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Hull/mooring/riser coupled dynamic analysis and sensitivity
study of a tanker-based FPSO
Arcandra Tahara, M.H. Kimb,*
aCSO Aker Engineering Inc., Houston, TX 77079, USAbDepartment of Civil Engineering, Ocean Engineering Program Texas A and M University,
Offshore Technology Research Center College Station, TX 77843, USA
Received 22 August 2002; revised 5 February 2003; accepted 7 February 2003
Available online 17 April 2004
Abstract
A computer program is developed for hull/mooring/riser coupled dynamic analysis of a tanker-based turret-moored FPSO (Floating
Production Storage and Offloading) in waves, winds, and currents. In this computer program, the floating body is modeled as a rigid body
with six degrees of freedom. The first- and second-order wave forces, added mass, and radiation damping at various yaw angles are calculated
from the second-order diffraction/radiation panel program WAMIT. The wind and current forces for various yaw angles of FPSO are
modeled following the empirical method suggested by OCIMF (Oil Company International Marine Forum).
The mooring/riser dynamics are modeled using a rod theory and finite element method (FEM), with the governing equations described in a
generalized coordinate system. The dynamics of hull, mooring lines, and risers are solved simultaneously at each time step in a combined
matrix for the specified connection condition. For illustration, semi-taut chain-steel wire-chain mooring lines and steel catenary risers are
employed and their effects on global FPSO hull motions are investigated. To better understand the physics related to the motion
characteristics of a turret-moored FPSO, the role of various hydrodynamic contributions is analyzed and assessed including the effects of hull
and mooring/riser viscous damping, second-order difference-frequency wave-force quadratic transfer functions, and yaw-angle dependent
wave forces and hydrodynamic coefficients. To see the effects of hull and mooring/riser coupling and mooring/riser damping more clearly,
the case with no drag forces on those slender members is also investigated. The numerical results are compared with MARIN’s wave basin
experiments.
q 2004 Elsevier Ltd. All rights reserved.
Keywords: FPSO; Hull-mooring-riser coupled dynamic analysis; Mooring and riser damping; Large yaw angles; Case studies; Quadratic transfer function;
Motion simulations
1. Introduction
FPSOs have been successfully installed and operated in
many places worldwide for oil and gas production. Besides
environmental risk related to oil spills, FPSOs have a
number of advantages compared to other platforms. The
biggest advantage is huge storage capacity (no pipeline
needed) and ample deck space giving better layout
flexibility. Recently, Minerals Management Service
(MMS) has approved the use of FPSOs with double hull
in the Gulf of Mexico.
Several researchers have done various studies about
the dynamic characteristics of FPSOs in winds, waves,
and currents. Wichers [22], for example, initiated a
comprehensive study for numerical simulations of a turret-
moored FPSO in irregular waves with winds and currents.
He derived the equation of motions of such model in the
time domain using an uncoupled method and solved rigid-
body and mooring-line dynamics separately. On the other
hand, several researchers [20,13] investigated the behavior
and stability of turret-moored FPSOs based on a set of
simplified ship-maneuvering equations.
Spars and TLPs are designed so that their natural
frequencies are away from the dominant wave frequencies
in all six degree-of-freedom modes. On the other hand, the
natural frequencies of FPSOs in heave and pitch are within
typical frequency band of sea energy spectra, and thus heave
and pitch wave-frequency motions tend to be large.
These wave frequency motions in turn can excite riser
0141-1187/$ - see front matter q 2004 Elsevier Ltd. All rights reserved.
doi:10.1016/j.apor.2003.02.001
Applied Ocean Research 25 (2003) 367–382
www.elsevier.com/locate/apor
* Corresponding author. Tel.: þ1-979-847-8710; fax: þ1-979-862-8162.
E-mail address: [email protected] (M.H. Kim).
and mooring-line motions creating significant interaction
effects. Therefore, the hull/mooring/riser coupling effects of
FPSOs are expected to be more important compared with
spars and TLPs. The interactions between hull and slender
members of deepwater platforms are difficult to be
investigated by model testing because of the depth
limitation of wave basins. The mismatch of Reynolds
numbers between the slender members of model and
the prototype is another intrinsic problem in the physical
model testing.
On the other hand, the dynamic interactions between hull
and slender members can be evaluated numerically in
several ways. One simple approach is called uncoupled
analysis, which assumes that mooring lines and risers
respond statically (as a mass-less non-linear spring) to hull
motions [13]. With this assumption, the inertia effects and
hydrodynamic loading on mooring lines and risers are
neglected. After hull motions are calculated, the mooring
and riser dynamics can be evaluated independently by
inputting the fairlead responses. The reliability and
accuracy of this approach is expected to diminish as water
depth increases. Kim et al. and Ma and Lee [8,9,10,14]
showed that such uncoupled analysis of TLPs and spars may
be inaccurate when used in deepwater. Wichers et al. [25]
showed that the uncoupled analysis may give even larger
error in case of FPSO. Wichers et al. [25] concluded that
fully coupled dynamic models are necessary to estimate
realistic design values. Using hull/mooring/riser coupled
dynamic analysis tools [2,10], the effects of risers and
mooring lines on FPSO hull motions and vice versa can be
more accurately predicted, as illustrated in this paper.
Turret-moored FPSOs are free to rotate in the horizontal
plane, and thus may have large yaw motions in non-parallel
wind–wave–current environments or in multidirectional
waves. In such a case, the variation of wave forces and other
hydrodynamic coefficients against various yaw angles need
to be incorporated for more reliable motion analysis. To
include such effects, all the first- and second-order wave
forces and hydrodynamic coefficients have to be pre-
calculated and tabulated for various yaw angles, which
requires substantial computational effort. Instead, one can
use, as an approximation, the single set of hydrodynamic
quantities calculated at the mean yaw angle and use them
throughout entire simulation. So far, no researcher quanti-
tatively showed how important the effects of exact yaw-
angle dependent hydrodynamic forces are.
One of the most difficult factors in the numerical
simulation of a turret-moored FPSO is the reasonable
estimation of hull viscous damping. The low-frequency
viscous reaction forces on FPSOs were measured by
Wichers and Ji [24]. They also examined the coupling
terms due to the combined modes of motions in still water
and in current. A conclusion of this study is that the viscous
part in normal direction contributes significantly to the hull
dynamics, particularly in currents, and thus cannot be
neglected. In the present study, we simulated FPSO motions
with or without considering the empirical viscous forces on
FPSO hull, and quantitatively showed the difference
between them.
When simulating FPSO motions numerically, no
researcher so far used the exact second-order difference-
frequency wave force QTFs [11,7], which is computationally
very intensive. Instead, most researchers used the so-called
Newman’s approximation [15] which assumes that the
difference-frequency force QTFs can be approximated by
the mean-drift forces and moments (diagonal values) when
the system’s natural frequencies are small. In the present
study, both Newman’s approximation and the full-QTF
approach are used to illustrate the reliability of the
approximation method popular in the offshore industry.
Here, the wave force QTFs are calculated from the second-
order diffraction/radiation program WAMIT [12].
Recently, the extreme responses of a turret-moored
FPSO in the Gulf of Mexico were also studied experimen-
tally by Baar et al. [3]. They investigated the responses of a
FPSO in collinear and non-collinear winds, waves, and
currents of 100-year hurricane. A conclusion from their
study is that the responses of their turret-moored FPSO are
more sensitive to non-collinear environmental conditions. A
similar experimental study for a turret-moored FPSO
designed for 6000-ft water depth was also conducted by
Ward et al. [21] in the Offshore Technology Research
Center wave basin. They also showed that the responses of
the FPSO are more severe in non-collinear environmental
conditions. In this regard, a typical non-parallel 100-yr
storm in the Gulf of Mexico is used as an environmental
condition.
2. Description of FPSO, mooring system and Riser
The vessel used in this study is a 1,440,000 bbls storage
tanker and has an LBP of 310 m, a beam of 47.17 m, and a
depth of 28.04 m. At the full-load condition, the vessel has
an average draft of 18.9 m, with displacement of 240,869
MT. The internal turret mooring system is located 63.55 m
aft of the forward perpendicular of the vessel and has
15.85 m of diameter. The main particulars of the vessel are
summarized in Table 1. The body plan and its corresponding
isometric view are shown in Fig. 1. According to the
common rule of classification societies, transverse sections
are numbered from aft to forward perpendiculars. Thus,
station 0 is on the stern and station 20 is on the bow.
Hull viscous damping of the same vessel is obtained by
the model test conducted by Wichers and Ji [24] at MARIN.
He divided the hull into four parts and determined the
associated resistance coefficients. Those viscous damping
coefficients in sway (normal) direction are shown in Fig. 2.
The in-line hull viscous damping is expected to be small,
thus not considered in the present simulations.
The turret supports 12 chain-wire-chain mooring system
and 13 catenary risers. Tables 2 and 3 show the main
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382368
particulars of the mooring system and the hydrodynamic
coefficients for them. The main particulars of the riser
system are shown in Table 4. The 12 anchor legs and
mooring lines are arranged in four groups, each group
having three anchor legs and 90-degree apart against each
other. The bottom-touching part of each leg consists of
studless Grade K4 chain terminating at the anchor pile. The
chain used for the top portion (Segment 3) is exactly the
same as that for Segment 1 except for the shortened length.
Schematic representation of the turret mooring system is
shown in Fig. 3. It follows from this figure that the x-axis
points to the East, y-axis points to the North, and z-axis
positive upwards. It is assumed that the initial ship
longitudinal axis coincides with the x-axis-bow to the East.
In the present study, 13 SCR are included. The prototype
riser particulars are shown in Table 4 while their
hydrodynamic coefficients are presented in Table 5. The
location of the risers is shown in Fig. 4 and angular
arrangement of each riser is listed in Table 6. It should be
noted that the risers are not symmetric with respect to the
x-axis. In the dynamic analysis for slender members,
tangential drag forces are expected to be negligible, thus
not included. The sea floor is modeled as elastic bed with
non-linear spring whose restoring force is proportional to
the displacement squared. The expected Coulomb friction
from the seabed and possible vortex induced vibration
(VIV) are not considered in the present simulations.
3. Environmental condition
A typical 100-year hurricane in the Gulf of Mexico with
significant wave height of 12.2 m and peak wave period of
14 s is selected as wave environment. As for wind, 1 h mean
wind speed (at 10 m height) of 41.1 m/s is used and the time
dependent wind velocity is generated from the correspon-
ding API wind spectrum. The wind direction is assumed to
be 30-deg left of waves. As for currents, a storm driven
Fig. 1. Body plan and isometric view of FPSO.
Table 1
Main particulars of turret-moored FPSO
Designation Symbol Unit Quantity
Vessel size KDWT 200
Length between perpendicular Lpp m 310
Breadth B m 47.17
Depth H m 28.04
Draft T m 18.90
Length beam ratio L=B 6.57
Beam draft ratio B=T 2.5
Displacement MT 240,869
Block coefficient Cb 0.85
Center of buoyancy forward of
section 10
FB M 6.6
Water plane area A m2 13,400
Water plane coefficient Cw 0.9164
Center of water plane area
forward of section 10
FA m 1.0
Center of gravity above base KG m 13.32
Metacentric height tranverse MGt m 5.78
Metacentric height longitudinal MGl m 403.83
Transverse radius of gyration
in air
Kxx m 14.77
Longitudinal radius of gyration
in air
Kyy m 77.47
Yaw radius of gyration in
air
KCC m 79.30
Wind area frontal Af m2 1,012
Wind area side Ab m2 3,772
Turret in center line behind
Fpp (20.5% LppÞ
m 63.55
Turret elevation below tanker base m 1.52
Turret diameter m 15.85
Fig. 2. Viscous damping coefficients over the length of FPSO hull.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382 369
shear current is assumed. The current is assumed to flow
from 30-deg right of wave direction. The non-collinear
environmental condition is summarized in Table 7.
The JONSWAP spectrum used here is the same as that
of Hasselman et al. (1973) with enhancement parameter
g ¼ 2:5 :
SðvÞ ¼ ag2v25 exp 21:25v
v0
� �24
" #g
exp 2ðv2v0Þ
2t2v20
� �ð1Þ
where g is the peakedness parameter, and t is the shape
parameter (0.07 for v # v0 and 0.09 for v $ v0Þ: The
value of a is related to a prevailing wind velocity of Uw and
a fetch of X; and can be written as
a ¼ 0:076ðXÞ20:22 ð2Þ
The shape of the JONSWAP spectrum used for the
present study is presented in Fig. 5.
The 1-hr wind speed used for the API wind spectrum is
based on the recurrence period of 100 years. The API wind
spectrum has the following expression.
SðvÞ ¼s2ðzÞ
2pfp 1 þ1:5v
2pfp
" #5=3ð3Þ
where fp is average factor derived from measured spectrum
and is given by
fp ¼0:025VwðzÞ
zð4Þ
The symbol sðzÞ is the standard deviation of wind speed
and related to turbulence intensity. The value of sðzÞ can be
expressed as
sðzÞ ¼ 0:15z
20
� �20:125
VwðzÞ ð5Þ
where VwðzÞ is the one hour mean wind speed (m/s) z meters
above water level. The corresponding wind velocity
spectrum used in the present study is plotted in Fig. 6.
The wind and current forces and moments on FPSO hull
are in general difficult to assess numerically, and thus have
to be estimated based-on empirical formulas. An
extensive experimental data set for wind and current forces
Table 4
Riser particulars
Designation Top tension
(kN)
OD
(mm)
AE
(kN)
Mass
(kg/m)
Dry/wet
(N/m)
Liquid prod. 1112.5 444.5 18.3 £ 106 196.4 1927/1037
Gas prod. 609.7 386.1 10.8 £ 106 174.1 1708/526
Water injection 2020.0 530.9 18.6 £ 106 285.7 2803/1898
Gas injection 1352.8 287.0 31.4 £ 106 184.5 1810/1168
Gas export 453.9 342.9 8.6 £ 106 138.4 1358/423
Cdn ¼ 1; except for water and gas injection ¼ 1.414.
Table 2
Main particulars of FPSO mooring system
Designation Unit Quantity
Pretension Kn 1201
Number of lines 4 £ 3
Degrees between the 3 lines deg. 5
Length of mooring lines m 2087.9
Radius of location of chain stoppers on turn table m 7.0
Segment 1 (ground section): chain
Length at anchor point m 914.4
Diameter mm 88.9
Dry weight kg/m 164.9
Wet weight kg/m 143.4
Stiffness AE kN 794841
Mean breaking load (MBL) kN 6515
Segment 2: wire
Length m 1127.8
Diameter mm 107.9
Dry weight kg/m 42.0
Wet weight kg/m 35.7
Stiffness AE kN 690168
Mean breaking load (MBL) kN 6421
Segment 3: chain
Length m 45.7
Table 3
Hydrodynamic coefficients for chains and wire
Coefficients to be used Symbol Chain Rope/wire
Drag normal Cdn 2.45 1.2
Added inertia coefficient normal Cin 2.0 1.15Fig. 3. General arrangement of mooring system.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382370
on FPSO-type hulls are available, and the results are
documented in a book published by OCIMF [17].
4. Wind and current loads using OCIMF data
For FPSO dynamic analysis, wind induced surge–sway–
yaw responses can be large because wind loading contains
significant energy close to the natural frequencies of
horizontal plane motions. For static equilibrium, both
wind and current forces are important.
The wind and current loading coefficients for typical
VLCCs at various heading angles are presented in OCIMF
document (1994). The resultant wind force and moment
acting on a tanker are then calculated from the following
equations
FXw ¼1
2CXwrwV2
wAT ð6Þ
FYw ¼1
2CYwrwV2
wAL ð7Þ
MXYw ¼1
2CXYwrwV2
wALLpp ð8Þ
where AT and AL are transverse and longitudinal projected
areas of the tanker above MWL. FXw;FYw; and MXYw are the
surge, sway wind forces and yaw wind moments, respec-
tively. CXw;CYw; and CXYw are the longitudinal, lateral
force and yaw moment coefficients, respectively. These
coefficients can be read from the graphs given for the
following conditions
1. Wind angle of attack: 180 8 (bow) to 0 8 (stern).
2. Two drafts: representing fully loaded and ballasted
tanker condition.
3. Two bows configuration: cylindrical bow and conven-
tional bulbous bow.
Similarly, current loading coefficients CXw;CYw; and
CXYw are also given in the OCIMF data set as function of
current angle of attack, water depth to draft ratio ðd=TÞ; the
bow configuration, and loading condition. In the present
study, we assumed that the tanker is fully loaded and has
cylindrical bow.
It should be noted that all the force coefficients of the
OCIMF data are presented with respect to the body-fixed
coordinate whose origin is at the mid-ship, and the
corresponding sign convention is shown in Fig. 7. Since
the origin of our earth-fixed global coordinate system is on
the center of the turret, the wind and current forces
calculated from the OCIMF data need to be transferred to
those with respect to the global coordinate system as follows
~FX
~FY
( )¼
cos u 2sin u
sin u cos u
" #FX
FY
( )ð9Þ
~MXY ¼ FY Xtur þ MXY ð10Þ
Table 5
Hydrodynamic coefficients for risers
Designation Symbol Coefficient
Drag normal Cdn 1.0
Added inertia coefficient normal Cin 1.0
Connection level below tanker base 1.52 m
Total length 1829 m
Fig. 4. General arrangement of the risers.
Table 6
Earth bound azimuthal arrangement of risers
Designation
Riser location (8)
Liquid prod. (LP) 0 90 180 270Gas prod. (GP) 45 135 225 315Water injection (WI) 165 337.5Gas injection (GI) 30 210Gas export (GE) 300
Table 7
Design environmental condition
Designation Unit Value
Waves
Hs m 12.19
Tp sec. 14
Wave spectrum JONSWAP ðg ¼ 2:5Þ
Wave direction deg. 180 (to West)
Wind
Wind speed (1-hr) m/s 41.12@10 m
Wind spectrum API RP 2A-WSD
Wind direction deg. 210
Storm current profile (linear between points)
Depth: 0 m m/s 1.07
60.96 m m/s 1.07
91.44 m m/s 0.09
Seabed m/s 0.09
Current direction deg. 150
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382 371
where ~FX ; ~FY ; and ~MXY are the surge, sway forces and yaw
moments with respect to the global coordinate system. The
symbol u is the instantaneous yaw angle of the vessel,
and Xtur is the distance between the center of turret and
the mid-ship.
5. Hydrodynamic computation using wamit
FPSO’s horizontal motions have smaller natural fre-
quencies than those of significant wave energy, and thus
more likely excited by second-order difference-frequency
wave forces. Therefore, the inclusion of the second-order
slowly varying wave forces in FPSO motion analysis is very
important. For the computation of hydrodynamic coeffi-
cients (added mass and radiation damping) and first- and
second-order wave forces, a second-order diffraction/radia-
tion program called WAMIT is used [12]. This program is
based on the three-dimensional panel method (boundary
integral equation method) and Green’s theorem with a free-
surface Green function.
The wetted surface of the vessel is discretized by
quadrilateral panels, as shown in Fig. 8. Smaller panels
were distributed near the waterline to enhance the accuracy
of waterline integrals used for second-order forces. For the
second-order computation, the free surface near the FPSO
also needs to be discretized, and it is shown in Fig. 9.
The FPSO hull, shown in Fig. 8, is symmetric
with respect to the x-axis. The symmetry is exploited in
the first- and second-order computation, and thus only half
domain is discretized, as shown in Fig. 9. For each half
domain, the body and free surface are discretized by 1843
and 480 panels, respectively. The truncation radius of the
free surface panels is 294 m from the turret. The
convergence of the difference-frequency QTFs is known
to be much faster than the sum-frequency QTFs. From
convergence test, the truncation radius and number of
panels are found to be sufficient for the desired accuracy of
the present study.
The wave force quadratic transfer functions are com-
puted for nine wave frequencies, ranging from 0.24 to
1.8 rad/sec and the intermediate values for other frequencies
are interpolated from them. In the present example and
frequency range of interest, the interpolated values were
found to be sufficiently accurate. For slowly varying surge
motions, only the QTF values near the diagonal are used.
The hydrodynamic coefficients and wave forces are
expected to vary appreciably with large yaw angles and the
effects should be taken into consideration for the reliable
prediction of FPSO global motions. Therefore, they are
calculated in advance for various yaw angles with 5-degree
interval and the data are tabulated as inputs.
The second-order diffraction/radiation computation for a
3D body is computationally very intensive especially when
it has to be run for various yaw angles. Therefore, many
researchers avoided such a complex procedure and have
instead used simpler approach called Newman’s approxi-
mation i.e. the off-diagonal components of the second-order
difference-frequency QTFs are approximated by their
Fig. 5. Wave spectrum.
Fig. 6. Wind velocity spectrum. Fig. 8. Grid modeling of body surface of FPSO.
Fig. 7. Sign convention and coordinate system for OCIMF data.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382372
diagonal values (mean drift forces and moments). The
approximation can be justified only when the relevant
natural frequency is very small and the slope of QTFs near
the diagonal is not large. In this paper, the full QTFs are
calculated and the validity of Newman’s approximation is
tested against more accurate results with complete QTFs.
6. Hull/mooring/riser coupled dynamic analysis
The non-linear hull/mooring/riser coupling character-
istics of turret-moored FPSOs in irregular waves are
investigated in this section. When water depth is large,
hull/mooring/riser coupling effects are expected to be
appreciable, and their dynamics should be solved simul-
taneously as an integrated system.
For the static/dynamic analysis of mooring lines and
risers, an extension of the theory developed for slender rods
by Garrett [4,16] was used. Assuming that there is no torque
or twisting moment, one can derive a linear momentum
conservation equation with respect to a position vector ~rðs; tÞ
which is a function of arc length s and time t :
2ðB~r00Þ00 þ ðl~r0Þ0 þ ~q ¼ m€~r ð11Þ
l ¼ T 2 Bk2 ð12Þ
where primes and dots denote spatial s-derivative and time
derivative, respectively, B is the bending stiffness, T the
local effective tension, k the local curvature, m the mass per
unit length, and ~q the distributed force on the rod per unit
length. The scalar variable l can be regarded as a Lagrange
multiplier. The rod is assumed to be elastic and extensible,
thus the following condition is applied
1
2ð~r·~r 2 1Þ ¼
T
AtE<
l
AtEð13Þ
where E ¼Young’s modulus, At ¼ Ae 2 Aið¼outer 2 inner
cross sectional area). For these equations, geometric non-
linearity is fully considered and there is no special
assumption made concerning the shape or orientation of
lines. The benefit of this equation is that Eq. (11) is directly
defined in the global coordinate system and does not require
any transformations to the local coordinate system, which
saves overall computational time significantly.
The normal component of the distributed external force
on the rod per unit length, qn;, is given by a generalized
Morison equation:
qn ¼ CIrAe _vn þ CD
1
2rDlvnrlvnr þ CmrAe€rn ð14Þ
where CI;CD and Cm are inertia, drag, and added mass
coefficients, and _vn; vnr; and €rn are normal fluid acceleration,
normal relative velocity, and normal structure acceleration,
respectively. The symbols r and D are fluid density and
local diameter. In addition, the effective weight, or net
buoyancy, of the rod should be included in qn as a static
load.
A finite element method similar to Garrett [4] has
been developed to solve the above mooring dynamics
problem and the details of the methodology are given in
Refs. [18,19]. The FEM allows any combination of mooring
types and materials as long as their deformations are small
and within proportional limit. The upper ends of the
mooring lines and risers are connected to the hull fairlead
through generalized elastic springs and dampers. The
combination of linear and torsional springs can model
arbitrary connection conditions. The forces and moments
proportional to the relative displacements are transmitted to
the hull at the connection points. The transmitted forces
from mooring lines and risers to the platform are given by
~FP ¼ ~Kð ~T~uP 2 ~uIÞ þ ~Cð ~T_~uP 2 _~uIÞ; ð15Þ
where ~K; ~C are stiffness and damping matrices of connectors
at the connection point, and ~T represents a transformation
matrix between the platform origin and connection point.
The symbols ~uP; ~uI represent column matrices for the
displacements of the platform and connection point.
Then, the following hull response equation can be
combined into the riser/mooring-line equations in the time
domain:
ð ~M þ ~Mað1ÞÞ€~up þð1
0
~Rðt 2 tÞ_~up dtþ ~KH ~up
¼ ~FD þ ~Fð1Þ þ ~Fð2Þ þ ~Fp þ ~Fw þ ~Fc þ ~FWD ð16Þ
where ~M; ~Ma are mass and added mass matrix,~R ¼retardation function (inverse cosine Fourier transform
of radiation damping) matrix, ~KH ¼hydrostatic restoring
coefficient, ~FD ¼drag force matrix on the hull,~Fð1Þ; ~Fð2Þ ¼first- and second-order wave load matrix on the
hull, ~Fp ¼transmitted force matrix from the interface,~Fw ¼dynamic wind loading, ~Fc ¼current loading on hull,
Fig. 9. Grid modeling of body and free surface of FPSO.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382 373
and ~FWD ¼wave drift damping force matrix. To check the
relative importance, the diagonal components of the wave-
drift-damping matrix were calculated in the frequency
domain by using the mean-drift-gradient method suggested
by Aranha [1]. The time series of wave drift damping can
then be generated based on Newman’s (diagonal) approxi-
mation. In the present FPSO study, the wave drift damping
is found to be small compared to hull viscous damping and
mooring/riser damping.
The added mass at infinite frequency was obtained from
Kramers–Kronig relation. For the time series of ~Fð1Þ; ~Fð2Þ;
and ~FWD; a two-term Volterra series was used [6]. The hull
drag force in the normal direction was calculated with
respect to the instantaneous hull position based on the
Morrison drag formular with relative velocity squared. Care
should be taken not to double count the effects of steady
current, since it is already given by OCIMF data.
The static problem of the integrated system was solved
using Newton’s iterative method. The dynamic problem was
integrated using an efficient and reliable time marching
scheme similar to Adams–Moulton method [4]. In the
dynamic program, special consideration is required due to
the fact that the time derivatives of l do not appear in the
equations and the added mass matrix is a function of the
instantaneous position. In addition, the free-surface fluctu-
ation and possible contact of mooring lines and catenary
risers with the seafloor require special consideration.
7. Results and analysis
The time-domain simulations of hull/mooring/riser
coupled statics/dynamics are conducted by a computer
program WINPOST. All the response results presented in
this paper are with respect to the center of turret.
Each mooring line is equally divided into five elements
for bottom chain, eight elements for wire, and one element
for upper chain (line connected to the body). Since high-
order elements and interpolation functions are used in the
present FEM, convergence characteristics are found to be
excellent, which was checked by doubling the number of
elements. The foot-print of the mooring line at the sea floor
is carefully defined by performing static analysis of each leg
and matching the pretension at the fairlead with that
described in Table 2.
All risers are modeled as steel catenary risers (SCRs)
where a certain length of the risers touch the seafloor. The
risers are equally divided into 12 elements, and connected to
the hinged joint at turret. The total number of degrees of
freedom in the combined matrix for the coupled analysis is
2773. The inertia and drag coefficients used are listed in
Table 5.
For irregular wave simulations, 51 wave components
with random phases are used. The frequency interval is
randomly perturbed to avoid periodical repetition (Kim and
Yue, 1991). The simulation is started with the tanker system
in the equilibrium position. A ramping function is
introduced to gradually increase the wave loading from
zero to its actual value during the first 50 s of simulation.
8. Numerical static offset and free-decay tests
The results of numerical static offset tests are shown in
Fig. 10. The surge stiffness as well as line tension on each
mooring line match well with the target values provided by
Wichers and Devlin [23].
For free decay simulation of surge, initial displacement is
given by applying appropriate surge force and then the
system is released. Subsequently, the free-decay response is
recorded in the duration of 2000 s with the time interval of
0.01 s. From the time series and using the concept of
logarithmic decrement, damping coefficients can be calcu-
lated. Generally, the tanker hull will be exposed to four
kinds of damping forces; radiation, viscous, wave-drift, and
wind damping. Viscous and wind damping are difficult to be
analyzed by mathematical models, and thus have to be
determined empirically. On the other hand, the radiation and
wave drift damping may be obtained numerically.
In the present study, the radiation damping is computed
using the panel method and the results of surge damping
coefficients are shown in Fig. 11. The present results are
compared with the numerical and model test results of
Wichers [22,24]. In the same figure, wave drift damping in a
large wave ðH ¼12.2 m ¼ significant wave height of 100-yr
hurricane) are also presented for comparison. The wave drift
damping is proportional to the wave height squared, but it
turned out that its magnitude in surge is smaller than the
radiation damping even in such large waves. It is also seen
that the measured damping is much greater than the
calculated radiation and wave drift damping, which reveals
that the viscous damping from hull/mooring/riser is
dominant over the potential-flow-related contributions.
However, the radiation damping can be important to
wave-frequency motions.
A typical time history of the surge free-decay test is
presented in Fig. 12. All mooring lines and risers are
included in this example. Wichers and Ji [24] included the
current effects, and therefore, their damping is larger.
Fig. 10. Surge static offset curve of FPSO.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382374
The surge natural periods (381 s) calculated from the free-
decay run are identical. It should be noted that all the free-
decay tests were carried out in calm water, therefore there is
no wave drift damping in it.
8.1. Simulation for 100-year Hurricane (non-parallel
wind and current)
In this section, the motion and tension characteristics of
the FPSO system are simulated in the time domain for a
non-parallel wind-wave-current environment (100-year
hurricane).
To better understand the role of each important
hydrodynamic contribution, several different cases inclu-
ding/excluding important hydrodynamic parameters are
selected as follows. As pointed out earlier, wind and current
force coefficients are stored for various yaw angles using
OCIMF data. Wave forces are calculated in advance and
tabulated with 5-degree yaw angle interval. The maximum
given in the tables is the actual maximum value obtained
from 3-h simulations. The time interval for the simulation
was 0.01 s. The contributions from wave drift damping and
wave-current interaction effects are shown to be small thus
not included in all cases considered here.
† Case 1: Newman’s approximation was used for second-
order difference frequency forces. Cross flow viscous
drag forces and moments on the hull were excluded.
Wave forces on hull are varied against yaw angles.
The hydrodynamic coefficients (added mass, radiation
damping, hydrostatic coefficients) are assumed to be
constant regardless of the change in yaw.
† Case 2: Same as Case 1, but cross-flow hull drag was
included. By comparing Case 1 and 2, the effects of hull
viscous drag can be directly observed.
† Case 3. Same as Case 2, but the full second-order
difference-force QTFs were used instead of Newman’s
approximation. The Newman’s approximation has been
widely used in offshore industry in FPSO motion
analyses, and its efficacy can be checked by comparing
against Case 2.
† Case 4. Same as Case 2 but the wind yaw moments were
increased by 19% to account for the effects of super
structures on deck. This case is similar to Wicher’s
[23,25] and direct comparison is possible.
† Case 5. Same as Case 4 but impose zero drag coefficients
on slender members. By comparing with Case 4, the
mooring/riser damping effects can be identified.
† Case 6. Same as Case 4 but the wave forces are
assumed to be constant (at the mean yaw angle) and
do not vary with yaw motions. The effects of
changing wave forces with yaw motions can be
directly observed.
In all cases, the vertical-plane motions (heave and pitch)
remain almost the same regardless of the variation of
methodology. Therefore, from now on, our discussions will
mainly be focused on horizontal-plane motions. In addition,
heave and pitch motions are dominated by wave-frequency
components and can be predicted pretty well even by linear
potential wave-body interaction theory.
8.2. Case 1 (Without hull viscous damping)
The hull-motion and riser/mooring tension results for
Case 1 are summarized in Table 8. Here, we can observe
that the slowly varying surge responses dominate wave-
frequency responses. It is also found that both wind forces
and wave forces are important to low-frequency responses.
Since hull viscous drag is not included, most of the
surge/sway damping is expected to come from risers and
mooring lines. However, their contributions to yaw mode
are small. The magnitudes of resonant slowly varying hull
responses are controlled by available damping. Neglecting
hull viscous damping, the low-frequency rms sway and yaw
motions of Case 1 are expected to be greatly overestimated.
Like surge and sway motions, slowly varying responses
dominate wave-frequency responses in yaw. The mean yaw
angle is primarily determined by the balance between
current and wind forces, and the contribution from the mean
wave drift yaw moment is relatively small. Therefore, the
mean yaw angle does not change much against different
methodologies.
Fig. 11. Surge radiation damping coefficients.
Fig. 12. The free decay test of FPSO.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382 375
8.3. Case 2 (With hull viscous damping)
In case 2, the cross-flow hull viscous drag is included.
Otherwise, the procedure would be the same as Case 1.
It should be noted that the hull drag in the normal
direction was calculated at the instantaneous yaw position
with Morison’s formula based on the relative velocity
(including wave kinematics) squared. The hull itself
was divided into several parts, and empirical damping
coefficients obtained from Wicher’s [23,25] experiment for
the same hull were assigned on each portion, which can be
seen in Fig. 2. The statistical results of Case 2 are
summarized in Table 8.
By including hull viscous drag, the rms values of sway
and yaw are greatly reduced, as expected. For sway, the
mean offset of Case 2 was increased by 65%, while the
standard deviation was decreased by factor of 3. For yaw,
the standard deviation was reduced by factor of 10.
Table 8
The results of Case 1,2 and 3
Vessel motions Case 1 Case 2 Case 3
Unit Mean Stdv Max Mean Stdv Max Mean Stdv Max
Surge total at turret m 244.0 17.0 283.3 238.2 10.6 261.3 240.2 10.9 264.2
Surge lf part m N/A 17.0 N/A N/A 10.6 N/A N/A 10.8 N/A
Surge wf part m N/A 0.6 N/A N/A 0.6 N/A N/A 0.6 N/A
Sway at turret m 8.4 11.6 35.1 13.9 3.3 23.8 17.0 6.0 36.0
Heave at turret m 0.0 2.3 7.8 0.0 2.3 7.8 0.0 2.4 7.4
Roll deg. 0.0 1.4 4.4 0.0 1.7 4.7 0.2 1.9 6.1
Pitch deg. 0.0 1.2 4.2 0.0 1.2 4.1 0.0 1.3 4.4
Yaw deg. 16.5 26.5 63.8 15.4 2.5 25.9 18.1 5.2 30.1
Mooring Tension (at fairlead)
Line#2 total kN 1779 290 2899 1653 169 2183 1683 176 2213
Line#2 lf part kN N/A 277 N/A N/A 151 N/A N/A 157 N/A
Line#2 wf part kN N/A 84 N/A N/A 77 N/A N/A 78 N/A
Line#8 total kN 847 184 2020 883 180 1921 871 183 1996
Riser Tension (at top)
Liquid prod. (line #13) kN 1315 184 2485 1298 181 2517 1301 184 2578
Water injection (line #22) kN 2275 278 4689 2254 276 4351 2264 279 4577
Gas export (line #25) KN 528 129 1494 528 128 1334 530 136 1850
Fig. 13. Surge and yaw difference frequency QTF of FPSO at 1708 of wave heading.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382376
Hence, neglecting the hull viscous damping can result in
serious overestimation of the rms yaw motions. The rms
surge motions are also appreciably decreased. The decrease
is mainly due to the reduction of slowly varying compo-
nents. Therefore, to predict reasonable dynamic/maximum
sway and yaw motions of a FPSO, the use of proper em-
pirical hull viscous drag is very important. It is also interes-
ting to see that the mean surge offset is reduced, while the
mean sway offset is increased after including hull drag effects.
It is also observed in a separate analysis that the rms
values of surge, sway, and yaw are slightly decreased if
wave kinematics are additionally included in the hull
viscous drag formula.
For other vertical-plane motions, such as heave, roll, and
pitch, the effects of hull viscous damping are almost
negligible. As a result of the change in global hull
motions, the rms tension on weather-side mooring (#2) is
significantly reduced, while that of lee-side mooring (#8) is
only slightly reduced.
8.4. Case 3 (With full QTF)
As mentioned before, Case 3 is the same as Case 2, but
the full second-order wave force/moment QTFs were used
instead of Newman’s approximation. The QTFs were
computed from the WAMIT second-order diffraction/radia-
tion panel program for various combinations of component
waves, which is computationally very intensive. The results
of Case 3 are listed in Table 8.
Compared to Case 2, the increase of sway and yaw can be
noticed. The most significant influence of using full QTF is
in yaw motion. The yaw standard deviation of Case 3 is
about twice higher than that of Case 2. For other quantities,
Case 3 and Case 2 are similar.
Fig. 14. Time history of Case 4 Response.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382 377
To better understand the increase of rms yaw motions by
using full QTF instead of Newman’s approximation, the
difference-frequency surge-force and yaw-moment QTFs are
plotted in the bi-frequency domain in Fig. 13. It is seen that
some off-diagonal components of yaw are much larger than
the diagonal values, which may be the reason for
the appreciable increase in slowly varying yaw responses.
From this comparison, it can be concluded that care needs to
be taken using Newman’s approximation especially when the
input sea spectrum is not narrow-banded or double-peaked.
8.5. Case 4: (Comparisons with MARIN’s results)
Case 4 is the same as Case 2 except that the yaw wind-
drag coefficients from the OCIMF data are increased by
19%, as suggested by ABS rule (1996), to compensate
additional forces due to superstructure and equipment above
the deck, which are not included in the OCIMF data. For this
case, the time histories of the 6DOF hull motions and
mooring(line#2)/riser(line#22) tension are given in Fig. 14.
The corresponding spectra are also plotted in Fig. 15. From
those figures, we can directly see that slowly varying
components dominate wave-frequency components for
horizontal-plane motions (surge, sway, yaw), while
the opposite is true for vertical-plane responses (heave,
pitch, roll).
Wichers and Delvin [23] conducted a similar numerical
analysis for the same FPSO considered here and it was
based on the methodology similar to Case 4. However, their
drag coefficients Cd ¼ 1 for risers and mooring lines are
Fig. 14 (continued )
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382378
slightly different from the Cd value 1.2 used in this paper.
The statistical results of Case 4 and Wichers [23] are
presented in Table 9.
Wichers [23] also conducted a series of experiments for
the same environment and FPSO design in MARIN’s new
wave basin. However, the lab generated current and wind
field did not exactly match with the target values. The FPSO
model was built with extra bulwark at the bow to avoid
green water on the deck, so the resulting wind loading is
expected to be different from the OCIMF-data-based
prediction. In addition, VIV of slender members were
also reported and the resulting in-line drag coefficients
are expected to increase under such circumstances.
The turbulence or unsteadiness of the current generated in
the experiment may also influence the discrepancy. Even the
direction of the currents fluctuated case by case. It is also
questionable that the lab-generated wind force is close to
OCIMF-based numerical evaluation.
Despite these and other uncertainties, the comparisons
between the current tension/global-motion prediction and
the measured values are reasonable. In particular,
the agreement for heave and pitch motions is excellent.
Better agreement can be achieved by modeling the model
and adjusting empirical parameters, such as drag coeffi-
cients, through calibration. However, no effort is made in
this paper for that purpose. In the present study, the roll
Fig. 15. Response Spectrum of Case 4.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382 379
viscous damping is not added, and thus roll rms motions are
expected to be over-predicted. This can be easily fixed by
adding empirical roll viscous damping of FPSO hull.
One noticeable discrepancy between the present predic-
tion and MARIN’s experiment is the mean yaw angle,
which is determined mainly from the balance between wind
and current forces on the hull. Whereas, the yaw rms values
are reasonably predicted.
Similar comparisons can also be made for the statistics of
riser/line tension. For taut line #2, the rms values of Case 4
are lower than those of the experiment, but the mean values
are almost the same. There exists similar trend for the mean
and rms tension of risers. The discrepancy in rms values
may be associated with the observed VIV in the experiment.
8.6. Case 5 (No drag on mooring/riser)
In Case 5, the same simulation as Case 4 is repeated with
the zero drag coefficients on risers and mooring lines to see
their effects on hull motions. However, the inertia and added
mass effects of the slender members are taken into
consideration. Since those inertia effects are expected to
be less important than damping and drag forces, this case is
similar to the uncoupled analysis, where the slender
members are treated as massless non-linear springs. The
major difference of this case compared to Case 4 is the
significant increase in surge and sway rms values. It is
mainly due to the absence of riser/mooring viscous
damping. As a result, the corresponding riser/mooring
dynamic tension is greatly over-predicted. For instance,
the over-prediction of dynamic tension for #13 riser can be
as large as factor of 3. On the other hand, the mean surge
offset is appreciably decreased with Cd ¼ 0: This example
typically shows the importance of hull/mooring/riser
fully coupled analysis for the global motion analysis of
turret-moored FPSOs in deep water.
8.7. Case 6 (With yaw-independent wave forces)
In Case 6, the same methodology as Case 4 is repeated by
assuming that the wave forces do not change with yaw
angles, which is a typical assumption used for the motion
analysis of floating platforms other than turret-moored
FPSOs. Under that assumption, the first- and second-order
wave forces are calculated at the mean yaw angle, and the
same values are used for all the other yaw angles during the
entire simulation. Using this approximation, the rms surge
and sway are slightly increased, while rms yaw is decreased.
On the other hand, the mean sway and yaw are appreciably
over-predicted. The increase of mean yaw is particularly
noticeable. This phenomena can partly be explained by the
mean surge drift forces and mean yaw moments plotted for
several different wave headings in the neighborhood of the
mean yaw angle, as in Fig. 16. It can be seen that the mean
yaw moments are more sensitive to the change of yaw
angles than the mean surge drift forces near the
spectral peak. The yaw-dependent wave forces should be
taken into consideration when yaw motions are large,
particularly in multi-directional waves and crossed-wave
conditions (Table 10).
Up to this point (Case1–6), all the time-domain
simulations were carried out by assuming that the added
Table 9
The results of analysis of Case 4 and [23,25]
Vessel motions Unit Case 4 Stdv Max Refs. [23,25] Stdv Max
Mean Mean
Surge total at turret m 238.1a 10.6b 261.4a 242.1a 16.2c 296.4a
Surge lf part m N/A 10.6 N/A N/A N/A N/A
Surge wf part m N/A 0.6 N/A N/A N/A N/A
Sway at turret m 14.0a 3.2b 28.4a 16.6b 4.1b 30.5a
Heave at turret m 0.0a 2.3a 8.0a N/A N/A N/A
Roll deg 0.1 1.7 4.80 N/A N/A N/A
Pitch deg 0.0a 1.2a 4.2a N/A N/A N/A
Yaw deg 15.5c 2.4a 26.5b 12.0b 2.6a 21.2a
Mooring tension (at fairlead)
Line#2 total kN 1651a 170b 2149b 1743a 351b 3433a
Line#2 lf part kN N/A 151 N/A N/A N/A N/A
Line#2 wf part kN N/A 71 N/A N/A N/A N/A
Line#8 total kN 884 180 1774 876 201 1985
Riser Tension (at top)
Liquid prod. (line #13) kN 1299a 181a 2653a 1182 þ 292 þ 3921d
Water injection (line #22) kN 2252a 276a 4179a 2149a 363a 5481b
Gas export (line #25) kN 528 þ 129a 1395a 482a 202b 2514d
a The difference between prediction and MARIN’s experiment can be described as within 25%.b The difference between prediction and MARIN’s experiment can be described as 25–50%.c The difference between prediction and MARIN’s experiment can be described as 100–200%.d The difference between prediction and MARIN’s experiment can be described as 50–100%.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382380
mass and radiation damping of FPSO hull do not vary with
yaw angles. We also examined the validity of this
assumption by actually calculating and using the yaw-
angle dependent added mass and radiation damping. It is
seen that all the results are only slightly changed (rms
difference less than 5%), which implies that the variation of
added mass and radiation damping can be neglected unless
yaw angles are very large.
9. Summary and conculsions
Hull/mooring/riser coupled dynamics analysis of a
turret-moored FPSO in non-parallel winds, waves, and
currents was conducted for six different cases to better
understand the motion characteristics, coupling effects, and
the role of various hydrodynamic contributions. The first-
and second-order wave forces, added mass, and radiation
damping were computed by a second-order diffraction/ra-
diation panel program for various yaw angles. The two-term
Volterra series model was then adopted for the generation of
the time series of first- and second-order wave loads in
irregular waves. The current and wind loading for various
yaw angles of hull were obtained from OCIMF empirical
data. The mooring/riser dynamics were modeled using a
generalized-coordinate-based rod theory and finite element
method. Then, the dynamics of hull, mooring lines, and
risers were solved simultaneously in a combined matrix
(fully coupled analysis) at each time step.
From the six different cases of simulations, the following
conclusions can be drawn.
† The slowly varying responses dominate wave-frequency
responses in surge, sway, and yaw, while wave-frequency
responses are more important for heave, roll, and pitch.
† The mean yaw angle is mainly controlled by the balance
of current and wind forces on hull, and the contribution
of the wave drift mean yaw-moment is less important.
The reliable computation of yaw mean offset and rms
responses plays an important role in obtaining reasonable
surge and sway responses.
† The inclusion of proper empirical value for hull viscous
damping is very crucial to reasonable estimate of
Table 10
The results of analysis of Case 5 and Case 6
Vessel motions Unit Case 5 Case 6
Mean Stdv Max Mean Stdv Max
Surge total at turret m 233.4 27.1 2102.7 241.4 10.9 266.22
Surge lf part m N/A 27.1 N/A N/A 10.9 N/A
Surge wf part m N/A 0.9 N/A N/A 0.6 N/A
Sway at turret m 12.6 9.3 35.3 16.8 3.8 25.7
Heave at turret m 0.0 2.4 8.7 0.0 2.3 7.9
Roll deg. 0.1 1.8 6.1 0.1 1.8 4.9
Pitch deg. 0.0 1.3 4.8 0.0 1.2 4.3
Yaw deg. 16.8 4.5 28.8 22.9 2.1 28.3
Mooring Tension (at fairlead)
Line#2 total kN 1644 547 4235 1701 179 2212
Line#2 lf part kN N/A 383 N/A N/A 161 N/A
Line#2 wf part kN N/A 361 N/A N/A 78 N/A
Line#8 total kN 987 324 3183 864 179 1972
Riser Tension (at top)
Liquid prod. (line #13) kN 1328 540 5958 1304 187 2335
Water injection (line #22) kN 2272 560 6244 2266 277 4097
Gas export (line #25) kN 554 294 3386 533 135 1491
Fig. 16. Surge and yaw mean drift forces LTF of FPSO.
A. Tahar, M.H. Kim / Applied Ocean Research 25 (2003) 367–382 381
horizontal plane motions. For slowly varying horizontal-
plane responses, viscous damping from hull, mooring,
and risers is much greater than radiation and wave drift
damping.
† The use of full second-order force QTFs increases sway
and yaw rms (slowly varying) responses. The influence
will be more important for broader or double-peaked
sea energy spectra. Otherwise, the motion prediction
based on the Newman’s approximation is pretty
reasonable.
† When uncoupled analyses are used and drag forces on
mooring/riser are neglected, surge and sway rms
responses can be significantly increased and riser/moor-
ing dynamic tension can be greatly over-predicted.
The use of yaw-independent wave forces (at mean yaw)
may be reasonable when yaw motions are not large.
Otherwise, or in multi-directional waves and crossed
waves, yaw dependent wave forces have to be used.
The present numerical results are compared with
MARIN’s experiments. The overall comparisons for
6DOF motions and mooring/riser tensions are reasonable
considering the various uncertainties involved with physical
model testing. In particular, the wave-frequency responses
match very well against measured values. The comparison
of slowly varying responses could be further improved by
using the actual lab-generated environment and calibrating
the empirical coefficients.
The present study has clearly demonstrated the role of
various hydrodynamic contributions in the prediction of the
motions of a turret-moored FPSO in non-parallel winds,
waves, and currents, and thus will help researchers and
engineers to develop their own methodology and numerical
tools in the future.
Acknowledgements
The present FPSO research was financially supported by
Minerals Management Service (MMS), Offshore Technol-
ogy Research Center (OTRC), and also partly by a Joint
Industry Project (BP-Amoco, CSO-Aker, Conoco, Brown
and Root, Sea Engineering).
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