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Journal of
Marine Science
and Engineering
Article
Numerical Investigation into Freak Wave Effects on
Deepwater Pipeline Installation
Pu Xu 1, *, Zhixin Du 1
1
2
*
and Shunfeng Gong 2
College of Civil Engineering, Fuzhou University, Fuzhou 350116, China; [email protected]
Institute of Structural Engineering, Zhejiang University, Hangzhou 310058, China; [email protected]
Correspondence: [email protected]
Received: 18 January 2020; Accepted: 3 February 2020; Published: 14 February 2020
Abstract: Freak waves are an extreme marine environment factor in offshore structure design and
become a potential risk, particularly for laying oil-gas pipelines in deep waters. The objective of this
study was to reveal the freak wave effects on dynamic behaviors of offshore pipelines for deepwater
installation. Thus, a dedicated finite element model (FEM) for deepwater pipeline installation by the
S-lay method was developed with special consideration of freak waves. The FEM also took pipelay
vessel motions, pipe–stinger roller interactions, and the cyclic contacts between the pipeline and
seabed soil into account. Real vessel and stinger data from an actual engineering project in the South
China Sea were collected to obtain an accurate simulation. Moreover, an effective superposition
approach of combined transient wave trains and random wave trains was introduced, and various
types of freak wave trains were simulated. Extensive numerical analyses of a 12 inch gas pipeline
being installed into a water depth of 1500 m were implemented under various freak wave conditions.
The noticeable influences of freak waves on the pipeline and seabed responses were identified, which
provides significant awareness of offshore pipelines for deepwater installation design and field
operation monitoring.
Keywords: offshore pipeline; installation simulation; deepwater; freak wave; S-lay method
1. Introduction
Freak waves occur unexpectedly far out at sea with remarkably large wave heights and are
deemed to be an extreme marine environment condition. The irregular distribution of freak wave
heights does not comply with the basic law of Rayleigh distribution for normal ocean waves, especially
in deep waters. The unique feature of freak waves makes it difficult for marine structural engineers
to sufficiently consider the huge wave loads in the design stage. In the past, plenty of tremendous
accidents, including shipwrecks and massive destruction of offshore structures, have been caused
by the great impact of freak waves [1,2]. These accidents have produced a striking warning on the
potential risk of freak waves for lay barge and offshore structures and have attracted wide attention on
the investigation into freak-wave-induced structural responses.
The offshore pipeline is a representative type of marine structure that is widely utilized for crude
oil and natural gas transportation from subsea well sites to surface processing facilities. In recent
years, the great demand for energy resources has facilitated the expansion of oil-gas exploitation
into deepwater areas. The S-lay approach is one of most common methods of deepwater pipeline
installation to the sea floor owing to its excellent adaptability and workability [3]. In this pipelay
technique, numerous section pipes with designed lengths are welded and inspected on the operating
lines of the vessel. The qualified pipeline is drawn by the tensioners and slides over the stinger to
arrive at the seabed. The overall pipeline is characterized as an S-shaped curve and divided into two
regions, as displayed in Figure 1. The upper curved section of the pipeline from the tensioner to the
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J. Mar. Sci.
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lift-off
point
denoted as the overbend, and the suspended section from the LOP to the seabed
is known as the sagbend. The whole process of laying the pipeline generally takes months or even
is known as the sagbend. The whole process of laying the pipeline generally takes months or even
longer periods, and is more likely to encounter the occurrence of freak waves. Therefore, to assess
longer periods, and is more likely to encounter the occurrence of freak waves. Therefore, to assess
the influences of freak waves on the dynamic behaviors of S-laying pipelines in deep waters is highly
the influences of freak waves on the dynamic behaviors of S-laying pipelines in deep waters is highly
significant for the purpose of pipelay design and operation safety.
significant for the purpose of pipelay design and operation safety.
z
Sea level
Heave
Sway
Yaw
y
Freak wave
Pitch
Surge
x
o Vessel Tensioner
Roll
Overbend
Stinger
Current
LOP
Pipelin
Sagbend
TDZ
TDP
Seabed
Figure 1. Deepwater pipeline installation by the S-lay method under exposure to freak waves.
Figure 1. Deepwater pipeline installation by the S-lay method under exposure to freak waves.
A reasonable wave generation method is necessary to simulate freak waves and explore their
impact
marine structures.
A numerical
is extensively
due and
to itsexplore
convenient
A on
reasonable
wave generation
methodtechnique
is necessary
to simulateemployed
freak waves
their
simulation
and
good
repeatability.
Davis
and
Zarnick
[4]
initially
proposed
a
wave
focusing
method
impact on marine structures. A numerical technique is extensively employed due to its convenient
to
simulate and
freakgood
waves
by controlling
theand
focalized
time
space.
Subsequently,
al. [5]
simulation
repeatability.
Davis
Zarnick
[4] and
initially
proposed
a wave Baldock
focusinget
method
applied
the
technique
to
accumulate
numerous
water
waves
and
produce
a
huge
transient
wave
group.
to simulate freak waves by controlling the focalized time and space. Subsequently, Baldock et al. [5]
Fochesato
et technique
al. [6] superposed
wave trains
of different
to generate
(3D)
applied the
to accumulate
numerous
waterdirections
waves and
produce three-dimensional
a huge transient wave
freak
waves.
Zhao et
four
focusing
to generate
the freak
trainsthreeand
group.
Fochesato
et al.
al.[7,8]
[6] presented
superposed
wave
trainsmodels
of different
directions
to wave
generate
numerically
simulated
the
wave
effect
on
a
floating
structure.
Liu
et
al.
[9]
developed
a
modified
dimensional (3D) freak waves. Zhao et al. [7,8] presented four focusing models to generate the freak
phase
modulation
approach to
focus wave
trainseffect
with on
thea specified
phase and
obtained
precise
wave trains
and numerically
simulated
the wave
floating structure.
Liu
et al. [9]the
developed
wave
spectrum
that
coincided
well
with
the
target
results.
Hu
et
al.
[10]
employed
a
probability-based
a modified phase modulation approach to focus wave trains with the specified phase and obtained
superposition
method
to calculate
the generation
of a freak
wave.
Tang
et al. [11]a
the precise wave
spectrum
that coincided
well probability
with the target
results.
HuRecently,
et al. [10]
employed
improved
the phase
modulation model
a freak
wave and probability
investigatedofitsa effect
the
probability-based
superposition
methodtotogenerate
calculate
the generation
freak on
wave.
dynamic
responses
of
the
Floating
Production
Storage
and
Offloading
(FPSO)
and
Single
Point
Mooring
Recently, Tang et al. [11] improved the phase modulation model to generate a freak wave and
(SPM)
system.
et on
al. the
[12]dynamic
conducted
extensive
to observe
the greatStorage
differences
cylinder
investigated
itsPan
effect
responses
of tests
the Floating
Production
and in
Offloading
motion
under
waves
and
freak waves
obtained
the important
influencing
factors.
(FPSO)responses
and Single
Pointirregular
Mooring
(SPM)
system.
Pan etand
al. [12]
conducted
extensive
tests to observe
The
wave
focusing
and
superposition
techniques
were
demonstrated
to
effectively
generate
freak
the great differences in cylinder motion responses under irregular waves and freak waveswave
and
trains,
which
a prior
simulation
of theThe
wave
impact
on pipeline
installation in techniques
deepwater areas.
obtained
theprovided
important
influencing
factors.
wave
focusing
and superposition
were
Under theto
excitation
of surface
vessel
motions,
laying apipelines
usually exhibit
demonstrated
effectively
generatewaves
freak and
wave
trains,
which the
provided
prior simulation
of the
sophisticated
non-linear,
dynamic
responses.
The
complicated
S-lay
problems
mainly
result
from
large
wave impact on pipeline installation in deepwater areas.
pipeline
deflections,
pipe material
plasticity,
hydrodynamic
loads,the
and
boundary
interactions.
These
Under
the excitation
of surface
waves and
vessel motions,
laying
pipelines
usually exhibit
non-linear
features
could
cause
some
difficulties
for
analytical
approaches
and
experimental
tests
to
sophisticated non-linear, dynamic responses. The complicated S-lay problems mainly result from
obtain
accuratedeflections,
and comprehensive
simulations.
As ahydrodynamic
consequence, numerical
preferred
large pipeline
pipe material
plasticity,
loads, andtechniques
boundaryare
interactions.
for
modeling
systematical
of offshore
pipelines for
in the
S-lay process
[13–15].
Gong
et al. [16]
These
non-linear
features behaviors
could cause
some difficulties
analytical
approaches
and
experimental
and
Gong
and
Xu
[17]
developed
a
full
FEM
on
the
basis
of
OrcaFlex
to
simulate
the
structural
behaviors
tests to obtain accurate and comprehensive simulations. As a consequence, numerical techniques are
of
pipelinefor
installation
and explored
the influence
of normal
sea states
on the
pipeline
responses.
preferred
modeling systematical
behaviors
of offshore
pipelines
in the S-lay
process
[13–15].
Gong
Ivić
et [16]
al. [18,19]
established
a pipeline
laying model
the on
usethe
of non-linear
elastic beam
elementsthe
to
et al.
and Gong
and Xu
[17] developed
a fullby
FEM
basis of OrcaFlex
to simulate
structural behaviors of pipeline installation and explored the influence of normal sea states on the
pipeline responses. Ivić et al. [18,19] established a pipeline laying model by the use of non-linear
elastic beam elements to analyze the static behaviors of the S-laying pipe and formulated a specialized
J. Mar. Sci. Eng. 2020, 8, 119
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analyze the static behaviors of the S-laying pipe and formulated a specialized optimization method for
the pipeline laying operation. Xie et al. [20] investigated the dynamic loading history of laying pipelines
in light of a test-verified FEM and confirmed obvious pipeline plastic deformations resulting from the
S-lay operation. Cabrera-Miranda and Paik [21] quantified the probabilistic distribution of loads on a
marine riser and observed the highly random characteristic of the loads to aid in the determination of
nominal design values. Wang et al. [22] pointed out the probable underestimation of pipeline dynamic
behaviors for practical engineering and built a real-time installation monitoring system to predict
on-site pipeline responses. Recently, Liang et al. [23,24] presented a refined FEM to take account of the
complex surface contact behaviors of overbend pipes and reproduced the pipe laying process of a deep
S-lay case in the laboratory. Kim and Kim [25] employed the FEM-based linear beam element to present
an efficient, linearized, dynamic analysis approach for pipeline installation design. The aforementioned
studies usually adopted normal random waves as the input ocean conditions to calculate the dynamic
responses of laying pipelines. The neglect of the freak wave effect could result in the inadequacy of
pipeline installation design for field operation safety.
The objective of this study was to thoroughly investigate the freak wave effects on the dynamic
responses of offshore pipelines during deepwater S-lay installation. A new extended FEM with
particular consideration of freak waves was developed on the basis of our previous model [16] for S-lay
pipelines. This model took the induced vessel motions, pipe–stinger roller contacts, and pipe–seabed
soil interactions into account. The real vessel, stinger roller, and seabed soil data from an actual
engineering project in South China Sea were collected to obtain an accurate simulation. Furthermore,
an effective superposition technique was employed to generate freak waves by combining transient
wave trains and random wave trains. The insertion of various freak wave trains into the S-lay FEM was
then implemented to carry out a large number of numerical analyses of a 12 inch gas pipeline being
installed into a 1500 m water depth. Finally, the influences of the freak wave energy ratio coefficient,
focusing location, phase range, and peak value were sufficiently assessed on the pipeline and seabed
responses. The dynamic amplification factors (DAFs) of the axial tension, bending moment, von Mises
stress, longitudinal strain, pipeline embedment, and seabed resistance are discussed in detail in relation
to pipeline installation design and field operation safety.
2. Deepwater Pipeline Installation Simulation
A reasonable FEM for S-lay system was presented by Gong et al. [16] to explore the random wave
effects on the dynamic behaviors of deepwater pipeline installation. This model, developed within
the framework of OrcaFlex [26], was validated with acceptable accuracy and effective applicability
by an actual engineering case of S-laying pipelines. In this study, a new extension of the FEM
was implemented to consider the freak waves with wave-induced pipeline behaviors, pipe–stinger
roller contacts, pipe–seabed soil interaction, and pipelay vessel motions, as displayed in Figure 1.
The following section presents a concise description of the main features of the deepwater pipeline
installation model by the S-lay technique.
2.1. Pipeline Model
In the FEM of the S-lay system, the entire pipeline, from the tensioner to the sea floor, was
discretized into a sequence of mass nodes connected together by massless line segments, as displayed
in Figure 2. The local xyz-frames of references for the node and line segment were established, and the
mechanical properties of the pipe weight, buoyancy, drag force, and so on for each half-segment were
concentrated on its adjacent node. At either side of the node, two rotational springs and dampers were
employed to model the bending stiffness and damping of the line segment. At the center of the line
segment, an axial spring with a damper was utilized to represent its axial stiffness and damping, and a
torsional spring with a damper was applied to characterize its torsional stiffness and damping. For the
detailed calculation derivation of the tension force, bending moment, and torque moment, one can
refer to the literature [16], and their expressions are given by
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Te = Tw (ε) + (1 − 2ν) · (Po Ao − Pi Ai ) + EAnom · ξ · (dL/dt)/L0
J. Mar. Sci. Eng. 2020, 8, 119
(1)
4 of 22
M2 = Mb (κ2 ) + ς · (dκ2 /dt)
(2)
(2)
(3)
(3)
where Te and Tw are the effective tension and wall tension relating to the axial strain; Pi and Po are the
e and Tw and
are the
effective
tension
tension
relatingand
to the
axial cross-section
strain; Pi andareas;
Po areνthe
where Tpressure
internal
external
pressure;
Aiand
andwall
Ao are
the internal
external
is
internal
pressure
pressure;
i andstiffness
Ao are the
internal
and external
areas; ν
the
Poisson’s
ratio;and
EAexternal
nominalAaxial
defined
at zero
strain; L cross-section
is the instantaneous
nom is the
is the Poisson’s
EAnom
axiallength
stiffness
defined
at zero strain;
is the
instantaneous
length
of the lineratio;
segment;
L0isisthe
thenominal
unstretched
of the
line segment;
Mb isLthe
bending
moment
length oftothe
segment;
0 is
unstretched
lengthrelating
of the line
segment;
Mb is the
bending
moment
relating
theline
curvature
κ2 ;LT
is the
torque moment
to the
twist angle
ϕ; and
the damping
or the
relating to the
κ2; Tor isrepresent
the torque
moment
relating
to the twist
angle
and thedamping.
damping
coefficients
ξ, ς curvature
and ζ separately
axial,
bending,
and torsional
effects
of φ;
structural
coefficients
ξ, ς and
ζ separately
represent
bending,
andcarbon–manganese
torsional effects of steel
structural
The oil-gas
pipelines
installed
in deepaxial,
waters
comprise
with adamping.
distinct
pipelines
in deep
waters comprise
carbon–manganese
a distinct
yield The
pointoil-gas
and some
plasticinstalled
deformation
capability.
The pipeline
material featuressteel
werewith
simulated
by
yield
pointtheory
and some
plastic deformation
The pipeline
material features
were simulated
the
J2 flow
of plasticity
performancecapability.
with isotropic
strain hardening.
The Ramberg–Osgood
by the [27]
J2 flow
of plasticity
performance
withstress
isotropic
The
model
wastheory
applied
to represent
the non-linear
andstrain
strainhardening.
relationship
ofRamberg–Osgood
the adoptive X65
model
[27]
was applied
representasthe non-linear stress and strain relationship of the adoptive X65
line
pipe,
which
could betoexpressed
line pipe, which could be expressed as
ε(σ) = σ/E + B(σ/σy )n n
(4)
ε (σ ) = σ / E + B(σ / σ y )
(4)
where σy is the effective yield stress, E is the elastic modulus, and B and n are the coefficient and the
where σ y is the effective yield stress, E is the elastic modulus, and B and n are the coefficient and
power exponent
of the constitutive model.
the power exponent of the constitutive model.
M 2 = M b (κ 2 ) + ς ⋅ (dκ 2 / dt )
Tt = Tor (φ/L0 ) + ζ · (dφ/dt)
T t= Tor (ϕ / L0 ) + ζ ⋅ (dϕ / dt )
Segment
Nx
Nz
α1
Sx1
Sx2 φ
Sy2
Sy1
Ny
Axial spring
+damper
Node
α2
Node…
Sz1
Sz2
Bending spring
+damper
Torsion spring
+ damper
Segment…
Figure
Figure2.2. Node
Node and
and line
line segment
segment model
modelof
ofthe
theS-lay
S-laypipeline.
pipeline.
2.2. Pipe–Stinger Roller Interaction
2.2. Pipe–Stinger Roller Interaction
In the overbend, the sections of the pipeline were continuously supported by 10 roller boxes that
In the overbend, the sections of the pipeline were continuously supported by 10 roller boxes that
were regularly spaced and settled on the articulated stinger, which was 75 m in length, as illustrated
were regularly spaced and settled on the articulated stinger, which was 75 m in length, as illustrated
in Figure 3. The stinger with three sections of truss structure was collected from the actual design
in Figure 3. The stinger with three sections of truss structure was collected from the actual design for
for the Hai Yang Shi You (HYSY) 201 pipelay vessel [28]. A group of pipe segments was employed
the Hai Yang Shi You (HYSY) 201 pipelay vessel [28]. A group of pipe segments was employed to
to simulate the stinger’s geometrical and mechanical properties. The clashing contacts between the
simulate the stinger’s geometrical and mechanical properties. The clashing contacts between the
pipeline and stinger rollers would vary with the vessel motions. Before the calculation of pipe–stinger
pipeline and stinger rollers would vary with the vessel motions. Before the calculation of pipe–stinger
roller interactions, an inspection had to be implemented to confirm whether the pipeline was in contact
roller interactions, an inspection had to be implemented to confirm whether the pipeline was in
with the roller. If a mutual interaction was identified, the contact force was calculated and applied to
contact with the roller. If a mutual interaction was identified, the contact force was calculated and
the pipe and the roller, which was given by
applied to the pipe and the roller, which was given by
Fr = [1/(1/k1 + 1/k2 )] × [d − (r1 + r2 )]
(5)
Fr = [1 / (1 / k1 + 1 / k 2 )]× [d − (r1 + r2 )]
(5)
where k1 and k2 are the contact stiffness of the pipe and the roller, d is the shortest separation distance
of the center lines between them, and r1 and r2 are the corresponding radii.
Pipe
Roller
Roller box
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(a)
where
k1Eng.
and2020,
k2 are
the
J.
Mar. Sci.
8, 119
contact stiffness of the pipe and the roller, d is the shortest separation distance
5 of 22
of the center lines between them, and r1 and r2 are the corresponding radii.
(b)
Pipe diagram of the deepwater S-lay stinger: (a) Pipe–roller interaction; (b) articulated
Figure 3. Schematic
stinger of the Hai Yang Shi You (HYSY) 201 vessel.
Roller
2.3. Pipe–Seabed Soil Interaction
Roller box
At the touchdown
zone (TDZ), the laying pipeline was freely supported by the seabed soil,
(a)
which was liable to be trenched and remolded under dynamic installation in deep waters. In the
vertical plane, the dynamic features of the cyclic pipe–seabed interactions were simulated by a nonlinear hysteretic soil model with hyperbolic secant stiffness formulations [29], as shown in Figure 4.
(b)
In this model, four types of pipe–soil penetration modes were applied to characterize the cyclic
variations of the pipeline periodic embedment into the seabed. For the not-in-contact pattern, the
Figure
3. Schematic
diagram
of the
deepwater
S-lay
stinger:
(a) Pipe–roller
interaction;
(b) articulated
seabed
resistance
P(z) is
naturally
zero.
For other
three
patterns,
including
initial penetration,
uplift,
Figure
3. Schematic
diagram
of the
deepwater
S-lay
stinger:
(a) Pipe–roller
interaction;
(b) articulated
stinger
of
the
Hai
Yang
Shi
You
(HYSY)
201
vessel.
and repenetration,
the
relationships
between
the seabed resistance P(z) and the penetration z nonstinger of the Hai
Yang
Shi You (HYSY)
201 vessel.
linearly
vary
in
hysteretic
cycles
with
the
incessant
shift of the penetration modes.
2.3. Pipe–Seabed Soil Interaction
In another Soil
view
of the horizontal plane, the lateral and axial pipe–seabed interactions were
2.3. Pipe–Seabed
Interaction
At theby
touchdown
zoneCoulomb
(TDZ), the
layingmodel,
pipeline
was freely
supported
by the
seabed soil,
simulated
the modified
friction
which
expressed
the lateral
resistance
andwhich
axial
At thetotouchdown
zoneremolded
(TDZ), the
laying
pipeline
was freely
supported
by
thevertical
seabedplane,
soil,
was
liable
be
trenched
and
under
dynamic
installation
in
deep
waters.
In
the
friction force with the deflection as a bilinear equation, as illustrated in Figure 5. When the lateral
which
was liable
to be
trenched
and
remolded
under dynamic
installation
in
deep waters.
In the
the
dynamic
features
of
the
cyclic
pipe–seabed
interactions
were
simulated
by
a
non-linear
hysteretic
displacement y varies from −ybreakout to +ybreakout, the linear friction force is given by Fy = −ks Ay , in
vertical
plane,
thehyperbolic
dynamic features
of the cyclic
pipe–seabed
simulated
by model,
a nonsoil model
with
secant stiffness
formulations
[29],interactions
as shown inwere
Figure
4. In this
s refers to the seabed shear stiffness and A represents the contact area. When the lateral
which
k
linear
hysteretic
soil model
with hyperbolic
secant
stiffness
[29],cyclic
as shown
in Figure
4.
four types
of pipe–soil
penetration
modes were
applied
to formulations
characterize the
variations
of the
displacement
y four
exceeds
theof
range
between
−ybreakout and
+ybreakout
, the
frictiontoforce
of the pipe
is cyclic
equal
In
this
model,
types
pipe–soil
penetration
modes
were
applied
characterize
the
pipeline periodic embedment into the seabed. For the not-in-contact pattern, the seabed resistance P(z)
to μP(z) , where
is the vertical seabed
resistance
andseabed.
μ is the For
soil the
friction
coefficient.pattern,
This model
variations
the P(z)
pipeline
embedment
into initial
the
not-in-contact
is naturallyofzero.
For otherperiodic
three patterns,
including
penetration,
uplift,
and repenetration, the
the
could
effectively
avoid
the
discontinuous
nature
of
the
friction
force
at
zero
lateral
displacement
and
seabed
resistance
P(z) is
naturally
zero. For other
three
including
initial penetration,
uplift,
relationships
between
the
seabed resistance
P(z) and
thepatterns,
penetration
z non-linearly
vary in hysteretic
was
conveniently
implemented
the
numerical
program
[30].
and
repenetration,
the relationships
between
themodes.
seabed resistance
P(z) and the penetration z noncycles
with the incessant
shift ofin
the
penetration
linearly vary in hysteretic cycles with the incessant shift of the penetration modes.
P(z)
Ultimate
In another view of the
horizontal plane,
thepenetration
lateral and axial pipe–seabed interactions were
resistance, Pu
simulated by the modified Coulomb
friction
model,
which expressed the lateral resistance and axial
(1) Initial
friction force with the deflectionpenetration
as a bilinear equation, as illustrated in Figure 5. When the lateral
displacement y varies from −ybreakout to +ybreakout, the linear friction force is given by Fy = −ks Ay , in
stiffness
and A represents the contact area. When the lateral
which ks refers to the seabed shear (5)
Repenetration
(2) Uplift
following
lift-off
displacement y exceeds the range between −ybreakout and +ybreakout, the friction force of the pipe is equal
to μP(z) , where P(z) is the vertical seabed resistance and μ is the soil friction coefficient. This model
O
z
(4) Suction releases
could effectively avoid the discontinuous
nature
(3) Suction
decays of the friction force at zero lateral displacement and
with repentration
was conveniently implemented in the numerical program [30].
P(z)
Ultimate penetration
Ultimate suction
Pu
resistance,resistance,
Pu-suc
(1) Initial
penetration
Figure
Figure 4.
4. Non-linear
Non-linear hysteretic
hysteretic seabed
seabed soil
soil model
model [29].
[29].
In another view of the horizontal
plane, the lateral and axial pipe–seabed interactions were
(5) Repenetration
(2) Uplift
simulated by the modified Coulombfollowing
frictionlift-off
model, which expressed the lateral resistance and axial
friction force with the deflection as a bilinear equation, as illustrated in Figure 5. When the lateral
z
(4) Suction releases
displacement y varies fromO−ybreakout
to +ydecays
breakout , the linear friction force is given by Fy = −ks Ay,
(3) Suction
with repentration
in which ks refers to the seabed shear stiffness and A represents the contact area. When the lateral
displacement y exceeds the range between
−ybreakout and +ybreakout , the friction force of the pipe is equal
Ultimate suction
to µP(z), where P(z) is the vertical seabed
resistance
and µ is the soil friction coefficient. This model
resistance,
Pu-suc
could effectively avoid the discontinuous nature of the friction force at zero lateral displacement and
Figure in
4. Non-linear
hysteretic
seabed
soil model [29].
was conveniently implemented
the numerical
program
[30].
J. Mar.
Mar. Sci.
Sci. Eng.
Eng. 2020,
2020, 8,
8, 119
119
J.
J. Mar. Sci. Eng. 2020, 8, 119
of 22
22
66 of
6 of 22
Fy
Fy
μP(z)
μP(z)
-ybreakout
-ybreakout
o
o
ybreakout
ybreakout
y
y
-μP(z)
-μP(z)
Figure 5. Modified Coulomb friction model.
Figure 5. Modified
Modified Coulomb friction model.
5
5
5
5
4
4
4
4
Pitch
( deg
Pitch
( deg
) )
Surge
Surge
( m()m)
2.4.
2.4. Pipelay
Pipelay Vessel
Vessel Motions
Motions
2.4. Pipelay Vessel Motions
According
According to
to the
the geometrical
geometrical features
features of
of the
the HYSY
HYSY 201
201 vessel,
vessel, aa pipelay
pipelay vessel
vessel model
model was
was built
built
According to the geometrical features of the HYSY 201 vessel, a pipelay vessel model was built
with
a length
length of
of 204.65
204.65 m
m and
and breadth
breadth of
of 39.2
39.2 m.
m. The
with a
The wave
wave frequency
frequency motion
motion of
of the
the vessel
vessel was
was
with a length of 204.65 m and breadth of 39.2 m. The wave frequency motion of the vessel was
simulated
simulated by
by use
use of
of the
the displacement
displacement response
response amplitude
amplitude operators
operators (RAOs),
(RAOs), which
which define
define the
the vessel
vessel
simulated by use of the displacement response amplitude operators (RAOs), which define the vessel
motion
motion responses
responses for
for each
each degree
degree of
of freedom
freedom (DoF)
(DoF) to
to one
one specified
specified wave
wave direction
direction and
and wave
waveperiod.
period.
motion responses for each degree of freedom (DoF) to one specified wave direction and wave period.
Considering
heave, roll,
pitch, and
Considering the
the six
six DoFs
DoFs of
of vessel
vessel motions
motions (surge,
(surge, sway,
sway, heave,
roll, pitch,
and yaw),
yaw), the
the motion
motion
Considering the six DoFs of vessel motions (surge, sway, heave, roll, pitch, and yaw), the motion
response
response spectra
spectra of
of the
the vessel
vessel at
at the
the stinger
stinger base
base were
were derived
derived in
in light
light of
of the
the RAOs
RAOs of
of the
the HYSY
HYSY 201
201
response spectra of the vessel at the stinger base were derived in light of the RAOs of the HYSY 201
vessel,
as
illustrated
in
Figure
6.
Almost
all
six
DoFs
of
the
vessel
motion
responses
were
vessel, as illustrated in Figure 6. Almost all six DoFs of the vessel motion responses were greatly
greatly
vessel, as illustrated in Figure 6. Almost all six DoFs of the vessel motion responses were greatly
noticeable
motion was
was comparatively
comparatively remarkable
noticeable for
for the
the quartering
quartering seas,
seas, in
in which
which the
the heave
heave motion
remarkable for
for all
all
noticeable for the quartering seas, in which the heave motion was comparatively remarkable for all
seas.
It
is
noted
that
the
slow
drift
motion
of
the
vessel
was
restrained
to
be
very
small
by
the
seas. It is noted that the slow drift motion of the vessel was restrained to be very small by the advanced
seas. It is noted that the slow drift motion of the vessel was restrained to be very small by the
advanced
dynamic positioning
[31],
sotaken
it was
notconsideration
taken into consideration
in the
following
dynamic positioning
system [31],system
so it was
not
into
in the following
analyses
due
advanced dynamic positioning system [31], so it was not taken into consideration in the following
analyses
due
to
its
small
effect
on
the
pipeline
dynamic
behaviors.
to its small effect on the pipeline dynamic behaviors.
analyses due to its small effect on the pipeline dynamic behaviors.
3
3
Quartering
Quartering
2
2
1
1
5
5
Head/stern
Head/stern
2
3
4
Wave
2 height(m)
3
4
Wave height(m)
Head/stern
Head/stern
1
1
5
5
2
3
2 height(m)
3
Wave
Wave height(m)
4
4
5
5
4
4
Roll
( deg
Roll
( deg
) )
Sway
Sway
( m()m)
2
2
0
00
0
5
5
4
4
3
3
Quartering
Quartering
2
2
1
1
0
00
0
Quartering
Quartering
1
1
1
1
0
00
0
3
3
2
3
Wave
2 height(m)
3
Wave height(m)
4
4
2
2
1
1
Beam
Beam
1
1
Beam
Beam
3
3
5
5
0
00
0
Figure 6. Cont.
1
1
Quartering
Quartering
2
3
4
2 height(m)
3
4
Wave
Wave height(m)
5
5
J. Mar. Sci. Eng. 2020, 8, 119
J. Mar. Sci. Eng. 2020, 8, 119
7 of 22
7 of 22
5
10
4
8
Yaw( deg)
Heave( m)
Quartering
6
Beam
4
2
0
3
2
1
Head/stern
0
0
1
2
3
Wave height(m)
Quartering
4
5
0
1
2
3
Wave height(m)
4
5
Figure 6.
6. Motion
Motion response
response spectra
spectra of
of the
the HYSY
HYSY 201
201 pipelay
pipelay vessel
vessel at
at the
the stinger
stinger base.
Figure
base.
3. Freak Wave Generation
3. Freak Wave Generation
Based on a large amount of ocean observations and laboratory tests, a great many generation
Based on a large amount of ocean observations and laboratory tests, a great many generation
models of freak waves have been developed to investigate the phenomenon of rogue wave impact [32,33].
models of freak waves have been developed to investigate the phenomenon of rogue wave impact
In contrast with the non-linear model, the linear superposition model is simply understood by offshore
[32,33]. In contrast with the non-linear model, the linear superposition model is simply understood
structure engineers and can be rapidly simulated by researchers. It is also noted that during deepwater
by offshore structure engineers and can be rapidly simulated by researchers. It is also noted that
installation, the pipeline usually experiences large tension forces of the tensioners, and the influence
during deepwater installation, the pipeline usually experiences large tension forces of the tensioners,
of hydrodynamic forces induced by non-linear wave factors is very small. A time history train of
and the influence of hydrodynamic forces induced by non-linear wave factors is very small. A time
freak waves must be inserted into the developed installation FEM for the dynamic analysis of an S-lay
history train of freak waves must be inserted into the developed installation FEM for the dynamic
pipeline. Therefore, the linear superposition technique was employed to generate the freak wave trains.
analysis of an S-lay pipeline. Therefore, the linear superposition technique was employed to generate
the
trains. Approach
3.1. freak
Linearwave
Superposition
In theSuperposition
linear superposition
3.1. Linear
Approach method, freak waves are described as a combination of transient
wave trains with random wave trains for different energy proportions. The transient waves were
In the linear superposition method, freak waves are described as a combination of transient
simulated by the wave focusing model which converges the wave energy of a certain number of wave
wave trains with random wave trains for different energy proportions. The transient waves were
components at a specified position at the assigned time. The random waves were deemed to be a
simulated by the wave focusing model which converges the wave energy of a certain number of wave
stationary stochastic process of dispersed energy. The standard JONSWAP spectrum was employed to
components at a specified position at the assigned time. The random waves were deemed to be a
represent the random sea states in the South China Sea. The generation formula of freak waves can be
stationary stochastic process of dispersed energy. The standard JONSWAP spectrum was employed
expressed as
to represent the random sea states
in the South China Sea. The generation formula
of freak waves can
 12
 21
N Z
N Z fi
X



be expressed asX  fi

η(x, t) = Ep1
2S( f )d f  cos[ki (x − xp ) − ωi (t − tp )] + Ep2
2S( f )d f  cos[ki x − ωi t + φi ]
(6)


i=1
fi−1
N
1
2
i=
N 1
fi−1
1
2
η ( x, t ) = Ep1    2S ( f )df  cos[k i ( x − xp ) − ωi (t − t p )] + Ep 2    2S ( f )df  cos[k i x − ωi t + ϕ i ]
fi
fi
(6)
 f

 f

1 
i =1 
where Ep1 and Ep2 are
the energy ratio coefficients of transienti=waves
and random
waves; the spectral
h
i
densityEfunction
S(the
f) =
αg2 /(ratio
16π4coefficients
f 5 ) exp −1.25
(transient
f / fm )−4 waves
γβ ; α isand
the random
spectralwaves;
energythe
coefficient;
p1 and Ep2is
are
energy
of
spectral
where
h
i
2 −4 2β 2
2
4 5
S
(
f
)
=
α
g
/(
16
π
f
)
exp
−
1
.
25
(
f
/
f
)
γ
;
α
is
the
spectral
energy
coefficient;
density
function
is
(
)
and g is the gravitational constant. β = exp − f − fm m/ 2τ fm , in which τ is the spectral width
2
parameter;
is the peak constant.
frequency;βγ=isexp
the− peak
N is
thethe
number
of width
wave
( f − fenhancement
2τ 2 f m2 , factor;
and g is thef m
gravitational
in which
τ is
spectral
m)
components; ki , ωi , and φi are the wave number, angular frequency, and phase lag of the ith wave
parameter; fm is the peak frequency; γ is the peak enhancement factor; N is the number of wave
component; and xp and tp are two constants separately representing the focusing position and time of
components; ki , ωi , and ϕi are the wave number, angular frequency, and phase lag of the ith wave
transient waves.
component; and xp and tp are two constants separately representing the focusing position and time
of
waves.
3.2.transient
Case Study
i −1
i −1
[
[
(
]
)]
Before the generation of freak waves, there should be a clear mathematical definition. The popularly
3.2. Case Study
acceptable criterion for freak waves was adopted in this study, which defines the maximum wave
Before
generation
freak
waves, there
should
be Based
a clearupon
mathematical
height
to be the
more
than two of
times
its significant
wave
height.
the ocean definition.
statistics inThe
the
popularly
acceptable
criterion
for
freak
waves
was
adopted
in
this
study,
which
defines
the
South China Sea, the significant wave height, Hs = 2.0 m, and the peak period, Tp = 8.7 s, were
maximum
wave
height to bespectrum,
more thanastwo
times itsinsignificant
height. Based peak
uponfrequency,
the ocean
specified for
the JONSWAP
illustrated
Figure 7. wave
The corresponding
statistics
in
the
South
China
Sea,
the
significant
wave
height,
H
s
=
2.0
m,
and
the
peak
period,
Tp peak
= 8.7
fm = 0.115 Hz, and the spectral energy coefficient, α = 0.002, were calculated along with the
s, were specified for the JONSWAP spectrum, as illustrated in Figure 7. The corresponding peak
frequency, fm = 0.115 Hz, and the spectral energy coefficient, α = 0.002, were calculated along with the
2
S( f ) (m /Hz)
trains were set as Ep1 = 0.4 and Ep2 = 0.6, and the distribution range φ of the phase lag was taken as
1.1π. The wave focusing time and position were set at tp = 1000 s and xp = 0 m. Figure 8 illustrates a
part of the time history trains of generated freak waves, and the beginning simulation time point was
shifted to 750 s with the duration of 500 s so as to cover the maximum wave height in the globe time
J. Mar.
Mar. Sci.
Sci. Eng.
Eng.
2020,
119
of 22
22
It
can
be8,8,observed
that the freak wave amplitude suddenly surged to a great wave crest
of
J.domain.
2020,
119
88 of
5.1 m at the focusing time of 1000 s. The maximum wave height attained 7.8 m, which is 3.9 times
peak
factor, γ wave
= 3.3. Besides,
the spectral
width
parameter
was varied
with the
largerenhancement
than its significant
height. The
wave time
history
trainsσ properly
reflect
the value
basic
enhancement factor, γ = 3.3. Besides, the spectral width parameter σ was varied with the value of
of
wave
frequency.
If
f
≤
f
m
,
τ
=
0.07;
otherwise,
f
>
f
m
,
τ
=
0.09.
characteristic of freak waves in the ocean sea and satisfy the wave amplitude criterion for its
wave frequency. If f ≤ fm , τ = 0.07; otherwise, f > fm , τ = 0.09.
The selected wave spectrum was discretized into 900 components by use of the equal energy
definition.
approach. These wave components were then gathered in the numerical flume to constitute a
8
sequence of transient wave trains and random wave trains. The energy proportions for both wave
Hs=2.0 m
trains were set as Ep1 = 0.4 and Ep2 = 0.6, and the distribution
range φ of the phase lag was taken as
T = 8.7 s
6
1.1π. The wave focusing time and
position were set at tp =p 1000 s and xp = 0 m. Figure 8 illustrates a
part of the time history trains of generated freak waves, and the beginning simulation time point was
4 of 500 s so as to cover the maximum wave height in the globe time
shifted to 750 s with the duration
domain. It can be observed that the freak wave amplitude suddenly surged to a great wave crest of
5.1 m at the focusing time of 1000
2 s. The maximum wave height attained 7.8 m, which is 3.9 times
larger than its significant wave height. The wave time history trains properly reflect the basic
characteristic of freak waves in the ocean sea and satisfy the wave amplitude criterion for its
0
definition.
0.0
0.1
0.2
0.3
0.4
f (Hz)
8
Figure 7. JONSWAP spectrumHfor
Hs = 2.0 m.
s=2.0Hm
Figure 7. JONSWAP spectrum for
s = 2.0 m.
T = 8.7 s
η (m)
2
S( f ) (m /Hz)
6
p components by use of the equal energy
The selected wave spectrum
was discretized into 900
6
approach. These wave components
were then gathered in the numerical flume to constitute a sequence
4
of transient wave trains and random wave trains. The energy proportions for both wave trains were set
as Ep1 = 0.4 and Ep2 = 0.6, and the distribution range ϕ of the phase lag was taken as 1.1π. The wave
3 2 set at tp = 1000 s and xp = 0 m. Figure 8 illustrates a part of the time
focusing time and position were
history trains of generated freak waves, and the beginning simulation time point was shifted to 750 s
with the duration of 500 s so as to cover the maximum wave height in the globe time domain. It can be
0
0.0
0.1
0.2
0.4 crest of 5.1 m at the focusing
observed that the freak wave 0amplitude
suddenly
surged
to a0.3great wave
f (Hz)
time of 1000 s. The maximum wave height attained
7.8 m, which is 3.9 times larger than its significant
wave height. The wave time history trains properly reflect the basic characteristic of freak waves in the
Figure 7. JONSWAP spectrum for Hs = 2.0 m.
-3 amplitude criterion for its definition.
ocean sea and satisfy the wave
750 800
900
1000
t (s)
1100
1200 1250
6
Figure 8. Time history trains of the freak wave.
3
η (m)
3.3. Sensitive Analysis
The time history trains of freak waves are crucial for the investigation into their effects on the
dynamic behaviors of S-laying pipelines. The sensitive analyses of generation factors for the freak
0
wave train must be conducted. Four input parameters, including the wave energy ratio coefficient,
focusing position, phase range, and peak value, were selected for the wave simulation by the linear
superposition technique. Plenty of freak wave trains were obtained, and a group of represented trains
-3
800
900in Figure
1000 9. 1100
1200 differences
1250
750illustrated
with the duration of 500 s are
Significant
in the wave crest and
t (s)
wave trough at the middle time were observed under different initial conditions.
Figure 8. Time history trains of the freak wave.
Figure 8. Time history trains of the freak wave.
3.3. Sensitive Analysis
3.3. Sensitive Analysis
The time history trains of freak waves are crucial for the investigation into their effects on the
The
historyoftrains
of freak
wavesThe
are sensitive
crucial for
the investigation
intofactors
their effects
the
dynamic time
behaviors
S-laying
pipelines.
analyses
of generation
for theonfreak
dynamic
behaviors
of
S-laying
pipelines.
The
sensitive
analyses
of
generation
factors
for
the
freak
wave train must be conducted. Four input parameters, including the wave energy ratio coefficient,
wave
train
must bephase
conducted.
inputvalue,
parameters,
including
ratiobycoefficient,
focusing
position,
range, Four
and peak
were selected
for the
the wave
wave energy
simulation
the linear
focusing
position,
phase
range,
and
peak
value,
were
selected
for
the
wave
simulation
by the linear
superposition technique. Plenty of freak wave trains were obtained, and a group of represented
trains
superposition
technique.
of freak in
wave
trains
were obtained,
and a group
represented
with the duration
of 500 sPlenty
are illustrated
Figure
9. Significant
differences
in the of
wave
crest andtrains
wave
with
the
duration
of
500
s
are
illustrated
in
Figure
9.
Significant
differences
in
the
wave
crest
and
trough at the middle time were observed under different initial conditions.
wave trough at the middle time were observed under different initial conditions.
J.J.Mar.
Mar.Sci.
Sci.Eng.
Eng.2020,
2020,8,
8,119
119
J. Mar. Sci. Eng. 2020, 8, 119
9 9ofof2222
9 of 22
-6
6
0
Ep1=0.35
Ep1=0.35
η (m)
η (m)
6 -6
6
0
0
-6
6 -6
6
0
0
-6
-6
6
6
0
0
-6
-6
0
Ep1=0.40
Ep1=0.40
ηη
(m)
(m)
0
6
60
0
-6
-66
60
Ep1=0.30
Ep1=0.30
6
Ep1=0.45
Ep1=0.45
0
100
100
200
300
200 t (s) 300
t (s)
400
400
500
500
0
-6
-66
6
0
0
-6
-66
6
0
0
-6
-66
6
0
0
-6
-6 0
0
xp=-200 m
xp=-200 m
xp=-100 m
xp=-100 m
xp=0 m
m
xp=0
xp=100 m
m
xp=100
xp=200 m
xp=200
m
100
100
(a)
(a)
ϕϕ=1.0
=1.0ππ
ϕϕ=1.2
=1.2ππ
ηη (m)
(m)
ϕϕ=1.1
=1.1ππ
ϕϕ=1.3
=1.3ππ
=1.4ππ
ϕϕ=1.4
100
100
400
400
500
500
(b)
(b)
η (m)
η (m)
66
00
-6 -6
66
00
-6 -6
66
00
-6 -6
66
00
-6 -6
66
00
-6 -6
00
200
300
200 t (s) 300
t (s)
200
300
200
(s) 300
t t(s)
400
400
500
500
66
00
-6
-6
66
00
-6
-6
66
0
-6
6
0
-6
6
0
-6
=3.6mm
ηη
=3.6
p
p
=4.1mm
ηη
=4.1
pp
=4.6mm
ηη
=4.6
pp
=5.1mm
ηη
=5.1
pp
ηη
=5.6
=5.6mm
pp
0
100
100
(c)
(c)
200
200 t t(s)
300
(s) 300
400
400
500
500
(d)
(d)
Figure
9.Time
Time
history
trains
of freak
freak
waves
under
different
input
(a)
energy
ratio
Figure
9.9.Time
history
trains
of freak
waveswaves
underunder
different
input conditions:
(a) energy
coefficient;
Figure
history
trains
of
different
input conditions:
conditions:
(a)ratio
energy
ratio
coefficient;
(b)
focusing
position;
(c)
phase
range;
(d)
wave
peak
value.
(b)
focusing (b)
position;
(c) position;
phase range;
(d) wave
peak
coefficient;
focusing
(c) phase
range;
(d) value.
wave peak value.
Figure
displays
the
maximum
wave
heights
of freak
wave
trains
with
ofofinitial
the
Figure
101010
displays
the
maximum
wave
heights
of freak
wave
trains
with
the the
variation
of the
Figure
displays
the
maximum
wave
heights
of
freak
wave
trains
with
thevariation
variation
the
initial
input
parameters.
It
can
be
seen
that
the
maximum
wave
height
linearly
increases
with
the
input
parameters.
It
can
be
seen
that
the
maximum
wave
height
linearly
increases
with
the
increase
initial input parameters. It can be seen that the maximum wave height linearly increases with theof
increase
theenergy
energyratio
ratio
coefficientEEp1p1,, which
which
denotes
energy
of
transient
wave
the
energyofof
ratio
coefficient
Ecoefficient
thedenotes
energy the
proportion
of the transient
in the
freak
increase
the
the
energyproportion
proportion
ofthe
thewave
transient
wave
p1 , which denotes
in
the
freak
wave
trains.
When
the
focusing
location
occurred
from
the
distance
x
p = −200 m to xp =
wave
Whentrains.
the focusing
location
occurred
from
the distance
xp distance
= −200 mxpto= x−200
in thetrains.
freak wave
When the
focusing
location
occurred
from the
m tom,xpthe
=
p = 200
200 m, the maximum
wave
height
firstly augmented
and then
reduced,
and
the attained
crest value
attained
maximum
heightwave
firstlyheight
augmented
then reduced,
and
the crest
value
7.86
m at the
200 m, thewave
maximum
firstly and
augmented
and then
reduced,
and
the crest value
attained
7.86 m at the point xp = 0 m. As the phase range added from 1.0π to 1.4π, the maximum wave height
point
xpat=the
0 m.
As xthe
added
fromadded
1.0π to
1.4π,
thetomaximum
wave height
gradually
7.86 m
point
p = phase
0 m. Asrange
the phase
range
from
1.0π
1.4π, the maximum
wave
height
gradually decreased. Oppositely, along with the augmentation of the wave peak value from 3.6 to 5.6
decreased.
Oppositely,
along with
the augmentation
of the wave
peak
value
to 5.6
the
gradually decreased.
Oppositely,
along
with the augmentation
of the
wave
peakfrom
value3.6
from
3.6 m,
to 5.6
m, the maximum wave height linearly magnified.
maximum
wave height
magnified.
m, the maximum
wave linearly
height linearly
magnified.
Hmax (m)
Hmax (m)
10
(b)
10
8 (b)
86
64
4 -200
-200
-100
-100
Ep1
Ep1
0
x0p(m)
xp(m)
0.40
0.40
0.45
0.45
100
100
200
200
Hmax
(m)
Hmax
(m)
0.35
0.35
10 (c)
10 (c)
8
8
6
6
4
41.0
1.0
10
(d)
10
(d)
8
8
6
6
4
43.6
3.6
Hmax
Hmax
(m)(m)
Hmax (m)
Hmax (m)
10
(a)
10
(a)
8
8
6
6
4
4 0.30
0.30
1.1
1.1
4.0
4.0
1.2
1.2
ϕ (π)
ϕ (π)
4.4
4.8
4.4η (m) 4.8
η (m)
1.3
1.3
5.2
5.2
1.4
1.4
5.6
5.6
Figure 10. Variation of the maximum freak wave height with different input conditions: (a) energy
Figure
the
wave
height
with
different
input conditions:
conditions:(a)
(a)energy
energy
Figure
10. Variation
Variation
of
the maximum
maximum
freak
input
ratio 10.
coefficient;
(b)of
focusing
position;freak
(c) phase
range;
(d)with
wavedifferent
peak value.
ratio
value.
ratiocoefficient;
coefficient;(b)
(b)focusing
focusingposition;
position; (c)
(c) phase
phase range;
range; (d) wave peak value.
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4. Numerical
Numerical Implementation
Implementation of
of Pipeline
Pipeline Installation
Installation under
under Freak
Freak Waves
Waves
4.
4. Numerical Implementation of Pipeline Installation under Freak Waves
4.1.
4.1. Pipelay
Pipelay Parameters
Parameters
4.1. Pipelay Parameters
According
According to
to aa practical
practical engineering
engineering case,
case, aa 12
12 inch
inch pipeline
pipeline was
was installed
installed into
into aa water
water depth
depth of
of
1500
m
in
the
Liwan3-1
(LW3-1)
gas
field
in
the
South
China
Sea.
The
laying
pipeline
parameters
listed
According
to
a
practical
engineering
case,
a
12
inch
pipeline
was
installed
into
a
water
depth
of
1500 m in the Liwan3-1 (LW3-1) gas field in the South China Sea. The laying pipeline parameters
in
Table
1Table
were
adopted,
which
included
thein
outer
diameter
D,
wall
t’thickness
steel pipe
ρp ,
1500
minin
the Liwan3-1
(LW3-1)
gas field
the the
South
China
Sea.thickness
The
laying
p , pipeline
listed
1 were adopted,
which
included
outer
diameter
D, wall
t’pparameters
,density
steel pipe
elastic
modulus
Poisson’s
ratio
v, effective
yield
stress
σyyield
, thickness
density
oft’the
corrosion
listed
in
1E,were
adopted,
which
included
the
outer
diameter
thickness
p, steel
pipe
density
ρTable
p, elastic
modulus
E, Poisson’s
ratio
v, effective
stresstD,
σc yand
, wall
thickness
tρc cand
density
ρc of
coatings,
weight
per
unit
length
in
air
w
,
and
submerged
weight
per
unit
length
w
.
density
ρ
p
,
elastic
modulus
E,
Poisson’s
ratio
v,
effective
yield
stress
σ
y
,
thickness
t
c
and
density
ρ
a
the corrosion coatings, weight per unit length
in air wa, and submerged weight pers unit length wsc. of
the corrosion coatings, weight per unit length in air wa, and submerged weight per unit length ws.
Table
Table1.1. Laying
Laying pipeline
pipelineparameters.
parameters.
Table
1.
Laying
pipeline
parameters.
3
D
(MPa)
ttcc (mm)
(mm) ρρcc (kg/m
(kg/m33)) w
D(mm)
(mm) t’t’p p(mm)
(mm) ρpρp(kg/m
(kg/m)3) EE(MPa)
(MPa) vv σσyy (MPa)
waa (N/m)
(N/m) w
wss (N/m)
(N/m)
3
3
5
5
D323.9
(mm) t’p23.8
(mm)
ρp 7850
(kg/m
E
(MPa)
σy (MPa)
tc (mm)
ρc (kg/m
(N/m) ws917.2
(N/m)
v
323.9
23.8
7850 ) 2.07
2.07
0.3
448
3.0
950 ) wa1754.9
1754.9
917.2
448
3.0
950
××
1010 0.3
323.9
23.8
7850
2.07 × 105 0.3
448
3.0
950
1754.9
917.2
X65material
materialgrade
grade
was
used
forsteel
the pipe,
steel whose
pipe, stress–strain
whose stress–strain
relationship
curve is
X65
was
used
for the
relationship
curve is displayed
X65
material
grade
was
used
for
the
steel
pipe,
whose
stress–strain
relationship
curve
is
displayed in Figure 11 on the basis of the Ramberg–Osgood model. The non-linear relationship
in Figure 11 on the basis of the Ramberg–Osgood model. The non-linear relationship between the
displayed
in bending
Figure 11moment
on the and
basiscurvature
of the Ramberg–Osgood
model.inThe
non-linear
between the
of the steel pipe shown
Figure
12 was relationship
obtained by
bending moment and curvature of the steel pipe shown in Figure 12 was obtained by use of the
between
the
bending
moment
and
curvature
of
the
steel
pipe
shown
in
Figure
12
was
obtained
by
use of the hysteretic bending model, which gave a precise simulation of the bending state of the
hysteretic bending model, which gave a precise simulation of the bending state of the overbend pipeline
use
of the pipeline
hysteretic
bending
model,
whichcontacts
gave a precise
simulation
overbend
under
the cyclic
clashing
with stinger
rollers.of the bending state of the
under the cyclic clashing contacts with stinger rollers.
overbend pipeline under the cyclic clashing contacts with stinger rollers.
500
500
400
σ (MPa
) )
σ (MPa
400
σy=448 MPa
σB=0.0028
=448 MPa
y
300
300
200
n=11.3
B=0.0028
200
n=11.3
100
100
0
0.0
0
0.0
0.2
0.4
0.6
0.4 ε (%) 0.6
ε (%)
0.2
0.8
0.8
1.0
1.0
Figure 11. Stress–strain curve for the Ramberg–Osgood model.
Figure 11. Stress–strain curve for the Ramberg–Osgood model.
Figure 11. Stress–strain curve for the Ramberg–Osgood model.
M
M
O
O
κ
κ
Figure
Figure 12.
12. Non-linear
Non-linear hysteretic
hysteretic moment–curvature
moment–curvature relationship.
relationship.
Figure 12. Non-linear hysteretic moment–curvature relationship.
The
vertical distribution
distributionofofthe
the
current
speed
among
various
water
depths
is illustrated
in
The vertical
current
speed
among
various
water
depths
is illustrated
in Figure
◦
Figure
13vertical
inoflight
of themeasurement.
fieldofmeasurement.
The
current
direction
0 with
in line
with
the
the current
among
various
depths
isline
illustrated
Figure
13 inThe
light
thedistribution
field
Thespeed
current
direction
waswater
set was
as
0°set
inas
thein
pipelay
pipelay
heading.
The
ocean
current
was
considered
as
a
two-dimensional
steady
flow
in
the
vertical
13
in lightThe
of the
field
measurement.
The current
direction was set
as 0°flow
in line
with
the pipelay
heading.
ocean
current
was considered
as a two-dimensional
steady
in the
vertical
plane.
plane.
TheThe
hydrodynamic
calculated
bytwo-dimensional
means
Morison’s
equation
[34]
and
are given
given
by
heading.
ocean current
waswere
considered
as ameans
steady
flow[34]
in
the
vertical
plane.
The hydrodynamic
loadsloads
were
calculated
by
of of
Morison’s
equation
and
are
by
(∆ · aw + Ca · ∆loads
Fd =hydrodynamic
· ar ) +were
0.5 · Ccalculated
· ρw · A · vby
∆ is the mass
of fluid[34]
displaced
bygiven
the pipe,
|, in which
r |vrmeans
D
The
of
Morison’s
equation
and
are
by
Fd = (Δ ⋅ a w + C a ⋅ Δ ⋅ a r ) + 0.5 ⋅ C D ⋅ ρ w ⋅ A ⋅ vr vr , in which Δ is the mass of fluid displaced by the
F
⋅ a + C ⋅ Δ ⋅ a r ) + 0.5 ⋅ C D ⋅ ρrelative
vr the
, in which Δ is the mass of fluid displaced by the
d = (Δ
w ⋅ A ⋅ v r to
αw isw the afluid acceleration
earth, Ca is the added mass factor, αr is the fluid
pipe,
pipe, αw is the fluid acceleration relative to the earth, Ca is the added mass factor, αr is the fluid
J. Mar. Sci. Eng. 2020, 8, 119
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αw is the fluid acceleration relative to the earth, Ca is the added mass factor, αr is the fluid acceleration
acceleration
relative
the pipe, CD is the drag coefficient, ρw is the density of sea water, A is the drag
relative to the
pipe, Cto
D is the drag coefficient, ρw is the density of sea water, A is the drag area, and νr
area,
and
ν
r is the fluid velocity relative to the pipe. For the hydrodynamic calculation, Ca was taken
is the fluid velocity relative to the pipe. For the hydrodynamic calculation, Ca was taken as 1.0, and the
as
andaxial
the and
CD the
for normal
the axial
and thewas
normal
directions
wasand
assumed
to be 0.024 and 1.2,
CD 1.0,
for the
directions
assumed
to be 0.024
1.2, respectively.
respectively.
0
d (m)
-300
-600
-900
-1200
-1500
0.0
0.2
0.4
0.6
vc (m/s)
0.8
1.0
Figure 13. Current speed distribution with various water depths.
Figure 13. Current speed distribution with various water depths.
With regard to the non-linear hysteretic soil model applied in this study, a group of seabed soil
With regard to the non-linear hysteretic soil model applied in this study, a group of seabed soil
parameters was selected to describe the basic features of soft clay in the deep water, as listed in
parameters was selected to describe the basic features of soft clay in the deep water, as listed in Table
Table 2. The ultimate penetration resistance Pu (z) and the nominal bearing capacity factor Nc (z/D) are
2. The ultimate penetration resistance Pu(z) and the nominal bearing capacity factor N c ( z D) are
non-linearly related to the penetration z and are given by [29]
non-linearly related to the penetration z and are given by [29]
PuP(z()z)== N
·D
Nc ((z/D
z D))⋅·SSu( (zz) )⋅ D
(7)
(7)
b
NN
c (cz/D
( z D))=
= aa ⋅·((zz/D
D) b)
(8)
(8)
u
c
u
where the
in which
which S
isthe
themudline
mudline shear
shear
ugzz,, in
) =SSu0u 0 +
+ SSug
Su0
u0 is
where
the soil
soil undrained
undrainedshear
shearstrength
strengthrefers
referstotoSuS(zu )( z=
strength and Sug is the shear strength gradient, and a and b are the non-dimensional penetration factors.
strength and Sug is the shear strength gradient, and a and b are the non-dimensional penetration
The saturated soil density ρsoil and normalized maximum stiffness Kmax were taken for the soft clay;
factors. The saturated soil density
ρsoil and normalized maximum stiffness Kmax were taken for the soft
other soil model parameters for different penetration patterns were specified as the defaults, including
clay; other soil model parameters for different penetration patterns were specified as the defaults,
the suction ratio f suc and the decay factor λsuc , repenetration coefficient λrep and soil buoyancy factor f b .
including the suction
ratio fsuc and the decay factor λsuc, repenetration coefficient λrep and soil
In addition, the seabed soil friction coefficient µ and shear stiffness ks were adopted for the simulation
buoyancy factor fb. In addition, the seabed soil friction coefficient
μ and shear stiffness ks were
of axial and lateral pipe–seabed interactions [35].
adopted for the simulation of axial and lateral pipe–seabed interactions [35].
Table 2. Seabed soil model parameters.
Table 2. Seabed soil model parameters.
Su0 (kPa)
Su0 (kPa)
1.51.5
Sug (kPa/m)
Sug (kPa/m)
1.51.5
ρsoil (t/m3 ) 3
a
b
K
f
ρsoil (t/m )
Kmax suc
fsuc
a
b max
1.51.5
6.06.0 0.25
200
0.25 200 0.6
0.6
λsuc
λsuc
1.0
1.0
λ
λrep
rep
0.3
0.3
f
µ
k (kN/m3 )
s
3)
fb b
ks (kN/m
μ
1.5
0.55
33.3
1.5 0.55
33.3
Calcultion Method
Method
4.2. Calcultion
calculation of
of laying pipeline
pipeline responses
responses induced
induced by freak waves contained two
The dynamic calculation
modules: one
one was
was the
the S-lay
S-lay model
model and
and another
another was
was the
the freak
freak wave
wave train.
train. Firstly,
Firstly, a global
global S-lay model
atat
a water
depth
of 1500
m. m.
This
model
comprised
the
with the
the framework
frameworkof
ofOrcaFlex
OrcaFlexwas
wasestablished
established
a water
depth
of 1500
This
model
comprised
pipelay
vessel,
tensioner,
stinger,
pipeline,
and seabed.
UnderUnder
the combined
actionsactions
of self-weight,
the
pipelay
vessel,
tensioner,
stinger,
pipeline,
and seabed.
the combined
of selfbuoyancy,
and internal
the equilibrium
positions of the
laying pipeline
from the
tensioner
on the
weight,
buoyancy,
andforces,
internal
forces, the equilibrium
positions
of the laying
pipeline
from
vessel via on
thethe
stinger
to the
weretoinitially
determined
by utilization
of theby
catenary
technique.
tensioner
vessel
via seabed
the stinger
the seabed
were initially
determined
utilization
of the
Subsequently,
the
hysteretic
bending
stiffness
and
the
clashing
mutual
contacts
of
pipe-stinger
rollers
catenary technique. Subsequently, the hysteretic bending stiffness and the clashing mutual contacts
were
further taken
intowere
account
to obtain
equilibrium
configurations
of the pipeline.
The final
of
pipe-stinger
rollers
further
taken the
intofull
account
to obtain
the full equilibrium
configurations
of
static
results The
of the
S-lay
system
were
taken
as the
initial
values
of as
thethe
dynamic
simulation.
the
pipeline.
final
static
results
of the
S-lay
system
were
taken
initial values
of the dynamic
simulation.
Based upon the linear superposition technique, a series of time history trains of freak waves
were obtained from the MATLAB program. These freak wave trains were then inserted into the
J. Mar. Sci. Eng. 2020, 8, 119
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J. Mar.Based
Sci. Eng.upon
2020, 8,the
119linear
12 of 22
superposition technique, a series of time history trains of freak waves
were obtained from the MATLAB program. These freak wave trains were then inserted into the
developed
sea states.
developed S-lay
S-lay model
model as
as the
the input
input conditions
conditions of
of extreme
extreme sea
states. The
The geometric
geometric non-linearities
non-linearities of
of
the
the laying
laying pipeline,
pipeline, spatial
spatial variations
variations of
of hydrodynamic
hydrodynamic forces,
forces, and
and clashing
clashing contacts
contacts were
were sufficiently
sufficiently
incorporated
incorporated in
in the
the simulation.
simulation. The
The time
time domain
domain calculations
calculations of
of the
the S-lay
S-lay system
system under
under freak
freak waves
waves
were
conducted
by
use
of
the
explicit
dynamic
integration
approach.
Besides,
critical
damping
were conducted by use of the explicit dynamic integration approach. Besides, critical damping and
and
target
target damping
damping were
were utilized
utilized to
to cut
cut down
down the
the spurious
spurious non-physical
non-physical high
high frequency
frequency responses,
responses, and
and
they
were
demonstrated
to
have
little
effect
on
the
pipeline
behaviors.
Finally,
the
whole
motion
they were demonstrated to have little effect on the pipeline behaviors. Finally, the whole motion
equations
equations for
for the
the vessel
vessel and
and all
all line
line nodes
nodes were
were solved
solved by
by iterative
iterative update
update of
of the
the forces
forces and
and moments
moments
on
time step.
step.
on the
the nodes
nodes and
and segments
segments at
at each
each time
4.3. Time
Time History Response of Pipelay Vessel Motions
The pipelay vessel motions are significant top excitation boundaries of the S-laying pipeline and
cause dynamic responses. Under
Under the
the generated
generated freak
freak wave
wave trains
trains shown
shown in
in Figure
Figure 8 for the extreme
quartering
quartering sea,
sea, the time history responses
responses of six DoFs of pipelay vessel motions were calculated
calculated by
use of displacement RAOs, as displayed in Figure 14. The heave motion among vessel translation
responses
responses was
was more prominent than the surge and the sway motion, and the pitch motion among
vessel rotation responses was larger than the roll and
and the
the yaw
yaw motion.
motion. These results validate the
above-mentioned response spectra of the pipelay vessel. Moreover,
Moreover, all six DoFs of the vessel motion
response amplitudes
amplitudesabruptly
abruptlyrose
rose
and
attained
maximum
values
the middle
time
250 s,
and
attained
maximum
values
nearnear
the middle
time of
250of
s, which
which
also reflects
thetime
basic
time history
characteristic
freak waves.
also reflects
the basic
history
characteristic
of freakofwaves.
2
3.4
Surge
Sway
Heave
1
θ (° )
Sxyz(m)
1.7
0.0
0
-1
-1.7
-3.4
Pitch
Roll
Yaw
-2
0
100
200
t (s)
300
400
500
0
100
200
t (s)
300
400
500
Figure 14.
14. Time
Time history
history responses
responses of pipelay vessel motions under freak waves.
Figure
5. Results Analysis
5. Results Analysis
5.1. Effect of the Wave Energy Ratio Coefficient
5.1. Effect of the Wave Energy Ratio Coefficient
In the simulation of freak wave trains, the energy ratio coefficient directly dominates the energy
In the simulation of freak wave trains, the energy ratio coefficient directly dominates the energy
proportion of transient waves and random waves. By selecting four energy ratio coefficients, Ep1 = 0.30,
proportion of transient waves and random waves. By selecting four energy ratio coefficients, Ep1 =
0.35, 0.40 and 0.45, a group of freak wave trains in Figure 9a was utilized as the input marine
0.30, 0.35, 0.40 and 0.45, a group of freak wave trains in Figure 9a was utilized as the input marine
environment conditions for the dynamic analyses of the S-laying pipeline. The pipeline and seabed
environment conditions for the dynamic analyses of the S-laying pipeline. The pipeline and seabed
response results, which includes the axial tension, bending moment, von Mises stress, longitudinal
response results, which includes the axial tension, bending moment, von Mises stress, longitudinal
strain, pipeline embedment, and seabed resistance, are illustrated in Figure 15.
strain, pipeline embedment, and seabed resistance, are illustrated in Figure 15.
As the energy ratio coefficient Ep1 increased from 0.30 to 0.45, the axial tension of the overall
As the energy ratio coefficient Ep1 increased from 0.30 to 0.45, the axial tension of the overall
pipeline noticeably rose, and its maximum value at the top end increased by 39.9% from 3512.57 to
pipeline noticeably rose, and its maximum value at the top end increased by 39.9% from 3512.57 to
4915.02 kN. The bending moments of the pipeline had some differences between the overbend and the
4915.02 kN. The bending moments of the pipeline had some differences between the overbend and
sagbend, and the maximum results appeared at the last contact roller location in the overbend with a
the sagbend, and the maximum results appeared at the last contact roller location in the overbend
minor increase of 12.1% from 585.86 to 656.95 kN·m. In the sagbend, the maximum bending moment
with a minor increase of 12.1% from 585.86 to 656.95 kN·m. In the sagbend, the maximum bending
occurring near the touchdown point (TDP) had a prominent augmentation of 202.3% from 151.97 to
moment occurring near the touchdown point (TDP) had a prominent augmentation of 202.3% from
151.97 to 459.33 kN·m, and some bending moment crests along the touchdown pipeline formed as a
result of pipe bending and soil softening. Under the combined axial tension, bending moment, and
hydrostatic force, the von Mises stress of the pipeline increased to some extent and attained 20.8% of
J. Mar. Sci. Eng. 2020, 8, 119
13 of 22
459.33 kN·m, and some bending moment crests along the touchdown pipeline formed as a result of
pipe bending and soil softening. Under the combined axial tension, bending moment, and hydrostatic
J. Mar. Sci. Eng. 2020, 8, 119
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force,
the von Mises stress of the pipeline increased to some extent and attained 20.8% of the maximum
value from 461.27 to 557.10 MPa. Similarly, the maximum longitudinal strain of the pipeline rose
the maximum value from 461.27 to 557.10 MPa. Similarly, the maximum longitudinal strain of the
by 23.9%
from
tofrom
0.353%.
Moreover,
the
maximum
embedment
had a remarkable
pipeline
rose0.285%
by 23.9%
0.285%
to 0.353%.
Moreover,
thepipeline
maximum
pipeline embedment
had a
enlargement
1139.5% from
(0.130D)
0.533
m (1.616D),
and
maximum
resistance
remarkableofenlargement
of 0.043
1139.5%
from to
0.043
(0.130D)
to 0.533
mthe
(1.616D),
and seabed
the maximum
grew
by 199.8%
fromgrew
1.837
) to 5.507
(8.097w
is demonstrated
these results
s ). ItkN/m
seabed
resistance
by(2.701w
199.8%sfrom
1.837kN/m
(2.701w
s) to 5.507
(8.097ws). It isfrom
demonstrated
thatfrom
the energy
ratio coefficient
has an
obvious
effecthas
on an
theobvious
pipelineeffect
dynamic
and seabed
these results
that the energy
ratio
coefficient
on thebehaviors
pipeline dynamic
resistance.
Especially,
when
the Ep1Especially,
reaches 0.45,
the
wave causes
drastic
dynamic
responses
behaviors
and seabed
resistance.
when
thefreak
Ep1 reaches
0.45, the
freak wave
causes
drastic of
of the
pipeline in
and
seabed
the dynamic
pipeline responses
and seabed
interaction
the
TDZ.interaction in the TDZ.
700
5000
Ep1=0.30
Te(kN)
Ep1=0.40
Ep1=0.45
3000
M(kN⋅m)
Ep1=0.35
4000
Ep1=0.30
600
Ep1=0.35
500
Ep1=0.40
400
Ep1=0.45
300
200
2000
100
1000
-2500
-2000
-1500
-1000
x(m)
-500
0
0
-2500
500
-2000
-1500
(a)
-1000
x(m)
-500
0
500
(b)
600
0.4
Ep1=0.30
Ep1=0.30
Ep1=0.35
Ep1=0.40
ε (%)
σ (MPa)
Ep1=0.45
Ep1=0.35
0.3
Ep1=0.40
400
Ep1=0.45
0.2
200
0.1
-2000
-1500
-1000
x(m)
-500
0
0.0
-2500
500
-2000
-1500
(c)
-1000
x(m)
-500
(d)
8
Ep1=0.30
0.6
0.2
Ep1=0.35
Ep1=0.35
6
Ep1=0.40
P(kN/m)
1.2
Ep1=0.30
z/D
z(m)
4
0.6
500
6
0.0
0.0
0.4
0
Ep1=0.45
4
P/ws
0
-2500
2
1.8
Ep1=0.40
2
Ep1=0.45
0.8
-2400
-2200
-2000
x(m)
(e)
2.4
-1800
0
-2400
-2200
-2000
0
-1800
x(m)
(f)
Figure
15. Dynamic
responses
the S-laying
pipeline
freakenergy
wave ratio
energy
ratio
Figure
15. Dynamic
responses
of theofS-laying
pipeline
under under
variousvarious
freak wave
coefficients:
coefficients:
tension;
(b) bending
moment;
stress;
strain; (e)
pipeline embedment;
seabed
(a) tension;
(b) (a)
bending
moment;
(c) stress;
(d) (c)
strain;
(e)(d)
pipeline
embedment;
(f) seabed(f)
resistance.
resistance.
5.2. Effect of the Wave Focusing Location
5.2. Effect of the Wave Focusing Location
A noticeable characteristic of freak waves is the crest value appearing at the focusing position
A noticeable
characteristic
of freak
is the
the influence
crest valueofappearing
the focusing
position
where the
wave energy
accumulates.
To waves
explore
the waveatfocusing
location
on the
where
the
wave
energy
accumulates.
To
explore
the
influence
of
the
wave
focusing
location
on
the
dynamic responses of the laying pipeline, five focusing locations, xp = −200, −100, 0, 100, 200 m, were
dynamic responses of the laying pipeline, five focusing locations, xp = −200, −100, 0, 100, 200 m, were
assumed to simulate the freak waves shown in Figure 9b, which were separately taken as the input
surface wave conditions to perform a dynamic analysis of pipeline installation. The pipeline and
seabed response results illustrated in Figure 16 are the axial tension, bending moment, von Mises
stress, longitudinal strain, pipeline embedment, and seabed resistance.
When the wave focusing location varied from −200 m to 200 m, the pipeline and seabed
responses firstly rose and then dropped. The maximum responses occurred at the center position xp
J. Mar.
8, 119
= 0Sci.
m Eng.
with2020,
a peak
axial tension of 4550.13 kN, bending moment of 654.13 kN·m, von Mises stress14ofof 22
536.49 MPa, longitudinal strain of 0.340%, pipeline embedment of 0.406 m (1.231D), and seabed
resistance of 4.685 kN/m (6.889ws). The pipeline responses and seabed resistance at xp = 100 m and xp
assumed
towere
simulate
thelarger
freakthan
waves
in Figure
9b, which
weremseparately
taken
as the
input
= 200 m
slightly
the shown
corresponding
results
at xp = −100
and xp = −200
m, for
which
surface
wave
conditions
to
perform
a
dynamic
analysis
of
pipeline
installation.
The
pipeline
the freak waves produced by the forward focusing location led to more prominent motion responsesand
seabed
response
resultsEvidently,
illustrated
Figure 16
are theof
axial
tension,
bending
von Mises
of the
pipelay vessel.
theindynamic
behaviors
the laying
pipeline
andmoment,
seabed resistance
stress,
strain,
and seabed resistance.
are longitudinal
greatly influenced
bypipeline
the waveembedment,
focusing location.
700
5000
xp=-200 m
xp=0 m
4000
Te(kN)
xp=100 m
xp=200 m
M( kN⋅m)
xp=-100 m
3000
xp =-200 m
600
xp =-100 m
500
xp =0 m
400
xp =100 m
xp =200 m
300
200
100
2000
-2500
-2000
-1500
-1000
x(m)
-500
0
0
-2500
500
-2000
-1500
(a)
-1000
x(m)
-500
0
500
(b)
600
0.4
xp =-200 m
xp =-200 m
xp =-100 m
xp =100 m
xp =200 m
ε (%%
σ (MPa )
400
xp =-100 m
0.3
xp =0 m
xp =0 m
xp =100 m
0.2
xp =200 m
200
0.1
0
-2500
-2000
-1500
-1000
x(m)
-500
0
0.0
-2500
500
-2000
-1500
(c)
-1000
x(m)
-500
0
500
(d)
0.0
6
0.0
8
x p=-200 m
x p=-100 m
1.2
x p=0 m
6
x p=0 m
s
x p=100 m
4
x p=200 m
P/w
x p=-100 m
P(kN/m)
z/D
z(m)
x p=-200 m
0.4
4
0.6
0.2
2
2
x p=100 m
x p=200 m
0.6
-2400
-2200
-2000
1.8
-1800
0
-2400
-2200
-2000
x(m)
x(m)
(e)
(f)
0
-1800
Figure
Dynamic
responsesofofthe
theS-laying
S-laying pipeline
pipeline under
wave
focused
positions:
Figure
16. 16.
Dynamic
responses
undervarious
variousfreak
freak
wave
focused
positions:
(a) tension;
bending
moment;(c)
(c)stress;
stress;(d)
(d)strain;
strain; (e)
(e) pipeline
seabed
resistance.
(a) tension;
(b)(b)
bending
moment;
pipelineembedment;
embedment;(f)(f)
seabed
resistance.
When the wave focusing location varied from −200 m to 200 m, the pipeline and seabed responses
firstly rose and then dropped. The maximum responses occurred at the center position xp = 0 m
with a peak axial tension of 4550.13 kN, bending moment of 654.13 kN·m, von Mises stress of 536.49
MPa, longitudinal strain of 0.340%, pipeline embedment of 0.406 m (1.231D), and seabed resistance of
4.685 kN/m (6.889ws ). The pipeline responses and seabed resistance at xp = 100 m and xp = 200 m
were slightly larger than the corresponding results at xp = −100 m and xp = −200 m, for which the
freak waves produced by the forward focusing location led to more prominent motion responses of
the pipelay vessel. Evidently, the dynamic behaviors of the laying pipeline and seabed resistance are
greatly influenced by the wave focusing location.
J. Mar. Sci. Eng. 2020, 8, 119
15 of 22
J. Mar. Sci. Eng. 2020, 8, 119
15 of 22
5.3. Effect of the Wave Phase Range
5.3. Effect of the Wave Phase Range
The wave phase range plays a significant role in generating freak waves and, to some degree,
The wave phase range plays a significant role in generating freak waves and, to some degree,
determines the wave height by controlling the phases of wave components in a specified region.
determines the wave height by controlling the phases of wave components in a specified region. Five
Five groups of the wave phase range, ϕ = 1.0π, 1.1π, 1.2π, 1.3π and 1.4π, were selected to produce
groups of the wave phase range, φ = 1.0π, 1.1π, 1.2π, 1.3π and 1.4π, were selected to produce the
the freak wave trains shown in Figure 9c, and the influence of the wave phase range on the pipeline
freak wave trains shown in Figure 9c, and the influence of the wave phase range on the pipeline
behaviors
was
explored
wavetrains
trainswith
withthe
the
developed
S-lay
FEM
behaviors
was
exploredbybythe
thecombination
combination of
of these
these wave
developed
S-lay
FEM
for for
timetime
domain
dynamic
analyses.
seabedresponse
responseresults
results
aspects
of axial
tension,
domain
dynamic
analyses.The
Thepipeline
pipeline and
and seabed
onon
aspects
of axial
tension,
bending
moment,
von
Mises
stress,
longitudinal
strain,
pipeline
embedment,
and
seabed
resistance
bending moment, von Mises stress, longitudinal strain, pipeline embedment, and seabed resistance are
displayed
in Figure
17. 17.
are displayed
in Figure
ϕ=1.0π
ϕ=1.1π
ϕ=1.2π
ϕ=1.3π
ϕ=1.4π
Te(kN)
5000
4000
3000
700
ϕ=1.0π
ϕ=1.1π
ϕ=1.2π
ϕ=1.3π
ϕ=1.4π
600
M(kN⋅m)
6000
500
400
300
200
2000
100
1000
-2500
-2000
-1500
-1000
x(m)
-500
0
0
-2500
500
-2000
-1500
(a)
-1000
x(m)
-500
0
500
(b)
ϕ=1.0π
ϕ=1.1π
ϕ=1.2π
ϕ=1.3π
ϕ=1.4π
σ (MPa )
400
0.4
ϕ=1.0π
ϕ=1.1π
ϕ=1.2π
ϕ=1.3π
ϕ=1.4π
0.3
ε (%−
600
0.2
200
0.1
-1500
-1000
x(m)
-500
0
0.0
-2500
500
-2000
-1500
(c)
6
0.0
0.2
0.6
0.8
-2400
1.2
P(kN/m)
ϕ=1.0 π
ϕ=1.1 π
ϕ=1.2 π
ϕ=1.3 π
ϕ=1.4 π
z/D
z (m)
4
0.6
-500
0
500
(d)
0.0
0.4
-1000
x(m)
ϕ=1.0π
ϕ=1.1π
ϕ=1.2π
ϕ=1.3π
ϕ=1.4π
8
6
s
-2000
4
P/w
0
-2500
2
1.8
-2200
-2000
x(m)
(e)
2.4
-1800
2
0
-2400
-2200
-2000
0
-1800
x(m)
(f)
Figure
Dynamic responses
responses of
pipeline
under
various
freakfreak
wave wave
phase phase
ranges:ranges:
(a)
Figure
17.17.Dynamic
of the
theS-laying
S-laying
pipeline
under
various
tension; (b)
stress;
(d)(d)
strain;
(e) (e)
pipeline
embedment;
(f) seabed
resistance.
(a) tension;
(b) bending
bendingmoment;
moment;(c)(c)
stress;
strain;
pipeline
embedment;
(f) seabed
resistance.
With
increase
of wave
the wave
phase
1.0π
to all
1.4π,
the pipeline
and seabed
With
the the
increase
of the
phase
rangerange
from from
1.0π to
1.4π,
theall
pipeline
and seabed
responses
haddecreases.
prominentThe
decreases.
The reductions
in the maximum
values45.0%
were 45.0%
the axial
hadresponses
prominent
reductions
in the maximum
values were
for thefor
axial
tension,
tension,
from
5034.62 kN;
to 2769.11
for the moment,
bending moment,
fromto661.99
to kN·m;
506.08 29.0%
kN·m; for
from
5034.62
to 2769.11
23.6%kN;
for 23.6%
the bending
from 661.99
506.08
the von Mises stress, from 565.67 to 401.41 MPa; and 32.4% for the longitudinal strain, from 0.361%
J. Mar. Sci. Eng. 2020, 8, 119
16 of 22
J. Mar. Sci. Eng. 2020, 8, 119
16 of 22
29.0% for the von Mises stress, from 565.67 to 401.41 MPa; and 32.4% for the longitudinal strain, from
0.361% to 0.244%. Moreover, the maximum pipeline embedment reduced by 97.2%, from 0.649
(1.967D)
0.018 m (0.055D),
and the
maximum
seabed resistance
by 81.1%,
from 5.793
to
0.244%.toMoreover,
the maximum
pipeline
embedment
reduced bydropped
97.2%, from
0.649 (1.967D)
to
(8.518w
to 1.097 kN/m
(1.613w
s). When
the wave
phasedropped
range was
thefrom
bending
0.018
ms)(0.055D),
and the
maximum
seabed
resistance
by 1.0π,
81.1%,
5.793moment
(8.518wsand
) to
von Mises
ofs the
pipeline
in thephase
TDZ range
tremendously
to form
some and
crests,
illustrated
1.097
kN/mstress
(1.613w
). When
the wave
was 1.0π,jumped
the bending
moment
vonasMises
stress
in Figure
17b,c. in
This
can be explained
peakcrests,
curvesasofillustrated
pipeline embedment
and
of
the pipeline
thephenomenon
TDZ tremendously
jumped tofrom
formthe
some
in Figure 17b,c.
seabed
resistance can
shown
in Figurefrom
17e,fthe
as peak
the cyclic
of the
pipeline and
penetrating
into and
This
phenomenon
be explained
curvesmotions
of pipeline
embedment
seabed resistance
uplifting
from the
seabed,
resulting
in the
softening
trenching
ofand
seabed
soil, from
and the
drastic
shown
in Figure
17e,f
as the cyclic
motions
of the
pipelineand
penetrating
into
uplifting
the seabed,
pipe–seabed
interactions
induced
by freak
waves
causing
pipeline
flexural
deflections.
These
resulting
in the
softening and
trenching
of seabed
soil,
and thegreat
drastic
pipe–seabed
interactions
induced
results
adequately
demonstrate
that
the
phase
range
of
freak
waves
greatly
influences
the
dynamic
by freak waves causing great pipeline flexural deflections. These results adequately demonstrate
behaviors
of the
pipeline
the greatly
seabed,influences
particularly
the entire
axialoftension
and pipeline
that
the phase
range
of freakand
waves
the for
dynamic
behaviors
the pipeline
and the
embedment
as well for
as seabed
resistance
in theand
TDZ.
seabed,
particularly
the entire
axial tension
pipeline embedment as well as seabed resistance in
the TDZ.
5.4. Effect of Wave Peak Value
5.4. Effect of Wave Peak Value
Another noteworthy feature of freak waves is the peak value which generally represents the
impact
levels on
offshore structures.
order
to better
understand
wavegenerally
peak value
effect on the
Another
noteworthy
feature of In
freak
waves
is the
peak valuethe
which
represents
dynamiclevels
behaviors
of the S-laying
pipeline,
the five
representative
freak
Figure
impact
on offshore
structures.
In order
to better
understand
thewave
wavetrains
peakshown
value in
effect
on
9d were
generated
withof
their
wave
of 3.6, 4.1,
4.6, wave
5.1, and
5.6 m.
A time
the
dynamic
behaviors
the corresponding
S-laying pipeline,
thepeak
fivevalues
representative
freak
trains
shown
in
domain9d
analysis
of pipelinewith
installation
under these freak
conducted
to obtain
pipeline
Figure
were generated
their corresponding
wavewaves
peak was
values
of 3.6, 4.1,
4.6, 5.1,the
and
5.6 m.
and
seabed
response
results,
as shown
in Figureunder
18. these freak waves was conducted to obtain the
A
time
domain
analysis
of pipeline
installation
Since
theseabed
wave peak
valueresults,
gradually
became
pipeline
and
response
as shown
in larger
Figurefrom
18. 3.6 to 5.6 m, all the pipeline and seabed
responses
obvious
The
axial tension
of the
pipeline
and
Since showed
the wavean
peak
valueincrease.
gradually
became
larger from
3.6overall
to 5.6 m,
all the became
pipelinegreater,
and seabed
the maximum
tension
enlargedincrease.
by 32.6%,The
fromaxial
3647.71
to 4838.41
Thepipeline
bendingbecame
momentgreater,
of the
responses
showed
an obvious
tension
of the kN.
overall
pipeline
mildly increased
byenlarged
9.7% for its
value,
from to
602.24
to 660.69
MPa,
in the overbend.
and
the maximum
tension
bymaximum
32.6%, from
3647.71
4838.41
kN. The
bending
moment
Meanwhile,
themildly
bending
moment
thefor
sagbend
had a great
withtothe
increment
of the
its
of
the pipeline
increased
byin
9.7%
its maximum
value,increase
from 602.24
660.69
MPa, in
maximum Meanwhile,
value, attaining
103.2%, moment
from 197.25
tosagbend
400.83 kN·m.
the maximum
von Mises
overbend.
the bending
in the
had a Likewise,
great increase
with the increment
of
stress
of the pipeline
rose by 17.1%,
from
471.98
toto
552.47
MPa,
andLikewise,
the maximum
longitudinal
strain
its
maximum
value, attaining
103.2%,
from
197.25
400.83
kN·m.
the maximum
von Mises
of theofpipeline
roserose
by by
19.5%,
0.350%.
the maximum
pipeline
stress
the pipeline
17.1%,from
from 0.293%
471.98 toto552.47
MPa,Additionally,
and the maximum
longitudinal
strain
embedment
and
seabed
resistance
remarkably
enlarged
by 507.0%
127.3%,pipeline
respectively,
from
of
the pipeline
rose
by 19.5%,
from 0.293%
to 0.350%.
Additionally,
the and
maximum
embedment
0.086seabed
(0.261D)
to 0.522remarkably
m (1.582D)enlarged
and from
(3.510w
s) to 5.426
kN/m (7.978w
). Therefore,
and
resistance
by2.387
507.0%
and 127.3%,
respectively,
from s0.086
(0.261D)the
to
increase
in the freak
peak (3.510w
value would
result
in great
augmentation
of the
pipeline
behaviors
and
0.522
m (1.582D)
and wave
from 2.387
kN/m
(7.978w
increase
in the freak
s ) to 5.426
s ). Therefore,
seabedpeak
resistance.
wave
value would result in great augmentation of pipeline behaviors and seabed resistance.
4000
η p=3.6 m
700
ηp=3.6 m
η p=4.1 m
600
ηp=4.1 m
η p=4.6 m
500
ηp=4.6 m
400
ηp=5.1 m
300
ηp=5.6 m
Te(kN)
η p=5.1 m
η p=5.6 m
3000
M (kN⋅m)
5000
200
100
2000
-2500
-2000
-1500
-1000
x(m)
-500
0
500
0
-2500
(a)
-2000
-1500
-1000
x(m)
(b)
Figure 18. Cont.
-500
0
500
J. Mar. Sci. Eng. 2020, 8, 119
J. Mar. Sci. Eng. 2020, 8, 119
17 of 22
17 of 22
600
0.4
ηp=3.6 m
ηp=4.1 m
σ (MPa )
ηp=5.1 m
ηp=5.6 m
200
ηp=4.1 m
0.3
ε ( %%
ηp=4.6 m
400
ηp=3.6 m
ηp=4.6 m
ηp=5.1 m
0.2
ηp=5.6 m
0.1
0
-2500
-2000
-1500
-1000
x(m)
-500
0
0.0
-2500
500
-2000
-1500
(c)
-1000
x(m)
-500
0
500
(d)
0.0
6
0.0
ηp=3.6 m
8
ηp=4.1 m
ηp=4.6 m
1.2
ηp=5.1 m
6
ηp=4.6 m
2
s
ηp=5.1 m
4
ηp=5.6 m
P/w
P( kN/m)
ηp=4.1 m
0.4
4
0.6
ηp=3.6 m
z/D
z (m)
0.2
2
ηp=5.6 m
0.6
-2400
-2200
-2000
1.8
-1800
0
-2400
-2200
-2000
x(m)
x(m)
(e)
(f)
0
-1800
Figure
18. Dynamic
Dynamicresponses
responsesofof
S-laying
pipeline
under
various
freak peak
wavevalues:
peak values:
(a)
Figure 18.
thethe
S-laying
pipeline
under
various
freak wave
(a) tension;
tension;
(b) bending
stress;
(d)(e)strain;
(e) pipeline
embedment;
(f)resistance.
seabed resistance.
(b) bending
moment;moment;
(c) stress;(c)(d)
strain;
pipeline
embedment;
(f) seabed
6. Discussion
Discussion and
and Implications
Implications
6.
The deepwater
deepwater S-lay
S-lay FEM
FEM is
is aa complicated,
complicated, non-linear
non-linear structural
structural system,
system, and
and dynamic
dynamic response
response
The
analysis of
of the
the laying
laying pipeline
pipeline under
under freak
freak waves
waves is
isdifficult
difficult and
andtime-consuming
time-consuming for
for marine
marine structure
structure
analysis
engineers.
A
simplified
technique
was
presented
to
estimate
the
pipeline
dynamic
response
amplitudes
engineers. A simplified technique was presented to estimate the pipeline dynamic response
by means of by
the means
dynamic
(DAFs), which
defined which
by the maximum
responses
amplitudes
ofamplification
the dynamicfactors
amplification
factorsare(DAFs),
are defined
by the
relative
to
the
corresponding
static
results.
As
a
consequence,
the
dynamic
response
amplitudes
of the
maximum responses relative to the corresponding static results. As a consequence, the dynamic
laying
pipeline
can
be
easily
determined
if
the
static
responses
and
DAFs
are
given.
response amplitudes of the laying pipeline can be easily determined if the static responses and DAFs
As shown in Figure 19a, the pipeline and seabed DAFs in the parametric analyses were obtained
are given.
with As
theshown
variation
of the energy
coefficient.
AlongDAFs
with in
thethe
increase
of theanalyses
energy ratio
in Figure
19a, theratio
pipeline
and seabed
parametric
werecoefficient
obtained
E
,
the
DAFs
of
axial
tension,
bending
moment,
stress,
and
strain
gradually
increased,
in which
the
p1 the variation of the energy ratio coefficient. Along with the increase of the energy
with
ratio
tension DAF
prominent
from
1.69 to
2.37. The
pipeline
DAFincreased,
largely rose
coefficient
Ep1was
, the relatively
DAFs of axial
tension,
bending
moment,
stress,
and embedment
strain gradually
in
from
3.75
to
46.41,
and
the
seabed
resistance
DAF
increased
from
2.35
to
7.04.
Figure
19b
shows
the
which the tension DAF was relatively prominent from 1.69 to 2.37. The pipeline embedment
DAF
variation
in from
pipeline
seabed
DAFs
with the
wave focused
position, from
and all
thetoDAFs
firstly rose
largely
rose
3.75and
to 46.41,
and
the seabed
resistance
DAF increased
2.35
7.04. Figure
19b
up
and
then
dropped
down.
The
maximum
tension
DAF
reached
2.19,
and
the
maximum
pipeline
shows the variation in pipeline and seabed DAFs with the wave focused position, and all the DAFs
embedment
and
resistance
DAFsThe
reached
35.35 tension
and 5.99,
respectively.
Moreover,
pipeline
firstly
rose up
andseabed
then dropped
down.
maximum
DAF
reached 2.19,
and thethe
maximum
and seabed
DAFs with
theseabed
variation
in the wave
range
are and
illustrated
in Figure 19c.
As the wave
pipeline
embedment
and
resistance
DAFsphase
reached
35.35
5.99, respectively.
Moreover,
the
phase
range
increased,
all
of
the
DAFs
reduced
step
by
step.
The
DAF
reductions
were
from
2.43
to
pipeline and seabed DAFs with the variation in the wave phase range are illustrated in Figure 19c.
1.34
for
axial
tension,
from
56.50
to
1.57
for
pipeline
embedment,
and
from
7.40
to
1.40
for
seabed
As the wave phase range increased, all of the DAFs reduced step by step. The DAF reductions were
resistance.
thetension,
pipelinefrom
and seabed
enlarged
stage
by stage with
augmentation
from
2.43 toOppositely,
1.34 for axial
56.50 toDAFs
1.57 for
pipeline
embedment,
andthe
from
7.40 to 1.40
of
the
wave
peak
value,
as
displayed
in
Figure
19d,
the
DAF
increment
in
axial
tension
was from
for seabed resistance. Oppositely, the pipeline and seabed DAFs enlarged stage by stage
with 1.42
the
to 1.56, and theofDAF
increments
in pipeline
embedment
and seabed
resistance
were from
7.49 tension
to 45.44
augmentation
the wave
peak value,
as displayed
in Figure
19d, the
DAF increment
in axial
and from
obtained
DAFs of thein
pipeline
and
seabed behaviors
couldresistance
offer intuitional
was
from 3.05
1.42toto6.93.
1.56,These
and the
DAF increments
pipeline
embedment
and seabed
were
knowledge
for
offshore
pipeline
engineers,
which
could
be
used
to
consider
the
freak
wavebehaviors
effects in
from 7.49 to 45.44 and from 3.05 to 6.93. These obtained DAFs of the pipeline and seabed
the initial
stage.knowledge for offshore pipeline engineers, which could be used to consider
could
offerdesign
intuitional
the freak wave effects in the initial design stage.
J. Mar. Sci. Eng. 2020, 8, 119
J. Mar. Sci. Eng. 2020, 8, 119
3.0
18 of 22
18 of 22
50
Te
M
30
DAF
DAF
40
σ
ε
2.5
z (z/D)
P (P/ws)
2.0
1.5
20
10
1.0
0.30
0.35
Ep1
0.40
0
0.30
0.45
0.35
Ep1
0.40
0.45
(a)
2.5
50
Te
M
40
σ
ε
DAF
DAF
2.0
z (z/D)
P (P/ws)
30
20
1.5
10
1.0
-200
-100
0
x p(m)
100
0
-200
200
-100
0
x p(m)
100
200
(b)
60
2.5
z (z/D)
Te
P (P/ws)
M
σ
ε
40
DAF
DAF
2.0
20
1.5
1.0
1.0
1.1
1.2
ϕ (π)
1.3
0
1.0
1.4
1.1
1.2
1.3
ϕ (π)
1.4
(c)
2.5
T
60
e
M
σ
ε
40
DAF
DAF
2.0
z (z/D)
P (P/ws)
1.5
1.0
3.6
20
4.0
4.4
4.8
ηp(m)
5.2
0
3.6
5.6
4.0
4.4
η p(m)
4.8
5.2
(d)
Figure 19. Effect
Effect of freak wave conditions on dynamic amplification factors of pipeline behaviors and
position; (c)
(c) phase
phase range;
range; (d)
(d) peak
peak value.
value.
seabed resistance: (a) energy ratio coefficients; (b) focused position;
5.6
J. Mar. Sci. Eng. 2020, 8, 119
19 of 22
7. Conclusions
This paper presented a profound investigation of freak wave effects on the dynamic responses of
offshore pipelines for deepwater installation. For this purpose, an extended FEM of the S-lay system
was developed in OrcaFlex with the particular consideration of freak waves. The linear superposition
method of combined transient wave trains and random wave trains was applied to generate a series of
freak wave trains. The wave induced pipelay vessel motions, pipe–stinger roller interactions in the
overbend, as well as the cyclic contacts between the pipeline and seabed in the TDZ were also taken
into account in the dynamic analysis of laying pipelines. The influences of the freak wave energy ratio
coefficient, focusing location, phase range, and peak value on the pipeline and seabed behaviors were
estimated in detail, and the DAFs of the axial tension, bending moment, von Mises stress, longitudinal
strain, pipeline embedment, and seabed resistance were derived. Some significant conclusions were
obtained as follows:
(1)
(2)
(3)
(4)
The reasonable selection of wave parameters can effectively generate a variety of freak wave trains
by the linear superposition model. The maximum heights of freak wave trains are obviously
different with variations in the energy ratio coefficient, focusing position, phase range, and peak
value. The freak wave trains could be steadily incorporated into the developed S-lay FEM to
implement the dynamic analysis of deepwater pipeline installation.
The energy ratio coefficient has a great influence on the generation of freak waves and the induced
pipeline dynamic responses. With an increase in the energy ratio coefficient for transient waves,
all the pipeline behaviors and seabed resistance remarkably increase. Especially, when the Ep1
reaches 0.45, the interaction responses of the touchdown pipeline and seabed soil are drastically
noticeable, which causes tremendous variation in the bending moment, von Mises stress, and
pipeline embedment in the TDZ.
The dynamic behaviors of the laying pipeline and seabed resistance are also strongly influenced
by the wave focusing location. When the focusing wave is located at the center position xp = 0 m,
the responses of the offshore pipeline and seabed resistance are the most significant. Besides, the
axial tension, pipeline embedment, and seabed resistance for the forward wave focusing location
are slightly larger than the corresponding results for the negative wave focusing location.
The phase range and peak value of freak waves were proven to be important influencing factors in
the pipeline and seabed responses. As the wave phase range increases, the axial tension, bending
moment, von-Mises stress, longitudinal strain, pipeline embedment, and seabed resistance as
well as their DAFs remarkably decrease. On the contrary, when the wave peak value becomes
larger, the pipeline behaviors and seabed resistance obviously augment.
Author Contributions: Conceptualization, P.X. and S.G.; methodology, P.X. and S.G.; software, P.X.; validation,
P.X.; formal analysis, P.X. and Z.D.; investigation, P.X. and Z.D.; resources, P.X. and S.G.; data curation, Z.D.;
writing—original draft preparation, P.X. and Z.D.; supervision, S.G.; funding acquisition, P.X. and S.G. All authors
have read and agreed to the published version of the manuscript.
Funding: This research was funded by the National Natural Science Foundation of China (grant numbers 51809048,
51779223) and the Natural Science Foundation of Fujian Province, China (grant number 2018J05081).
Acknowledgments: The authors would like to thank the anonymous reviewers for their constructive comments
and suggestions.
Conflicts of Interest: The authors declare no conflict of interest.
Nomenclature
Ai
Ao
B
Ca
CD
internal cross-section area
external cross-section area
coefficient of the Ramberg–Osgood model
added mass coefficient
drag coefficient
J. Mar. Sci. Eng. 2020, 8, 119
d
D
E
Ep1
Ep2
EAnom
fm
g
k1
k2
ki
Kmax
ks
L
L0
Mb
n
N
Nc
Pi
Po
Pu (z)
r1
r2
S(f )
Su0
Sug
tc
tp
t’p
Te
Tw
Tor
wa
ws
xp
α
γ
κ2
µ
ν
ρc
ρp
ρsoil
ρw
ωi
φi
σy
ϕ
τ
ξ
ς
ζ
shortest separation distance of the center lines between the pipe and roller
pipe outer diameter
elastic modulus
energy ratio coefficient of a transient wave
energy ratio coefficient of a random wave
nominal axial stiffness
peak frequency
gravitational constant
pipe contact stiffness
roller contact stiffness
wave number of the ith wave component
soil normalized maximum stiffness
soil shear stiffness
instantaneous length of a line segment
unstretched length of a line segment
bending moment
power exponent of the Ramberg–Osgood model
number of wave components
soil nominal bearing capacity factor
internal pressure
external pressure
soil ultimate penetration resistance
pipe radius
roller radius
spectral density function
soil mudline shear strength
soil shear strength gradient
corrosion coating thickness
wave focusing time
pipe wall thickness
effective tension
wall tension
torque moment
pipe weight per unit length in air
pipe submerged weight per unit length
wave focusing position
spectral energy coefficient
peak enhancement factor
curvature
soil friction coefficient
Poisson’s ratio
pipe corrosion coating density
pipe density
saturated soil density
sea water density
angular frequency of the ith wave component
phase lag of the ith wave component
effective yield stress
twist angle
spectral width parameter
axial damping coefficient
bending damping coefficient
torsional damping coefficient
20 of 22
J. Mar. Sci. Eng. 2020, 8, 119
21 of 22
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