ringing and impulsive excitation from steep and breaking ... · the wave loads project forskel. dtu...
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Ringing and impulsive excitation
from steep and breaking waves
Results from the Wave Loads project
Henrik Bremose
DTU Wind Energy
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The Wave Loads projectForskEL. DTU Wind Energy, DTU Mech. Engng., DHI. 2010-2013.
Henrik Bredmose
Signe Schløer
Robert Mikkelsen
Stig Øye
Torben Juul Larsen
Taeseong Kim
Anders Melchior Hansen
Jesper Mariegaard
Flemming Schlütter
Jacob Tornfeldt Sørensen
Ole Svendstrup Petersen
Hans Fabricius Hansen
Anders Wedel Nielsen
Bjarne Jensen
Iris Pernille Lohman
Xerxes Mandviwalla
Bo Terp Paulsen
Harry Bingham
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Hydrodynamic loads
Simplest: Linear wave kinematics and Morison equation
Better: Fully nonlinear wave kinematics and
Morison-type force model
Advanced: CFD and coupled CFD
Zang and Taylor (2010)
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The Wave Loads projectForskEL. DTU Wind Energy, DTU Mech. Engng., DHI. 2010-2013.
Task B:
CFD methods for steep and breaking wave impacts
DTU, (DHI)
Task A:
Boundary conditions for phase resolving wave models
DHI
Task D:
Physical model tests
DHI
Task C:
Aero-elastic response to fully nonlinear wave forcing
DTU
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What is ringing?
f
F^
fw 2fw3fw
fNatural
Excitation of natural frequency byhigher-harmonic forcing fromnonlinear waves
Third-order inertia load theories:
FNV (1995): regular waves deep water
Krokstad et al (1998): irregular waves
Malenica & Molin (1995): finite depth
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What is impulsive excitation?
f
F^
fw 2fw3fw
fNatural
Sudden excitation of natural
frequency by large and rapid
force. Steep and breaking
waves.
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Study of nonlinear wave load effectsResponse calculations with Flex5 aero-elastic model, NREL 5MW turbine
Signe Schløer (2013)
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Kinematics from a fully nonlinear potential flow solver
‘OceanWave3D’, Engsig-Karup et al (2009)
Allan Engsig-Karup, Harry Bingham and Ole Lindberg
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From kinematics to distributed force
Force model (Rainey 1989, 1995)
Suited for fully nonlinear kinematics
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Response in bottom of towerFully nonlinear waves versus linear waves
Schløer et al (OMAE 2012)
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Static load analysis, h=30m
crest elevations
force peaks
depth integrated
force
nonlinear
linear
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Results of aero-elastic computations
Tower response – largest sea state
Linear waves can also excite the tower
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Results of aero-elastic computations
Monopile response – largest sea state
Vibrations less visible – occur on top of the wave loads
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Quantify fatigue effect
Equivalent load Accumulated equivalent load
Tower effect occur at 25m – wave nonlinearity is stronger for smaller depth
Monopile effect is largest at 40m, where it gives 4% larger equivalent loads.
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Quantify fatigue effect
Equivalent load Accumulated equivalent load
Tower effect occur at 25m – wave nonlinearity is stronger for smaller depth
Monopile effect is largest at 40m, where it gives 4% larger equivalent loads.
Conclusion of present study:
Wave nonlinearity not critical for equivalent fatigue loads.
But 4% in equivalent load corresponds to 18% in fatigue damage
More investigations with more sea states included needed
Inclusion of diffraction needed
Nonlinearity seems more important for ULS than for FLS
Hence ULS study is needed
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The Wave Loads projectForskEL. DTU Wind Energy, DTU Mech. Engng., DHI. 2010-2013.
Task B:
CFD methods for steep and breaking wave impacts
DTU, (DHI)
Task A:
Boundary conditions for phase resolving wave models
DHI
Task D:
Physical model tests
DHI
Task C:
Aero-elastic response to fully nonlinear wave forcing
DTU
![Page 17: Ringing and impulsive excitation from steep and breaking ... · The Wave Loads project ForskEL. DTU Wind Energy, DTU Mech. Engng., DHI. 2010-2013. Task B: CFD methods for steep and](https://reader036.vdocuments.us/reader036/viewer/2022081621/612d09b51ecc51586941f0b6/html5/thumbnails/17.jpg)
The OpenFOAM® CFD solver
Open source CFD toolbox
Vast attention during last 3 years
This study: interFoam solver
3D incompressible Navier-Stokes
two phases (water and air)
VOF treatment of free surface
Waves2foam wave generation toolbox has been developed and validated
(Niels Gjøl Jacobsen
PhD thesis 2011; Paper in Int. J. Num. Meth. Fluids)
OMAE2010
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t=59.0s
Platform height of 8.96m
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t=59.1s
Platform height of 8.96m
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t=59.2s
Platform height of 8.96m
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Development of a coupled solver
Compute outer flow field with potential flow wave model: OceanWave3D (Engsig-Karup et al 2009)
Compute inner field with wave-structure interaction with CFD-VOF model
Coupling zone
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Slender body enables one-way coupling (transfer)
Incident waves enforced in relaxation zone
Diffracted waves damped in relaxation zone
D: cylinder diameter
l: distance to relaxation zone
kA=0.2; kR=0.1; kh=1 Distance can be as small as L/6
Bo Terp Paulsen
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Validation for irregular wave forcing on a slope
Experiment in the Wave Loads project. Hs=8.3m (full scale). Scale 1:36
Bo Terp Paulsen
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Validation for irregular wave forcing on a slope
Experiment in the Wave Loads project. Hs=8.3m (full scale). Scale 1:36
Reconstruct incident wave field by linear analysis of wave gaugemeasurements. Total computed time series is 100s long.
Bo Terp Paulsen
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Bo Terp Paulsen
Validation for irregular wave forcing on a slope
Experiment in the Wave Loads project. Hs=8.3m (full scale). Scale 1:36
Free surface elevation 0.25 cm in front of cylinder
Inline force history
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Bo Terp Paulsen
Validation for irregular wave forcing on a slope
Experiment in the Wave Loads project. Hs=8.3m (full scale). Scale 1:36
Free surface elevation 0.25 cm in front of cylinder
Inline force history
Largest force is due to a breaking waveMay not break to same extent in experiment. Likely caused by limitation of linear construction technique. Better: flux boundary condition based on wave maker signal
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Computation of multi-directional waves
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Computation of multi-directional waves
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Detailed study on uni- and bi-directional wave group impacts
Bo Terp Paulsen
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Detailed study of regular wave forcing and higher-harmonic components
Third-harmonic force compared to FNV theory
Paulsen et al IWWWFB 2012
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The Wave Loads projectForskEL. DTU Wind Energy, DTU Mech. Engng., DHI. 2010-2013.
Task B:
CFD methods for steep and breaking wave impacts
DTU, (DHI)
Task A:
Boundary conditions for phase resolving wave models
DHI
Task D:
Physical model tests
DHI
Task C:
Aero-elastic response to fully nonlinear wave forcing
DTU
![Page 32: Ringing and impulsive excitation from steep and breaking ... · The Wave Loads project ForskEL. DTU Wind Energy, DTU Mech. Engng., DHI. 2010-2013. Task B: CFD methods for steep and](https://reader036.vdocuments.us/reader036/viewer/2022081621/612d09b51ecc51586941f0b6/html5/thumbnails/32.jpg)
Physical model test with a flexible cylinder at DHIBredmose et al OMAE 2013
Inspiration from de Ridder et al OMAE 2011 Target values
from NREL 5MW
reference WTPipe properties
tuning to get
1st and 2nd scaled
nat frequencies
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tuning to get
1st and 2nd scaled
nat frequencies
Instrumentation
accelerometers
displacement
transducer
Wave gauges!
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Example of measurementh=40.8m; Hs=8.3m; Tp=12.6s
impulsive excitationcontinuous forcing:
springing/ringing
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Which waves give the largest accelerations?
Fx
acceleration
in top
accelerometer
[m/s2]
Goda (2010) breaking criterion
See also Hansen et al (OMAE 2012)
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Which waves give the largest accelerations?
Deeper water: larger bulk accelerations. DEPTH AND ARM
Shallow water: larger extreme accelerations. NONLINEARITY AND BREAKING
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FEM model
Force model (Rainey 1989, 1995)
Linear wave detection
Nonlinear wave transformation
OceanWave3D (Engsig-Karup et al 2009)
Numerical reproduction of experiments
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Response, h=40.8 m
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Response, h=20.8 m
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The Wave Loads projectForskEL. DTU Wind Energy, DTU Mech. Engng., DHI. 2010-2013.
Task B:
CFD methods for steep and breaking wave impacts
DTU, (DHI)
Task A:
Boundary conditions for phase resolving wave models
DHI
Task D:
Physical model tests
DHI
Task C:
Aero-elastic response to fully nonlinear wave forcing
DTU