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    6 DEWI MAGAZIN NO. 39, AUGUST 2011

    EXTERNAL ARTICLE

    A. Heege

    ENGLISH

    A. Heege, P. Bonnet, L. Bastard, S. G. Horcas,J.L. Sanchez, P. Cucchini, A. Gaull;

    SAMTECH Iberica

    Numerical Simulation of

    Offshore Wind Turbines by a

    Coupled Aerodynamic,

    Hydrodynamic and Structural

    Dynamic Approach

    Abstract

    The central point of the present publicaon is an implicitly

    coupled aerodynamic, hydrodynamic and structural dynam-

    ic approach dedicated to oshore wind turbine simulaon.

    The mathemacal approach relies on an implicit non-linear

    dynamic Finite Element Method extended by Mul-Body-

    System funconalies, aerodynamics based on the Blade

    Element Momentum theory, controller funconalies and

    hydrodynamic loads.

    Oshore loads are formulated in terms of hydrostac buoy-

    ancy and hydrodynamic wave loads which are approximat-

    ed through Morisons equaon. Special aenon is focused

    on the implementaon of Morisons equaon in order to

    capture hydrodynamic coupling eects which are induced

    by the dynamic response of the oshore wind turbine.

    Two disnct applicaons of oshore wind turbines are ana-

    lyzed. First, a jacket-based oshore wind turbine is loaded

    hydro-dynamically through a wave eld described by Airys

    linear wave theory. As a second example, the aerodynamic

    and hydrodynamic coupling eects are put in evidence by a

    transient dynamic analysis of a oang oshore wind tur-bine anchored to the seabed by structural cables.

    Introducon

    The operaonal deecon modes and associated dynamic

    loads of oshore wind turbines originate, on one hand,

    from the aerodynamic and hydrodynamic loading, and, on

    the other hand, from the proper dynamic response of the

    enre oshore wind turbine system, including all control

    mechanisms.

    A decoupling of the dynamic oshore wind turbine system

    into sub-systems bears the risk of missing dynamic coupling

    eects which might prevail in many operaonal modes. In

    parcular in the case of oang oshore wind turbines,

    a decoupled aero-elasc and hydrodynamic formulaon

    does not permit to reproduce properly the global dynamic

    response of the wind turbine. This is because the speed

    variaons which are induced in the rotor plane by dynamic

    deecons of the oshore wind turbine aect directly the

    rotor aerodynamics and associated controller acons on

    the blade pitch posion and on the generator torque. As a

    consequence, an accurate tuning of controller parameters

    is dicult with simplied, decoupled oshore wind turbine

    models. In order to remedy these deciencies, the pro-posed mathemacal approach is specically formulated in

    order to capture dynamic coupling eects which might be

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    DEWI MAGAZIN NO. 39, AUGUST 2011 7

    induced simultaneously by aero-elasc and hydrodynamic

    loading of oshore structures. Accordingly, the relave

    velocity and acceleraon elds induced by a oang and/

    or vibrang oshore wind turbine are accounted for in the

    proposed coupled aerodynamic and hydrodynamic formu-

    laon.

    The implementaon of aerodynamic loads is based on the

    Blade Element Momentum theory where wind turbine spe-

    cic correcons for p and hub losses, wake eects and theimpact of the tower shadow are accounted. Hydrodynamic

    loads are composed of drag loads and of ineral loads and

    account for the relave velocity and acceleraon elds in

    between the uid and the moving and/or vibrang oshore

    structure.

    Two dierent applicaons of dynamic analysis of oshore

    wind turbines are presented. The wind turbine models are

    discrezed by more than 3,000 Degrees of Freedom (DOF)

    and account for all the abovemenoned coupling eects.

    Coupled Aero-elasc, Hydro-dynamic, Structural FEM &

    MBS Analysis

    The applied mathemacal approach is based on a non-lin-

    ear Finite Element formalism, which accounts simultane-

    ously for exible Mul-Body-System funconalies [1][2]

    [3][4], control devices, aerodynamics in terms of the Blade

    Element Momentum theory [1][2][4][5][6][7], hydrostac

    buoyancy loads and nally hydrodynamic loads in terms of

    the Morison equaon [2][5][10][11][12][13][14].

    Mathemacal background

    In the context of an Augmented Lagrangian Approach and

    the one-step me integraon method of Newmark [1][3],

    the incremental form of the equaons of moon in the pres-ence of constraints is given in equaon (1). According to the

    denion of the residual vector ofequaon (1), the vectorg

    assembles the sum of elasto-visco-plasc internal forcesInt.

    g , complementary ineral forces where centrifugal and

    gyroscopic eects are included, external forces Ext.g , the

    aero-dynamic forces AeroF

    and nally the hydro-dynamic

    and hydrostac loads HydroF

    . The vector introduces ad-

    dional equaons of the generalized soluon

    ,q , whichare used to include general Mul-Body-System/MBS func-

    onalies for the modelling of the power train, pitch and

    yaw drives and nally further DOF which are related to con-

    troller state variables for blade pitch, yaw orientaon and

    generator modelling.

    The non-linear set ofequaons (1) is solved iteravely and

    further details on the me integraon procedure, error es-

    mators and soluon strategies can be found in the SAM-

    CEF-Mecano user manual [1].

    Aero-dynamic and structural coupling

    Blades are modeled in the S4WT soware [1][2] through a

    non-linear FEM formalism adapted to large transformaons

    and large rotaons. For computaonal eciency, the struc-

    tural blade model is presented either in terms of Super Ele-

    ments [1][3], or in terms of non-linear beam elements. The

    elemental aerodynamic forces are computed according tothe Blade Element Momentum/BEM theory including spe-

    cic correcons and addional models for the p and hub

    losses, turbulent wake state, tower shadow eect, dynamic

    inow and dynamic stall [1][2][5][6][7][8][9].

    The structural/aerodynamic coupling is performed implic-

    itly at the blade secon nodes of the structural blade model

    through the connecon of Aerodynamic Blade Secon Ele-

    ments which contribute in terms of elemental aerodynam-

    ic forces to the global equilibrium equaon (1). The discre-

    saon of the aerodynamic loads corresponds to the FEM

    discresaon of the structural blade model and the nodesfor the aero-elasc coupling are generally located at the

    chord length posions of typically about 15 to 20 blade sec-

    ons distributed along the blade span. Taking into account

    that the aerodynamic loadsI

    Pitch

    I

    Drag

    I

    Lift M,F,F presentedin equaon (2) are included in the residual vector ofequa-

    on (1), once the iterave soluon ofequaon (1) to (8) is

    found, the induced velocies, angles of aack, Prandtl loss

    coecients, hydrodynamic forces and the global structural

    dynamic response are consistent.

    It is emphasized that this methodology features a strong

    coupling, i.e. all equaons associated either with aerody-

    namics, hydrodynamics, structures, mechanisms, or control

    loops are solved simultaneously. A major advantage of astrong coupling is that blade vibraons induced by aero-

    dynamic forces and/or hydrodynamic loads, implicitly aect

    the structural response of the global dynamic wind turbine

    model. Accordingly, the relave speeds relV

    that enter in

    the aerodynamic load computaon, account implicitly for

    the aerodynamically induced speeds indV

    and the result-

    ing speeds BV of the structural Blade Secon nodes.

    where a and a are respecvely the axial and tangenal in-

    ducon factors. Details on the procedure applied in order

    to compute the induced speed vector indV in terms of the

    aerodynamic inducons are given in references [1][2][5].

    Hydrostac buoyancy & hydrodynamic wave loads

    In the present work, oshore loads are presented by hydro-

    stac buoyancy loads and by hydrodynamic forces which

    approximate wave loads. The hydrostac buoyancy loads

    are composed of a buoyancy force vector ,t)q(Buoy

    F and

    of a buoyancy restoring moment ,t)q(Buoy

    M . The hydro-

    dynamic wave loads ,t)q,q,q(orison

    F

    are approximated

    through Morisons equaon in terms of a drag and an iner-

    a term [10][11][12].

    Analogously to the aero-elasc coupling through the connec-

    on of Aerodynamic Blade Secon Elements to the FEM

    model of the rotor blades, the coupling of hydrodynamic

    loads to the oshore structure is realized through Hydro-

    dynamic Load Elements/HLE. In the context of a non-linear

    FEM formalism, the Hydrodynamic Load Elements are

    to be considered as 1-noded elements connected to the

    nodes of the FEM mesh of the oshore structure. Accord-

    ingly, each node of the FEM model of the oshore struc-

    ture is loaded by a six-dimensional vector ,t)q,q,q(Hydro

    F

    according to equaon (3).

    Large transformaons & uid kinemacs

    In parcular in the case of oang oshore wind turbines,

    the enre wind turbine, or sub-components like for exam-

    ple the mooring lines, might by subjected to large oscilla-ons which produce eventually large rotaons. In order to

    account properly for large displacements, large rotaons

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    length[m]wave:waveL[s],periodwave:waveT,[rad/m]numberwaveangular:wave2pi/Lk

    Level/SWLWaterStilltodistance:zfrequency,wave:,waterdepth:dheight,wave:Hwith

    (11)t)sin(kxsinh(kd)

    z))cosh(k(d2

    2

    H

    fluidu

    (10)1,2,3kj,i,with)ia

    jq(

    ka)

    ka

    jq(ia

    kq

    jaia

    aCsubV

    add

    ijM

    tv

    tv

    a:spanthetolarperpendicuvectorunitonaccelerati

    qSpan_plane

    Projt

    v:planespantheonprojectedvectoronaccelerati

    (9)q

    )t

    v(

    a

    CsubVMorisonF

    q

    addM

    tcoefficienMorison1,tcoefficienmassadded,tcoefficiendrag

    volumesubmerged,diameter:Dspan,submerged

    spanelementtonormalcomponentvelocitystructural&particlefluid&

    (8)

    (7)2

    (6)

    pointatsurfaceto)(nbody,submergedofsurfaceenvelope:)S(

    levermomentrestoring:lFWL,w.r.t.depth:E,densityfluid:vectorgravity

    (5),

    (4),

    (3),

    'a,),BSVinfowV(findVandindVBSVinfowVrel

    Vwith

    (2)it)A,q,q(2relVt),q,q(iC*2

    1PitchM,DragF,LiftF

    ForcesExternal,ForcesInternalwith

    )(:vectorResidual

    factorPenalty:pmatrix,JacobianConstraint:vectorConstraint:

    matrixInertia&Mass:M:,matrixDamping:C,matrixStiffness:K

    sMultiplierLagrangeofVector:,vectorvectorPosition

    (1)2

    0000

    0

    00

    0

    :aC

    mC:

    aC:

    dragC

    ,t):q(effV,t):q(

    effL

    :vu

    )t

    v

    t

    u(a

    ,t)Cq(eff

    Vt

    u,t)q(

    eff V,t)q,q,q(

    InertiaF

    )vu|(vu|drag,t)Cq(effL

    D,t)q,q(

    DragF

    ,t)q,q(InertiaF,t)q,q(

    DragF,t)q,q,q(

    MorisonF

    qnormal:,tq,tq

    , :g

    ,t)qS(

    dsg,t) q,t) E(q(n,t)q(l

    ,t)qS(

    dsg,t) q,t) E(q(n,t)q(HstatF

    ,t)q(Buoy

    M,t)q(BuoyF,t)q(

    HstatF

    ,t)q(Buoy

    M,t)q,q,q(MorisonF,t)q(

    BuoyF,t)q,q,q(

    HydroF

    a

    ,t)q,q(AeroF

    ,t)q,q,q(Ext.g,t)q,q,q(

    Int.g

    p]T[Bq[M]Ext.gHydroFAeroFInt.g,t)q,q,q(R

    q/,[B]

    onAccelerati:q,:q

    )(,t)q(

    ,t)q,q(R

    q

    ][[B]

    ]T

    [B[K]

    q

    ][][

    ][[C]

    q

    ][][

    ][[M]

    8 DEWI MAGAZIN NO. 39, AUGUST 2011

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    DEWI MAGAZIN NO. 39, AUGUST 2011 9

    and/or deformaons of the oshore wind turbine, the

    kinemacal variables which are involved in the hydrostac

    & hydrodynamic formulaon of equaons (3) to (8) are

    formulated implicitly as a funcon of the soluon of the

    respecve me integraon step of the global equilibrium

    equaon (1). According to Fig. 1 and Fig.2, the eecvely

    submerged depth ),q(eff

    E t is measured w.r.t. to a me

    variable Free Water Level/FWL dened by the wave height

    t),q(W

    . It is noted that a span length vector t),q(Span

    L

    and the associated envelope surface ),tqS( are aachedto each node of the FEM mesh of the oshore. The surface

    normal vector ,t)q(n

    ofequaon (5) is to be interpreted as

    the outward normal for any point of the integral of the en-

    velope surface ),tqS( . Since the span vector t),q(SpanL and

    the envelope surface ),tqS( are moving and rotang with

    the associated structural node of the FEM mesh, the uid

    depth ),q(eff

    E t depends implicitly on the soluon vector

    (t)q

    of the respecve me integraon step. As a conse-

    quence, the buoyancy, drag and ineral loads ofequaons

    (5) to (8) account implicitly for the soluon-dependent ef-

    fecvely submerged span length ),q( teff

    L and for the ef-

    fecvely submerged volume ),q( teffV .

    Hydrostac buoyancy force and restoring moment

    Hydrodynamic loads are introduced through 1-noded Hy-

    drodynamic Load Elements/HLE aached to each node

    of the FEM mesh of the oshore component. According

    to equaon (5), the buoyancy force ,t)q(Buoy

    F and the

    restoring moment ,t)q(Buoy

    M are obtained from the in-

    tegraon of the pressure distribuon that acts on the en-

    velope surface of the submerged oshore components. In

    case of cylindrical geometries, the integrals ofequaon (5)

    are obtained analycally. According to the rst integral

    term ofequaon (5), the direcon of the buoyancy force,t)q(

    BuoyF

    is opposed to the gravity vector and funcon

    of the integral of the pressure acng on the submerged

    envelope surface. The restoring moment ,t)q(Buoy

    M is

    determined by the second integral term of equaon (5)

    where the lever vector ,t)q(l points from the origin of the

    local coordinate system of the Hydrodynamic Load Ele-

    ment to the respecve integraon point of the envelope

    surface ),tqS( with the normal vector ,t)q(n .The orienta-

    on of the local axis of the restoring moment ,t)q(Buoy

    M

    results from the integral soluon of the second term of

    equaon (5) which is funcon of the inclinaon of the o-

    shore component w.r.t. to the gravity vector.

    Hydrodynamic wave loads according to Morisons equa-

    on

    Morisons formula was originally applied to the computa-

    on of uncoupled hydrodynamic forces on vercal, xed

    piles with shallow water wave loading. It has since been

    extended to a three-dimensional formulaon for arbitrar-

    ily oriented moving structures, with both wave and cur-

    rent loadings [10][11][12]. As stated in equaons (6) to

    (8), the coupled Morison equaon presents an empirical

    formulaon that describes the hydro-dynamic loads as a

    superposion of a uid drag DragF

    and an ineral term

    InertiaF

    that accounts for the added uid mass acceler-ated due to the uid-structure interacon.

    DEWI oers an independent service

    or periodic technical inspections

    on wind turbines and wind arms

    during the project lie cycle. The

    services provided by DEWI allowproject developers, wind arm owners

    or investors to combine technical

    saety with a reliable and proftable

    management within the long-term

    operation o the wind arm.

    As one o the leading international

    consultants in the feld o wind energy,

    DEWI oers all kinds o wind energy related

    measurement services, energy analyses and

    studies, urther education, technological,economical and political consultancy or

    industry, wind arm developers, banks,

    governments and public administrations.

    DEWI is accredited to EN ISO/IEC 17025 and

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    recognised as an independent institution in

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    www.dewi.de

    Wind Turbine inspecTion

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    10 DEWI MAGAZIN NO. 39, AUGUST 2011

    The uid drag vector formulated in equaon (7) and the u-

    id ineral load vector formulated in equaon (8) are both

    contained in the plane perpendicular to the span direcon,

    but show generally dierent direcons, i.e. the angle of

    aack of the drag forces and the angle of aack of the

    inera forces do not generally coincide.

    A coupled formulaon of Morisons approach is exposed

    in references [11][12] in a form analogous to equaon (8)

    where the direcon of the Morison inera load vector is

    determined by 2 disnct contribuons with a-priori 2 dif-

    ferent vector orientaons. The rst term of the Morison

    equaon (8),

    t

    u

    t),q(eff

    V ,

    contributes to the Morison inera forces, if the unperturbed

    uid ow is accelerated. The direcon of that vector compo-

    nent corresponds to the direcon of the unperturbed uid

    direcon, but projected into the plane which is perpendicu-

    lar to the span direcon of the oshore component. The

    second term of the Morison equaon (8) contributes to theinera forces through the relave uid-structure accelera-

    on

    )(t

    v

    t

    u

    which results from the unperturbed uid ow accelera-

    on and from the dynamic response of the oshore struc -

    ture. It should be noted that both vector components

    ofequaon (8) are projected onto the same plane which is

    perpendicular to the span wise direcon, but the respecve

    vector orientaons of these two terms are not necessarily

    aligned if the structure vibrates and/or oats.

    It is conjectured that the inclusion of the uncoupled inera

    term of the Morison equaon (8) might not be straighor-

    ward for a formulaon dedicated to the simulaon of cou-

    pled hydrodynamic and structural dynamic phenomena.

    It is spulated that the basic Morison equaon as stated in

    references [10][11][12] might lead to an overesmaon of

    hydrodynamic drag and/or inera loads, because hydrody-

    namic inducons and/or wave dispersion are not accounted

    for in that formulaon.

    Added Mass & Eigen-ModesThe inera term InertiaF

    of the Morison equaon (8) mod-

    ies the total mass associated to the submerged oshore

    Fig. 1: S4WT wind turbine model supported by

    OC4 jacket oshore structure

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    DEWI MAGAZIN NO. 39, AUGUST 2011 11

    Fig. 2: Submerged span for node above Free Water Level/FWL and below FWL

    structure and as a consequence the Eigen-Modes of the o-

    shore wind turbine are aected.

    As outlined, the implemented algorithm for the hydrody-

    namic loads accounts implicitly for the kinemacs induced

    by a heavily moving oshore wind turbine and transient

    wave height. The total mass taken into account in the Ei-

    gen-mode computaon of the oshore structure is comple-

    mented through the derivave of the inera term of the

    Morison equaon (8) with respect to the relave accelera-

    ons in between the uid and the vibrang and/or oang

    oshore structure. Equaons (9, 10) dene the added mass

    term in terms of the derivave of the Morison inera force

    with respect to the structural acceleraons of the respec-

    ve node of the FEM model. As stated in equaon (10) in

    tensorial form using the Einstein summaon convenon,

    the added uid mass is obtained through the derivave of

    the Morison inera term and can be presented in terms of

    two contribuons. The rst contribuon is determined by

    the added massa

    Csub

    V mulplied by the dyadic productof the acceleraon unit vector aa

    . It is emphasized that

    the unit vector a is contained in the plane perpendicular tothe span wise direcon of the respecve component and

    might be interpreted as the vector dening the direcon of

    the inera loads. The second term ofequaon (10) depends

    not only on the vector a

    , but as well on the structural ac-

    celeraon of the respecve FEM node q and on the deriva-

    ve of the acceleraon unit vector a

    . As a consequence

    the addional uid mass included in the global mass and

    inera matrix of equaon (1) becomes me dependent

    and also dependent on the instantaneous spaal direcon

    of the relave acceleraon which occurs in between the

    uid and the submerged oshore structure. Therefore, not

    only do the Eigen-Frequencies of the oshore wind turbine

    become me dependent, but also the Eigen-Shapes are af-

    fected by the added uid mass, because the added mass is

    direconal.

    Airys linear wave theory

    In the present studies, the unperturbed uid velocity/accel-

    eraon eld is modelled according to equaon (11) through

    Airys wave theory [13][14] that approximates the transient

    uid dynamics of waves as a funcon of parameters like wa-

    ter depth, wave height and period.

    The following application examples are based on fluid/

    water speed distributions according to equation (11) andare generated by the independent program Waveloads of

    the University of Hannover [13].

    Fig. 3: Zoom on wave speed & wave height at node #40 located at limit

    to free uid surface of jacket

    Fig. 4: hydrodynamic drag force, Morison inera force & and buoyancy

    force at node#40

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    12 DEWI MAGAZIN NO. 39, AUGUST 2011

    Applicaon Examples

    Two disnct simulaons of oshore wind turbines are

    presented. Even though the implemented methodologysupports the implementaon of very complex oshore

    structures in terms of general FEM models, in the present

    examples the oshore structures are modelled by non-line-

    ar beam elements of circular geometry.

    The rst applicaon corresponds to an oshore wind tur-

    bine supported by a jacket structure that corresponds to

    the OC4 reference base line model [15]. The second exam-

    ple presents a oang oshore wind turbine whose oater

    and mooring lines correspond to the OC3 reference model

    [16].

    Oshore wind turbine supported by Jacket structure

    Fig. 1 presents the S4WT wind turbine model supported by a

    jacket structure according to the OC4 reference model [15].

    The applied wind turbine model comprises in total 3732

    DOFs and includes a detailed gearbox model, pitch and yaw

    drives and further exible structural components like the

    bedplate and nacelle structure in terms of Super Elements.

    The jacket structure is modelled by non-linear beam ele-

    ments and loaded by buoyancy and hydrodynamic loads.

    The following simulaon results correspond to a load case

    with wind eld of a mean speed of 10 [m/s] and a wave

    denion according to Airys linear wave model with the

    following characteriscs:

    Wave Height: 6m, Wave Period: 10s, Water Depth: 50m

    Angle in between wave & wind direction: 0 [deg.]

    Note that the spaal uid speed distribuon is obtained

    from the external soware Waveloads [13]. The corre-

    sponding acceleraon eld of the external wave and the

    relave structural-uid acceleraons of equaons (8) are

    computed in the hydrodynamic element of the solver SAM-CEF-Mecano.

    Fig. 3 presents the hydrodynamic boundary condions for

    the jacket node #40 located closely to the Sll Water Level/

    SWL. The applied wave velocies in longitudinal XGL and

    vercal ZGL direcons refer to the le ordinate ofFig. 3 and

    the wave height refers to the right ordinate of Fig. 3. The

    locaon of the jacket node #40 considered here is depicted

    in Fig. 1. Fig. 4 presents for node #40 the resulng buoyancy

    force, the uid drag and nally the Morison inera force.

    Floang oshore wind turbine

    Fig. 5 presents the S4WT model of a floating offshore wind

    turbine supported by a floating structure according to ref-

    erence [16]. The wind turbine model comprises in total

    3402 DOFs and includes a detailed power train model, pitch

    and yaw drives and further flexible structural components

    like the mooring lines.

    The simulated load case corresponds to a constant wind

    eld of a mean speed of 16 [m/s] and a wave denion ac-

    cording to equaon (11) with the following characteriscs:

    Wave Height: 6m, Wave Period: 10s, Water Depth:

    320m

    Angle in between wave & wind direction: 45 [deg.]

    As depicted in Fig. 5, the floating offshore wind turbine is

    attached by 3 cables which are separated each by a rotationof 120 [degrees] w.r.t. to the vertical reference axis. The

    length of each cable is about 700 [m]. In S4WTs floating

    Fig. 5: S4WT model of OC3 oshore 5-MW baseline wind turbine

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    Werbung

    Samtech

    1/1

    4c

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    14 DEWI MAGAZIN NO. 39, AUGUST 2011

    Fig. 6: Generator speed, blade pitch & power transients induced by the oang wind turbine oscillaons

    wind turbine model, the cables are presented either by

    non-linear cable elements (neither compression, nor bend-

    ing stiffness), or respectively by non-linear Beam Ele-

    ments.

    The large oscillations of the floating wind turbine induce

    large low frequency speed variations in the rotor plane.

    Fig. 6 clearly shows the low frequency speed and rotor

    torque variations induced by the global tilt oscillations of

    the floating turbine. It can be noted that further controller

    tuning would be required in order to reduce these oscilla-

    tions induced by the floating wind turbine concept.Fig. 6 presents the blade pitch, speed and power transients

    of the presented oang oshore wind turbine. The pre-

    sented transients of blade pitch angle and the produced

    power show low frequency oscillaons induced by the ro-

    tor plane speed variaons due to the lt oscillaons of the

    enre oang wind turbine.

    The tower-top trajectory in longitudinal XGL direcon (direc-

    on of incoming wind) and in the horizontal YGL, is shown

    on the top-right corner ofFig. 5. The maximum oscillaon

    of the tower-top of the oang wind turbine in the longi-

    tudinal direcon is evaluated from -1.5 [m] to 9 [m], i.e. a

    total displacement range of the tower-top of nearly 14[m]

    in the longitudinal direcon. In the case of the simulated

    wave height of 6 [m], due to the induced buoyancy loads,

    the wind turbine top oscillates approximately 2[m] in the

    vercal direcon.

    On the lower right poron ofFig. 5, the external hydrody-

    namic uid loads applied on a specic node of the mooring

    line FEM model are presented. The locaon of mooring line

    node #49 is presented in Fig. 5. It is noted that the Morison

    inera force module presents a phase oset with respect

    to the drag force. The drag and ineral forces are both con-

    tained in the same plane perpendicular to the span direc-

    on, but the orientaon of both force components do not

    generally coincide.

    Conclusions

    Morisons equaon was implemented in the solver SAM-

    CEF-Mecano in an extended form proposed in several refer-

    ences such as [11] and [12] in order to account for struc-

    tural dynamics and hydrodynamics coupling eects. The

    coupled form of the Morison equaon is interpreted as an

    empirical approximaon for the modelling of hydrodynamic

    currents and/or waves and can be decomposed into two

    principal contribuons. On the one hand, an uncoupled in-

    era term which is only funcon of the acceleraon of theuid ow, and, on the other hand, a coupled inera term

    which is funcon of the relave acceleraon in between

    the oshore structure and the unperturbed uid ow. It

    is conjectured that the precision and applicaon range of

    the coupled form of Morisons equaon might be improved

    with some further modicaons. First, it might be conven-

    ient to formulate not only the second term, but as well the

    rst term of the Morison equaon (8) implicitly as a func-

    on of the dynamic response of the oshore structure. Sec-

    ond, Morisons model does not account for hydrodynamic

    inducons on the unperturbed uid speeds and/or accel-

    eraons which would result from the uid-structure inter-

    acon. Analogously, the dispersion of an impacng wave

    on the oshore structure is not accounted for in Morisons

    empirical model. As a consequence, it is spulated that the

    applicaon of the Morison equaon might tend to an over-

    esmaon of hydrodynamic drag and/or uid inera loads.

    It is conjectured that the empirical formulaon of Morison

    might be improved if the added mass coecient, or respec-

    vely the Morison coecient, is formulated as an empirical

    decay funcon of the rao between the hydraulic diameter

    and the wavelength, as stated by MacCamy and Fuchs [17].

    These empirical decay funcons might approximate roughly

    the eect of uid-structure inducons and/or wave disper-

    sion, as it has been already reected in some recommendedpracces regarding oshore structures [18]. Future imple-

    mentaons will be devoted to automacally modifying the

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    DEWI MAGAZIN NO. 39, AUGUST 2011 15

    Morison coecient taking into account these experimental

    observaons and the corresponding wave dynamics. The

    fully coupledphilosophy of the current code will be kept

    during this new development, so the eects of the struc-

    ture kinemacs will be considered during hydrodynamic

    load computaon.

    Two disnct oshore wind turbines have been analyzed by

    a fully coupled aerodynamic, hydrodynamic and structural

    dynamic approach. In the rst applicaon example, theOC4 reference oshore wind turbine model was chosen.

    The corresponding aero-elasc S4WT wind turbine model

    is supported by a hydro-dynamically loaded jacket FEM

    model, includes exible MBS models of the major mecha-

    nisms like the power train including the gearbox, the yaw

    and the pitch drives, and comprises in total 3732 Degrees

    of Freedom. The required CPU me for transient analysis

    on a standard Intel Duo Core 3.2GHz computer, was similar

    compared to standard onshore high delity wind turbine

    models with a CPU me factor of about 45 with respect to

    real me. It is menoned that required CPU mes depend

    strongly on the number of Degrees of Freedom and on the

    excited frequency content of the respecve model. In the

    case of simplied wind turbine models that comprise less

    than 1000 DOFs, the required CPU is generally less than a

    factor of 10 with respect to real me.

    In the case of the OC3 oshore reference model, the oat-

    ing wind turbine model is not restrained by xaons as in

    the case of clamped jacket supports. Instead, the oater is

    aached to exible mooring lines aached to the seabed.

    As a consequence, the dynamic equilibrium of the oscillat-

    ing oang wind turbine is strongly inuenced by coupled

    buoyancy, hydrodynamic and aero-elasc loads which all

    strongly mutually interact together with controller acons.

    In parcular the low frequency oscillaons of the oangturbine induce large speed variaons in the rotor plane.

    In order to reduce the observed rotor plane speed varia-

    ons induced by the oscillang oang wind turbine, spe-

    cic controller tuning for blade pitch and generator torque

    would be required. Future research will include specic

    control strategies in order to reduce these oscillaons, for

    instance via the integraon of acve damping techniques.

    References

    [1]. SAMCEF-Mecano User Manual Version 14.1,

    http://www.samtech.com

    [2]. S4WT V3.1, SAMCEF for Wind Turbine User Manual,

    http://www.samtech.com

    [3]. Geradin, M. and Cardona, A., Flexible Multibody Dynamics: A Finite

    Element Approach. John Wiley and Sons Ltd, 2001

    [4]. Heege A., Betran J., Radovcic Y., Fatigue Load Computation of Wind

    Turbine Gearboxes by Coupled Finite Element, Multi-Body-System

    and Aerodynamic Analysis, Wind Energy, vol. 10:395-413, 2007.

    [5]. Heege A., Bonnet P., Bastard L., Horcas S. G., Sanchez J.L., Cucchini P.,

    Gaull A., Numerical simulation of offshore wind turbines by a cou-

    pled aerodynamic, hydrodynamic and structural dynamic approach,

    Proceedings EWEA 2011 conference, 14-17 March 2011, Brussels/

    Belgium.

    [6]. Bossanyi, E. A., GH-Bladed User Manual, Issue 14, Garrad Hassan and

    Partners Limited, Bristol, UK, 2004

    [7]. AeroDyn Theory Manual, December 2005 NREL/EL-500-36881,

    Patrick J. Moriarty, National Renewable Energy Laboratory Golden,

    Colorado A. Craig Hansen Windward Engineering, Salt Lake City,

    Utah

    [8]. Snel H., Schepers J. G., Joint Investigation of Dynamic Inflow Effects

    and Implementation of an Engineering Method, ECN Report ECN-

    C--94-107, 1995.

    [9]. Hansen M. H., Gaunaa M., Madsen H. A., A Beddoes-Leishman type

    dynamic stall model in state-space and indicial formulations, Riso

    Report Riso-R-1354(EN), 2004.

    [10]. Morison, J. R., O Brien, M. P., Johnson, J. W. and Schaaf, S. A., The

    forces exerted by surface waves on piles. Petroleum Transactions.

    189 (TP 2846), p 149, 1950

    [11]. Germanischer Lloyd Wind Energie GmbH, Guideline for the Certifica-

    tion of Offshore Wind Turbines. 1st June 2005

    [12]. American Petroleum Institute. Recommended Practice for FlexiblePipe, API Recommended Practice 17B. Third Edition, March 2002

    [13]. K.Mittendorf,B.Nguyen and M.Blmel. WaveLoads, A computer pro-

    gram to calculate wave loading on vertical and inclined tubes.User

    manual. Gigawind, Universitt Hannover. Version 1.01, August 2005

    [14]. Robert G.Dean, Robert A. Dalrymple. Advanced Series on Ocean En-

    gineering, Volume 2: Water wave mechanics for engineers and scien-

    tists. World Scientific Publishing Co. Singapore, 1991

    [15]. F. Vorpahl, W. Popko, D. Kaufer. Description of a basic model of the

    Upwind reference jacket for code comparison in the OC4 project

    under IEA Wind Annex XXX; Fraunhofer Institute for Wind Energy and

    Energy System Technology (IWES), 4 February 2011

    [16]. J. Jonkman, Definition of the Floating System for Phase IV of

    OC3,Technical Report, NREL/TP-500-47535, National Renewable En-

    ergy Laboratory Golden Colorado/USA, May 2010.

    [17]. MacCamy, R.C., Fuchs, R.A., Wave forces on piles: A diffraction theo-

    ry, U.S. Army Corps of Engineers, Beach Erosion Board, Tech. Memo

    No. 69,1954

    [18]. American Petroleum Institute. Recommended Practice for Planning,

    Designing, and Constructing Tension Leg Platforms, API Recommend-

    ed Practice 2T. Second Edition. August 1997


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