define the problem. The complete <strong>for</strong>mulation<br />
<strong>of</strong> these boundary conditions is in general difficult to solve, and first or second-order approximations are<br />
typically used to define the respective hydrodynamic <strong>for</strong>mulation. These are also referred to in the literature as<br />
the linear and weakly nonlinear <strong>for</strong>mulations.<br />
Linear potential flow theory is used in many different <strong>of</strong>fshore engineering problems. This theory considers, in<br />
addition to the potential flow assumptions described above, that the amplitudes <strong>of</strong> both the incident waves and<br />
the motions <strong>of</strong> the floating structure are small when compared with the incident wavelength. Second-order,<br />
weakly nonlinear hydrodynamic theory assumes (as in the first-order case), small amplitudes <strong>for</strong> the incident<br />
waves and motions in comparison with the wavelength and characteristic body dimensions. However, this theory<br />
takes into account a more detailed representation <strong>of</strong> the velocity potential ( ) and all derived variables by<br />
considering a second-order approximation through a Taylor expansion series about the mean positions. A full<br />
description <strong>of</strong> the second-order approximation can be found in [111].<br />
The second order approximation more properly accounts <strong>for</strong> hydrodynamic loading on the wetted surface <strong>of</strong> the<br />
body <strong>for</strong> plat<strong>for</strong>ms which are subject to steep-sided or very large waves. Second order hydrodynamic loads are<br />
proportional to the square <strong>of</strong> the wave amplitude, and have frequencies equal to both the sum and the difference<br />
<strong>of</strong> the multiple incident wave frequencies. This means that although the natural frequencies <strong>of</strong> the structure<br />
are <strong>design</strong>ed to be outside the wave energy spectrum, the second order <strong>for</strong>ces will excite these frequencies,<br />
so despite the <strong>for</strong>ces being small in magnitude the resonant effect can be important. Three examples <strong>of</strong><br />
second order hydrodynamic <strong>for</strong>ces are given below.<br />
• Mean drift <strong>for</strong>ces. These <strong>for</strong>ces result in a mean <strong>of</strong>fset <strong>of</strong> the body relative to its undisplaced position,<br />
and are typically an order <strong>of</strong> magnitude lower than first order wave excitation <strong>for</strong>ces. The mean drift<br />
<strong>for</strong>ce is a combination <strong>of</strong> second order hydrodynamic pressure due to first order waves and the interaction<br />
between first order motion and the first order wave field. The viscous drag contribution to this <strong>for</strong>ce<br />
is significantly increased when there is a current present. Since the mooring line tension is <strong>of</strong>ten related<br />
non-linearly to plat<strong>for</strong>m displacement, the mean drift <strong>for</strong>ces can have an important effect.<br />
• Slowly varying drift <strong>for</strong>ces. These <strong>for</strong>ces have much longer periods than the main wave energy spectrum<br />
but are still within the range <strong>of</strong> horizontal plat<strong>for</strong>m motion. They result from non-linear interactions<br />
between multiple waves with different frequencies. Again the <strong>for</strong>ces resulting from slowly varying drift<br />
are generally small compared to <strong>for</strong>ces at the wave frequency, but they can cause large displacements<br />
in moored floating wind turbines which can in turn lead to high loads in the mooring lines. In addition<br />
these <strong>for</strong>ces can excite the large amplitude resonant translational motion <strong>of</strong> the floating plat<strong>for</strong>m.<br />
• High frequency <strong>for</strong>ces. These <strong>for</strong>ces have a frequency which is higher than the wave frequency and are<br />
also generally small in amplitude. They arise from the same source as low frequency drift <strong>for</strong>ces, i.e. interactions<br />
between multiple waves <strong>of</strong> varying frequency. The contribution from these <strong>for</strong>ces can be particularly<br />
important when analysing ‘ringing’ behaviour <strong>for</strong> floating wind turbine configurations such as<br />
93<br />
[8-1]<br />
[8-2]