numerical study of two vessels seakeeping in waves
TRANSCRIPT
Copyright © 2014 by ASME
NUMERICAL STUDY OF TWO VESSELS SEAKEEPING IN WAVES
Dexin Zhan Oceanic Consulting Corporation
St. John’s, NL, Canada
Don Bass Don Bass Marine Consulting
St. John’s, NL, Canada
David Molyneux Oceanic Consulting Corporation
St. John’s, NL, Canada
ABSTRACT This paper presents a numerical study of seakeeping in regular
waves for two vessels in close proximity using commercial
seakeeping software HydroStar and an in-house code
MOTSIM. The objective was to study the possible sheltering
effect of the larger vessel (FPSO) on the smaller one (OSV)
during personnel transfer between the two vessels, where one
vessel was at some angle relative to the other vessel and there
was no connection line between them. The study mainly
focused on the OSV motion resulting from the interaction of the
FPSO when the OSV was at different headings and wave
directions. Initially the OSV motions close to the FPSO (and
parallel) were compared with those for the OSV alone. For an
un-parallel position of the two vessels, an objective function
based on the OSV RAOs motion in roll, pitch and heave
directions was used to optimize the OSV position. Finally
comparisons between HydroStar and MOTSIM results are
provided.
The main conclusions are:
1) When the FPSO and OSV are located in parallel, the OSV
motions in sway, roll and yaw are larger than the single OSV
motions in head waves while surge, heave and pitch are almost
the same. The OSV motions in most of the six degrees of
freedom are smaller than the single OSV motions when the
waves are from other directions (always on the port side of the
FPSO), which means that there is a sheltering effect.
2) The simulation results from different OSV rotation angles
show that the hydrodynamic interaction between the FPSO and
OSV e.g. the sheltering effect is related to the OSV angle and
the wave heading. The objective function in roll, pitch and
heave RAOs indicates that the OSV should maintain a close to
parallel position with the FPSO to minimize motion when the
waves come from the port side of the FPSO from 180 to 240
degrees. When the wave direction is around 240 degrees the
OSV should have relatively small motion in waves for any OSV
rotation angle.
3) A comparison of HydroStar and MOTSIM results shows
that the MOTSIM results of a single vessel seakeeping
simulation is in a good agreement with HydroStar. In two
vessels situation more validation work needs to be done.
1. INTRODUCTION
There are many hydrodynamic interactions between bodies in
waves in oceanic engineering. For example, a shuttle tanker
may be alongside a FPSO while it takes on oil, or an offshore
supply vessel may be alongside a larger vessel which would be
taking on supplies. Another example is an underway
replenishment of long-term naval operations where two ships
travel in close proximity. One of the activities specific to
offshore operation is the transfer of personnel between support
vessels and other offshore structures. In the process of crew
transfer the two vessels/structures could be in different positions
or angles depending on the specific environment (such as wave,
wind or current). In some cases, the larger vessel is used to
provide a sheltering effect which can improve the likelihood of
a successful transfer. Therefore a study of the hydrodynamic
interaction between the two vessels is necessary and important.
In comparison to the single ship case, numerical seakeeping
simulation of the two-ship case is more complex because it has
12 degrees of freedom. Furthermore, hydrodynamic terms such
as added mass, damping, and wave diffraction force must
account for the presence of two ships in the flow field.
McTaggart et al. (2003) developed a frequency domain code
SHIPINT to predict motions in waves of two ships in close
proximity. A seakeeping experiment was conducted for
validation of this method using two semi-captive models in a
towing tank. In their research the two vessels were restricted to
a parallel position to model the replenishment process. Chen
and Fang (2001) also investigated hydrodynamic interactions
between two ships using a three-dimensional potential-flow
theory based on the source distribution technique. Islam (2013)
carried out a numerical study of dynamic interaction of parallel
moving ships in close proximity using speed dependent Green
function. A significant effect of the sway, roll and yaw for two
parallel moving ships was revealed. At present, research reports
of two un-parallel ships are few. In this paper the sheltering
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Proceedings of the ASME 2014 33rd International Conference on Ocean, Offshore and Arctic Engineering OMAE2014
June 8-13, 2014, San Francisco, California, USA
OMAE2014-23269
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effect between vessels in the process of personal transfer was
studied where the one vessel could be at some angle relative
another vessel. An optimization function based on the roll, pitch
and heave motion RAOs is presented to evaluate the supply
vessel movement at different rotation angles and wave
directions. Commercial software HydroStar and an in-house
code MOTSIM were used and their results were compared.
2. METHODOLGY FOR TWO VESSELS SEAKEEPING
2.1 HydroStar Software HydroStar is the commercial hydrodynamic software which has
been developed by Bureau Veritas since 1991. It provides a
complete solution of the first order problem of wave diffraction
and radiation and also the QTF for second order low-frequency
wave loads on a floating body with or without forward speed in
deep water and in finite water depth. Even though the classical
potential theory is applied, addition damping terms are included
in HydroStar to take into account energy dissipation that does
not exist when the inviscid and irrotational flow are assumed.
The HydroStar modules are shown in Figure 1, where the
commonly used modules are hslec (read geometry mesh), hsrdf
(compute radiation and diffraction), hsmec (compute ship
motions), and hsrao (output RAO files) etc. In version 7.02 of
HydroStar any number of bodies can be modeled [4]
. In multi-
body simulation the number of bodies and the first and last
identification numbers of the panels associated to each body are
defined in the input file while the coordinates and panels of
each body can be defined separately. The bodies’ relative
position are defined by two keywords TRANS and ROTA,
where the TRANS means translation in x- and y- direction, and
ROTA means rotation of the body mesh in the horizontal plane.
More details are given in Reference [4]. An example of two
vessel’s meshes and position for the FPSO and OSV in a
parallel position is displayed in Figure 2.
It should be noted that the CG positions of bodies also need to
be modified in the body motion input file when these vessels
change their relative position. For each translation and rotation
the new CG position of x and y coordinates of the vessels
should be recalculated by user. The matrix of inertia and
moments also needs be updated to respond to the global
coordinate system if you make a body rotation.
In HydroStar a RAOs file of the multi bodies is output when
running the hsrao module. The RAOs in directions of surge,
sway, heave, roll, pitch and yaw are relative to the global
coordinate system in the HydroStar software.
In this paper the main interest is focused on the OSV motion
under the potential sheltering effect of the FPSO. To compare
the OSV RAO motion at different rotation angles it is better to
express these RAOs in the OSV local coordinate system. In
order to solve the problem, instead of rotating the OSV we keep
the OSV fixed and translate/rotate the FPSO in the geometry
input file. In the process of translating and rotating the FPSO
the CG distance between the FPSO and OSV is kept the same as
the CG distance when translating/rotating the OSV. Meanwhile
the wave heading was also rotated with the FPSO to correspond
the wave from correct side of the FPSO. According to a
principle of relative motion the simulation results for these
movements are the same. But keeping in mind all the OSV
RAO results are relative to the OSV local coordinate system
when rotating the FPSO. For convenience, we still display the
position figure of the FPSO and OSV using rotating OSV in the
following section of this paper.
Figure 1: HydroStar Modules
Figure 2: Example of FPSO and OSV Bodies Meshes in
Parallel for HydroStar
2.2 MOTSIM Code
MOTSIM is a nonlinear time domain panel method based on a
weak scatterer hypothesis developed by Professor Don Bass in
association with NRC/IOT [5]
. Recently an extended version of
MOTSIM was developed in order to determine motions for two
vessels in close proximity.
The new version, MOTSIM12, basically doubles everything
that the older (six degrees of freedom) version does. For
example the ‘single’ version solves 21 equations, while the
‘double’ version solves 42 equations. The same ODE solver is
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used and practically all the routines in the six degrees of
freedom version are modified in a straight forward manner for
the 12 degrees of freedom case. The most significant changes
occur in the routines for memory function and scattering forces
calculation. They are changed significantly because the
hydrodynamics of two vessels oscillating side by side may
differ significantly from those for the individual oscillating
vessels. The hydrodynamics of two vessels operating side by
side are represented (in linear theory) by four sets of
hydrodynamic coefficients. If the vessels are named A and B,
there are four coefficients as follows:
(1) Added mass and damping coefficients for A due to the
oscillations of A in the presence of the vessel B at rest;
(2) Added mass and damping coefficients for A at rest with B
moving;
(3) Added mass and damping coefficients for B for B at rest
and A moving and;
(4) Added mass and damping coefficients for B moving in the
presence of A that is at rest.
From these coefficients, four added mass and damping files are
derived. The coefficients are calculated in a modified version of
the code Green3D using panel data from vessels A and B.
Memory functions for each of these four cases are derived using
Fourier series from the damping coefficients taken over a range
of 30 or 40 frequencies. The memory functions are integrated
with the appropriate accelerations using convolution integrals to
determine the inertial and scattering forces and moments acting
on the two vessels. Sectional accelerations and ‘average’
accelerations in the various modes and cross modes are
determined for these four cases according to their memory
functions. Similar convolution integrals are determined for
forward speed conditions using sectional or ‘averaged’
velocities instead of accelerations.
In order to overcome the drifting motion of the vessels in
MOTSIM, tethering lines are used to restrict vessels’ drifting. It
should also be noted that the OSV surge, sway and heave
motion in MOTSIM were transformed from global coordinate
to the OSV local coordinate in a post-processor in order to
compare with HydroStar result when the OSV had a rotation
angle.
3. SIMULATION PARAMETERS AND DEFINITIONS 3.1 Vessel particulars
Principal dimensions for the two vessels, Floating Production,
Storage and Offloading (FPSO) vessel and Offshore Supply
Vessel (OSV), are listed in Table 1. Only the loaded condition
was considered for the FPSO.
3.2 Definition of FPSO and OSV Positions
A global coordinate system OXYZ is established in Figure 3
which is the initial position of the FPSO, where origin O is
located at the water line and Z axis points upward. A local
coordinate system O’X’Y’Z’ for the OSV is also shown in the
figure. The translations in x and y directions are XT and YT, and
the rotation angle of OSV is α. As we mentioned in Section 2,
the RAO results of the OSV motion in this paper are relative to
the local coordinate system O’X’Y’Z’ for HydroStar and
MOTSIM.
Table 1: FPSO and OSV Principal Characteristics
Draft Units FPSO OSV
Lpp m 258 76.08
Breadth m 46 18
Draft m 18.35 6.47
Depth m 26.6 8.56
Displacement t 182409 6337
CG forward of
midship m 1.53 1.63
CG above keel m 15.33 6.7
GMt m 3.64 1.6
Kxx m 17.37 6.3
Kyy m 57.89 17.33
Kzz m 58.89 17.33
Figure 3: Definition of FPSO and OSV Positions
3.3 Wave heading definition
The wave heading angle definition is shown in Figure 4, where
the 1800 means head wave and 270
0 means beam wave from the
port. In this report four wave headings (180, 210, 240 and 270
degrees) are relative to the FPSO position, e.g. the global
coordinate system. And only regular waves were considered in
the simulation.
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Figure 4: Wave Heading Definition
4. SIMULATION RESULTS AND DISCUSSION 4.1 FPSO and OSV in Parallel Position
When the FPSO and OSV are parallel, the OSV angle α in
Figure 3 is 0 degree. The translation values of XT and YT are
138.2m and -62m, respectively, which means the OSV midship
is 47.2m ahead of the FPSO midship and the lateral gap
between the two vessels is 30m. Four wave headings (head
wave to beam wave) were used in the simulation to study the
sheltering effect. This might be the most common operational
scenario in crew transfer. The RAOs for the OSV next to the
FPSO are compared with the results of a single OSV as follows.
In this paper, the RAO is defined by motion amplitude divided
by the wave amplitude (roll, pitch and yaw are in degrees).
Figure 5 shows the comparison of RAOs between double
vessels and single vessel at 180 degrees waves (head wave)
using HydroStar software. It can be seen that when the FPSO
was present, the OSV sway, roll and yaw motion had some
changes compared to a single OSV, while the surge, heave and
pitch motions were close to the single OSV results (the values
of sway, roll and yaw of single OSV are all close to 0). This is
due to hydrodynamic interaction between the two ships when
they are in parallel and close proximity. These effects were
predicted by other researchers in numerical modeling and
physical model experiments for two parallel moving vessels[1][3]
.
For other wave directions (from the port side of the FPSO),
simulation results show that the OSV RAOs in most of 6
directions are smaller than results of a single OSV, which
indicates that the sheltering effect is more obvious when the
waves come from the port side of the FPSO. In these wave
conditions the OSV is located in a wave shadow of the FPSO
and the FPSO creates an obstruction to the propagation of
waves. Figure 6 shows an example of OSV RAOs comparison
of wave heading 240 degrees for double vessels and single
vessel (other wave angles are not shown in this paper). The
solid line represents the OSV result for the double vessels and
the dashed line with delta symbol is the ones of single OSV.
Frequency (r/s)
Surg
eR
AO
s(m
/m)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
Double, Wave 180 deg
Single, Wave 180 deg
OSV Surge RAOs, Wave 180
(a) Surge RAO
Frequency (r/s)
Sway
RA
Os
(m/m
)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
Double, Wave 180 deg
Single, Wave 180 deg
OSV Sway RAOs, Wave 180
(b) Sway RAO
Frequency (r/s)
Hea
veR
AO
s(m
/m)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
Double, Wave 180 deg
Single, Wave 180 deg
OSV Heave RAOs, Wave 180
(c) Heave RAO
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Frequency (r/s)
Rol
lRA
Os
(deg
/m)
0 0.5 1 1.5 20
2
4
6
8
10
Double, Wave 180 deg
Single, Wave 180 deg
OSV Roll RAOs, Wave 180
(d) Roll RAO
Frequency (r/s)
Pitc
hR
AO
s(d
eg/m
)
0 0.5 1 1.5 20
1
2
3
4
Double, Wave 180 deg
Single, Wave 180 deg
OSV Pitch RAOs, Wave 180
(e) Pitch RAO
Frequency (r/s)
Yaw
RA
Os
(deg
/m)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
Double, Wave 180 deg
Single, Wave 180 deg
OSV Yaw RAOs, Wave 180
(f) Yaw RAO
Figure 5: OSV RAO Comparisons for Double Vessels and
Single Vessel in Wave Angle 1800 (HydroStar)
Frequency (r/s)
Surg
eR
AO
s(m
/m)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
Double, Wave 240 deg
Single, Wave 240 deg
OSV Surge RAOs, Wave 240
(a) Surge RAO
Frequency (r/s)
Sway
RA
Os
(m/m
)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
Double, Wave 240 deg
Single, Wave 240 deg
OSV Sway RAOs, Wave 240
(b) Sway RAO
Frequency (r/s)
Hea
veR
AO
s(m
/m)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
Double, Wave 240 deg
Single, Wave 240 deg
OSV Heave RAOs, Wave 240
(c) Heave RAO
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Frequency (r/s)
Rol
lRA
Os
(deg
/m)
0 0.5 1 1.5 20
5
10
15
Double, Wave 240 deg
Single, Wave 240 deg
OSV Roll RAOs, Wave 240
(d) Roll RAO
Frequency (r/s)
Pitc
hR
AO
s(d
eg/m
)
0 0.5 1 1.5 20
1
2
3
4
Double, Wave 240 deg
Single, Wave 240 deg
OSV Pitch RAOs, Wave 240
(e) Pitch RAO
Frequency (r/s)
Yaw
RA
Os
(deg
/m)
0 0.5 1 1.5 20
0.5
1
1.5
Double, Wave 240 deg
Single, Wave 240 deg
OSV Yaw RAOs, Wave 240
(f) Yaw RAO
Figure 6: OSV RAO Comparisons for Double Vessels and
Single Vessel in Wave Angle 2400 (HydroStar)
4.2 FPSO and OSV with Relative Heading Angles to Waves
In this scenario the FPSO and OSV are in a position with a
translation and a rotation. The OSV rotation is relative to the
point O’, and the rotation angle α is defined as positive in
clockwise direction which could change from 0 to 180 degrees.
The XT and YT are still fixed at 138.3m and -62m, respectively.
In this situation a concern is focused on an analysis of sheltering
effect based on the all OSV motion RAOs in different OSV
rotating angles and wave directions.
As described above the crew transfer was conducted between
the FPSO and OSV. For a safe transfer in waves the smaller the
movement of the OSV, the lower the risk. According to the
transfer process, comparing with the OSV surge, sway and yaw
motions the roll, pitch and heave motions of the OSV play an
important role in the risk assessment. Normalized values of the
roll, pitch and heave motions were calculated by selecting the
maximum RAO motion in the frequency ranges divided by a
maximum value of all waves and OSV angles in the
corresponding motion. Then an objective function Y for an
optimization calculation based on the normalized data is created
as follows:
heavepitchroll YYY=Y
Where Yroll, Ypitch and Yheave are the normalized RAOs in roll,
pitch and heave, respectively. The Y is a function of the wave
direction and the OSV angle. Figure 7 shows the function Y
changes with wave headings while Figure 8 shows the function
Y changes with the OSV rotation angles (0~90 degrees).
From Figure 7 it can be seen that when the wave heading
changes from 180 to 240 degrees, the smallest value of Y is
appeared in OSV angle 0 degree. It means that the OSV should
keep in around 0 degree in order to keep a lower motion in roll,
pitch and heave directions when the waves come from 180 to
240 degrees. From Figure 8 it also can be seen that the lower
parts of function Y appears when the wave heading is 240
degrees, which means that comparing with the other wave
headings the sheltering effect is stronger when the waves come
from the 240 degrees whatever the OSV rotation angle is.
4.3 Comparison between HydroStar and MOTSIM Results
HydroStar and MOTSIM were developed by different
organizations. One is commercial software and another is an in-
house code. Their mathematic models applied to seakeeping
simulation are different. For example, a frequency domain
solver is used in HydroStar, a time domain is used in MOTSIM.
The most important is that the wave mean force (second order
wave force) was considered in MOTSIM, but HydroStar didn’t
calculate it in current RAO simulation in regular waves. The
wave drifting force affects ship’s motion in a considerable
range, especially for smaller frequency and higher amplitude
waves. This was observed in MOTSIM simulation when the
frequency is less than 0.3 rad/s and the simulation was
corrupted.
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Figure 9 shows a validation comparison between MOTSIM and
HydroStar results for a single OSV simulation in wave 210
degrees. A good agreement was achieved for these RAO results.
Figure 10 shows a comparison for double vessels simulation
while both vessels are in the parallel position (OSV 0 rotation
angle). Results of four wave directions are provided in the
figure. The dashed line with delta symbol represents MOTSIM
result while the solid line is HydroStar result. From the figure it
can be seen that in most of six directions MOTSIM data are
larger than the ones of HydroStar, and this phenomenon is also
appeared in other OSV angles (not provided in this paper). It is
considered that the current version of MOTSIM12 does not take
into account the sheltering type diffraction effects. A new
modification is on the way.
Wave Angle (deg)
Nor
mal
ized
Obe
jctiv
eFu
nctio
nY
160 180 200 220 240 260 280 300
1
1.5
2
2.5 OSV Angle 0 degOSV Angle 30 degOSV Angle 45 degOSV Angle 60 degOSV Angle 90 deg
Figure 7: OSV Normalized Objective Function Y Changes
with Wave Angles
OSV Angle (deg)
Nor
mal
ized
Obj
ectiv
eFu
nctio
nY
0 20 40 60 80 1001
1.5
2
2.5
3
3.5
4
Wave Angle 180 degWave Angle 210 degWave Angle 240 degWave Angle 270 deg
Figure 8: OSV Normalized Objective Function Y Changes
with OSV Angles
Frequency (r/s)
Hea
veR
AO
s(m
/m)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
HydroStar, Wave 210 deg
MOTSIM, Wave 210 deg
Single OSV Heave RAOs Comparison
(a) Surge RAO
Frequency (r/s)
Sway
RA
Os
(m/m
)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
HydroStar, Wave 210 deg
MOTSIM, Wave 210 deg
Single OSV Sway RAOs Comparison
(b) Sway RAO
Frequency (r/s)
Hea
veR
AO
s(m
/m)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
HydroStar, Wave 210 deg
MOTSIM, Wave 210 deg
Single OSV Heave RAOs Comparison
(c) Heave RAO
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Frequency (r/s)
Rol
lRA
Os
(deg
/m)
0 0.5 1 1.5 20
5
10
15
HydroStar, Wave 210 deg
MOTSIM, Wave 210 deg
Single OSV Roll RAOs Comparison
(d) Roll RAO
Frequency (r/s)
Pitc
hR
AO
s(d
eg/m
)
0 0.5 1 1.5 20
0.5
1
1.5
2
2.5
3
3.5
4
HydroStar, Wave 210 deg
MOTSIM, Wave 210 deg
Single OSV Pitch RAOs Comparison
(e) Pitch RAO
Frequency (r/s)
Yaw
RA
Os
(deg
/m)
0 0.5 1 1.5 20
0.5
1
1.5
2
HydroStar, Wave 210 deg
MOTSIM, Wave 210 deg
Single OSV Yaw RAOs Comparison
(f) Yaw RAO
Figure 9: OSV RAO Comparisons between HydroStar and
MOTSIM for Single Vessel in Wave 2100
Frequency (r/s)
Surg
eR
AO
s(m
/m)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
HydroStar, Wave 180 degHydroStar, Wave 210 degHydroStar, Wave 240 degHydroStar, Wave 270 degMOTSIM, Wave 180 degMOTSIM, Wave 210 degMOTSIM, Wave 240 degMOTSIM, Wave 270 deg
OSV Surge RAOs Comparison(Double Vessels, OSV 0)
(a) Surge RAO
Frequency (r/s)
Sway
RA
Os
(m/m
)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
HydroStar, Wave 180 degHydroStar, Wave 210 degHydroStar, Wave 240 degHydroStar, Wave 270 degMOTSIM, Wave 180 degMOTSIM, Wave 210 degMOTSIM, Wave 240 degMOTSIM, Wave 270 deg
OSV Sway RAOs Comparison(Double Vessels, OSV 0)
(b) Sway RAO
Frequency (r/s)
Hea
veR
AO
s(m
/m)
0 0.5 1 1.5 20
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
HydroStar, Wave 180 degHydroStar, Wave 210 degHydroStar, Wave 240 degHydroStar, Wave 270 degMOTSIM, Wave 180 degMOTSIM, Wave 210 degMOTSIM, Wave 240 degMOTSIM, Wave 270 deg
OSV Heave RAOs Comparison(Double Vessels, OSV 0)
(c) Heave RAO
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Frequency (r/s)
Rol
lRA
Os
(deg
/m)
0 0.5 1 1.5 20
5
10
HydroStar, Wave 180 degHydroStar, Wave 210 degHydroStar, Wave 240 degHydroStar, Wave 270 degMOTSIM, Wave 180 degMOTSIM, Wave 210 degMOTSIM, Wave 240 degMOTSIM, Wave 270 deg
OSV Roll RAOs Comparison(Double Vessels, OSV 0)
(d) Roll RAO
Frequency (r/s)
Pitc
hR
AO
s(d
eg/m
)
0 0.5 1 1.5 20
0.5
1
1.5
2
2.5
3
3.5
4
HydroStar, Wave 180 degHydroStar, Wave 210 degHydroStar, Wave 240 degHydroStar, Wave 270 degMOTSIM, Wave 180 degMOTSIM, Wave 210 degMOTSIM, Wave 240 degMOTSIM, Wave 270 deg
OSV Pitch RAOs Comparison(Double Vessels, OSV 0)
(e) Pitch RAO
Frequency (r/s)
Yaw
RA
Os
(deg
/m)
0 0.5 1 1.5 20
0.5
1
1.5
2
2.5
3
3.5
4
HydroStar, Wave 180 degHydroStar, Wave 210 degHydroStar, Wave 240 degHydroStar, Wave 270 degMOTSIM, Wave 180 degMOTSIM, Wave 210 degMOTSIM, Wave 240 degMOTSIM, Wave 270 deg
OSV Yaw RAOs Comparison(Double Vessels, OSV 0)
(f) Yaw RAO
Figure 10: OSV RAO Comparisons between HydroStar and
MOTSIM for Double Vessels in OSV Angle 00 (Parallel)
5. CONCLUSIONS This paper presents a numerical seakeeping simulation of two
vessels in close proximity with parallel or unparallel headings
using HydroStar and an in-house code MOTSIM. A normalized
optimization function based on vessel’s roll, pitch and heave
motion shows that the sheltering effect is stronger when the
supply vessel is located in a wave shadow of the FPSO which
means smaller movement of OSV and less riskiness for crew
transfer. Comparing with result of HydroStar, MOTSIM needs
more validation and modification in considering the sheltering
effect for two vessels seakeeping. It should be noted that the
viscous dissipation in the gap of two ships was not considered
in either software. The dissipation may largely damp the
vessel’s motion in reality[4]
although this usually applies to
much smaller gaps than the ones considered in this paper.
One observation made during the course of this research was
that there is very little data that can be used for validating
numerical simulations other than the head sea case, with
forward speed. This type of data would be very useful for
developing an understanding of the behavior of two ships in
close proximity for offshore engineering applications.
ACKNOWLEDGMENTS This work was carried out at Oceanic as part of a project which
was supported by the Atlantic Innovation Fund administered by
Atlantic Canada Opportunities Agency and additional funding
from Husky Energy. This support is gratefully acknowledged.
REFERENCES 1. Kevin McTaggart, David Cumming, C. C. Hsiung, Lin Li,
“Seakeeping of Two Ships in Close Proximity”, Ocean
Engineering 30 (2003), pp1051-1063.
2. Gung-rong Chen, Ming-chung Fang, “Hydrodynamic
interactions between Two Ships Advancing in Waves”,
Ocean Engineering 28 (2001), pp1053-1078.
3. M. Rafiqul Islam, Motohiko Murai, “Dynamic Interaction of
Parallel Moving Ships in Close Proximity”, J. Marine Sci.
Appl. 12 (2013), pp261-271.
4. HydroStar for Experts User Manual, Research Department
BUREAU VERITAS, March 2011.
5. Jacek S. Pawlowski, Don W. Bass, "A Theoretical and
Numerical Model of Ship Motion in Heavy Seas", SNAME
Transaction, Vol.9, 1991, pp. 319-352.
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