Hydrodynamic Aspects of Moored
Senti-Submersibles and TLP's
J.A. Pinkster, A. Dercksen and
A.K. Dey
Offshore Technology Conference,
Houston, Texas, USA, May 1993
Report No. 966-P, May 1993
Delft University of Technology
Ship Hydromechanics Laborato,y Mekelweg 2
2628 CD Delft The Netherlands Phone 015 - 7868 82
VOLUME I
25th ANNUAL
OFFSHORE TECHNOLOGY
CONFERENCE
LJt1i
ANNIVERSARY
1993
PROCEEDINGS
VOLUME i
ABSTRACT
The mean and low-frequency horizon-tal wave drift forces on 2 types of semi-submersible structures in regu-lar and in irreguregu-lar waves are
de-termined from model tests and
calcu-lations. For the measurement of the low-frequency drift forces in irre-gular waves use is made of a special
dynamic system of restraint.
Comparison of measured and computed drift forces in irregular waves show
increasing divergence between
predictions based on 3-dimensional potential theory and results of
ex-periments with increasing severity of
the irregular sea conditions.
Comparison between computed and
measured mean drift forces in regulat
waves show increasing divergence at
lower wave frequencies. A simple
model for approximating viscous
contributions to the drift forces in
irregular waves is applied to some
test results and it ís shown that the
correlation between measurements and predictions is improved.
In order to gain more detailed insight in the mechanisms of the
viscous contribution to the drift
force tests were carried out with single fixed vertical cylinder in
Hydrodynamic Aspects of Moored Semi-Submersibles and TLP's
J .A. Pinkster
Deift University of Technology
A. Dercksen
Maritime Research Institute Netherlands
A. K. Dey
Deift University of Technology
regular waves. The results of tests confirm that in conditions of waves
without current the major part of the viscous contribution to the drift force is confined to the splash zone of the cylinder.
INTRODUCTION
The motions and mooring forces of
Semi-Submersibles and TLP's moored in exposed locations are often dominated
by wave effects. These may be
sub-divided in first order wave frequency forces with frequencies corresponding
to the individual waves and mean and
low-frequency second order wave drift forces related to wave groups.
From the point of view of the design
of mooring systems both first and
second order wave loads and the mo-tion and mooring load response need
to be taken into account. At the
design stage predictions of these
quantities for a particular design
can be based on computational
methods, model tests or a rational
combination of both.
Computational methods for wave
frequency loads and motion response for semi-submersibles have been in
development since the early 70's.
based on linear hydrodynamic theory
and have proved their worth on many
occasions.
Non-linear, mean wave drift forces on
semi-submersible type structures can be computed based on the application of linear, 3-dimensional diffraction
theory computational methods combined
with either a far-field method or a near-field method for the evaluation
of the second order wave loads on the structure. In case a far-field method
is applied, generally only the mean second order horizontal drift forces
can be calculated. See reference [2] and reference [3] . If a near-field or
pressure integration method is
applied the mean and low-frequency
components of the drift forces can be
computed for 6 degrees of freedom.
See reference [4] . This type of
computational method assumes the flow
to be inviscid thus excluding any
effects which might arise from
separated flow around the structure. In the past efforts have been made to
verify the computational methods for the mean and low-frequency or slowly varying wave drift forces on
semi-submersible type structures. See
reference [5] . It has been surmised
that the drift forces on
semi-submersible type structures, which
consist of relatively slender
surface-piercing columns and
sub-merged floaters, are in some cases
significantly affected by viscous
effects in the flow around the
structural elements. Very little
ex-perimental data is available which
can give insight in such effects. See reference [10]
In order to increase insight in these effects MARIN, in co-operation with a number of offshore operators,
design-ers and manufactures, carried out
extensive model test programs and
computations among others of the mean
and slowly varying wave forces on
slender and full semi-submersibles. In this paper a number of aspects of
this research including the model
test programs and the correlation
between model test results and
results of computations are
discussed.
The findings of these studies have
confirmed that significant viscous
effects can be present in the
low-frequency wave forces on such
structures. As a result, a research
program has been initiated by the
Deift University of Technology into
determining such effects on
structu-ral elements of semi-subrnersibles
such as the columns and the
pon-toons. The purpose of this research
is to determine for which of these
elements the viscous effects play an
important role and, if possible, to
develop a rational computational
procedure for taking such effects
into account when determining the
mean and slowly varying drift forces
on the complete structure. In this
paper some results of recent model tests carried out on a fixed
verti-cal cylinder in waves are presented.
SECOND ORDER WAVE DRIFT FORCES
ON A SEMI-SUBMERIBLE
The subjects of this investigation were a slender 8-column Semi-Submer-sible I with circular columns and a displacement of 23,270 tonnes and a
full 6-column Semi-Submersible II
wíth square columns and a
displace-ment of 56,300 tonnes. The body plans of the semi-submersibles are given in Figure 1 and Figure 2. In the
follow-ing all results of measurements and computations will be given for the
full scale structures.
The aims of the study were as
follows:
-To increase insight in the mean and
low-frequency horizontal wave
excit-ing forces and motion responses of
large semi-submersibles
-To check the validity of
computa-tional methods for the prediction
of first order wave frequency
mo-tions and low-frequency wave drift forces based on 3-dimensional
The total scope of the research does not allow all aspects to be treated
here. In this paper the results of
the following investigations are
presented:
-Results of model tests in regular
waves to determine the mean hori-zontal wave drift force response. -Results of tests in irregular waves
to determine the mean and low-fre-quency wave drift force records.
The model tests were carried out at a scale of 1:40 in the Seakeeping Basin of MARIN. This basin measures 100 m x 24 m x 2.5 m.
MODEL TEST SET-UP IN THE BASIN
Measurements of the mean horizontal wave drift forces on a model in re-gular waves can be carried out using a soft-spring restraining or mooring system which consists of horizontal
wires incorporating soft linear
springs which are connected to force
transducers mounted on the model. The
mooring wires are connected at deck
level. The set-up for tests in regular waves is shown in Figure 3.
In order to measure the mean and
slowly varying horizontal wave drift
forces in irregular waves, ideally
the model should be moored in such a
way that all low frequency motion
response is suppressed while leaving the model completely free to carry
out the motions at wave frequencies.
The first requirement ensures that
the measured force is not affected by
dynamic magnification effects. The
second requirement can be deduced
from theoretical analysis of the
second order wave drift forces which show that part of the total second order excitation forces are directly dependent on the structural motions
at wave frequencies. See reference
[4]
As a consequence, the model
re-straining system must possess the
characteristics of an ideal Dynamic
Positioning system. For the model
tests a system consisting of
hori-zontal restraining wires connected to controllable tension winches was selected. See Figure 4. The winches
were operated based on an active
control system with a feed-back loop
supplemented by a feed-forward
control loop. See Figure 5.
The feed-back loop acted on the
hori-zontal position error and the time
derivative of the error (Proportio-nal-Differential control) . The
feed-forward control loop was based on the real-time measurement of the
re-lative wave elevation on the up-wave columns of the semi-submersible. It has been shown that a major part of the mean and slowly varying second order wave drift forces as predicted by potential theory, is due to terms
related to the square of the instan-taneous relative wave elevation
around the waterline of a floating
structure. This has been
demon-strated, among others, from model
tests on a tanker. See reference [4]
Application of back and
feed-forward control still does not result in full suppression of low-frequency motions however. This due to the fact that the feed-forward loop is
supply-ing an imperfect estimate for the
instantaneous low frequency
horizon-tal force. As a result, the total
restraining force is not equal and opposite to the low frequency wave
exciting force thus resulting in
residual low frequency motions. See
Figure 6. In order to obtain a best estimate of the total low frequency
wave force on the model, the measured
restraining force is corrected for
the residual horizontal motions of
the vessel. This is carried out
off-line after a test has been carried
out. The basic assumption behind this process is that the instantaneous
discrepancy between the true wave
force and the measured restraining force results in horizontal motion accelerations which are described by
the following relationship:
in which m represents the virtual
mass of the vessel and x(t) the
¡no-tion accellera¡no-tion. Assuming that the virtual mass is constant, the accele-ration force can be determined in the
time domain by passing a
double-differentiating filter over the time record of the low frequency horizon-tal motions. The best estimate of the
time record of the horizontal drift
force then follows from:
Fd(t) = Fm(t)
+ m (t)An example of time records of
measured restraining force, residual
surge motion, correction force and
total drift force are shown in Figure 7, The results apply to Semi-Submer-sible II.
In order to verify the accuracy of
this procedure model tests were
repeated using different settings of
the dynamic restraining system.
An example of the results found for the spectral density of the slowly
varying wave drift force on the Semi-Submersible II in irregular head seas is shown in Figure 8.
The results apply to the system of
restraint being adjusted to
repre-senting a spring system
(Proportio-nal control), a spring and damper
system (Proportional -Differential
control) and a P-D control including Feed-forward based on the relative
wave elevation measurements. The
results shown in the figure indicate
that the spectral density of the
drift force obtained from tests with
significantly different
characteris-tics of the restraining system are
reasonably consistent.
TESTS IN REGULAR WAVES
Tests in regular waves were carried out for both semi-submersibles for a
range of wave frequencies, wave
amplitudes and wave directions. For
the slender Semi-Submersible I tests
in head seas were carried out
with-out and with bracings. The results
are given in Figure 9 through Figure 13 for both structures in head waves and in beam waves as mean drift force transfer functions.
In the figures the theoretical values
found on the basis of 3-dimensional
potential theory computations
ex-cluding the contribution from the
bracings are also given.
Comparison between the results of mo-del tests and computations show that in the lower wave frequency range the
mean drift forces tend to be
consi-stently underestimated by the
compu-tations. The effect of the bracings
on the mean drift forces on the
slender Semi-Submersible I in head
seas is to increase slightly the mean drift forces as can be seen from the comparison between the measured results shown in Fígure 9 and in
Figure 11.
TESTS IN IRREGULAR WAVES
Tests were again carried out for both semi-submersibles. The slender Semi-Submersible I was tested with-out
bracings.
Results of tests in irregular waves
are given in the form of time traces
of the measured low frequency drift forces compared with time traces of
the corresponding predicted low
fre-quency force based on 3-dimensional potential theory. In some cases the
spectral density of the computed and measured forces are compared. For the time domain predictions, use was made
of second order impuls response functions combined with the measured
time trace of the undisturbed
ir-regular wave record in the basin. See reference [5] . The time domain second order impuls response functions for the drift forces are obtained from the complete second order quadratic transfer functions computed in the
frequency domain. The quadratic transfer functions were computed
based on the pressure integration
Tests were carried out in different irregular sea conditions in order to determine the dependency of the cor-relation between computed and mea-sured forces on the sea condition. Time traces of the measured and com-puted drift force records for irre-gular haed seas are given in Figure
14 through Figure 17. The spectral
densities of the computed and
mea-sured surge drift forces on
Semi-Submersible II are compared in Figure
18 through Figure 20. Comparison
between measured and computed data
show that the correlation is good in low sea conditions with relatively
short mean periods. En higher sea
conditions combined with
corres-pondingly longer mean wave periods
the correlation worsens. Beside
significant differences in the force peak values, the phase shift between
peaks in the measured and computed
records increases in higher sea con-ditions. The trend is more or less
the same for both types of
semi-submersibles.
DISCUSSION
OF
RESULTS
FROM
TESTS IN REGULAR AND IRREGULAR
WAVES
The results found from tests in
regular and irregular waves with
respect to the drift force seem to support each other in that in both
cases the correlation between
measurement and computations worsen with an increase in the wave period.
The reduction in the correlation
seems to be accompanied by an
in-creasing phase shift between measured and computed forces. The peaks in the
computed drift forces tend to shift
relative to the wave groups. See
Figure 17.This is related to the fact
that in longer waves diffraction
effects which make up the major part of the drift forces in shorter waves
are reduced. In longer waves the
low-frequency drift forces are to a
larger extent dominated by the compo-nents related to the second order
set-down waves present in the irregu-lar wave field. The troughs of these
waves, which have periods comparable
to the wave group periods, are in
phase with the peaks of the wave
groups. See Figure 21. The
low-frequency wave force components due
to these waves are in phase with the
horizontal acceleration of the fluid which is largest when the slope of
the set-down waves is greatest. This
occurs after the peak in the wave
group passes the structure. Due to
this effect the peaks in the computed
wave drift forces in irregular waves with longer mean periods tend to lag
behind the peaks in the wave groups.
The measured records, however, still
shown that the peak forces co-incide
with the peaks in the wave groups. A
possible explanation is that in
longer waves, viscous forces, which
are dominated by velocity related
effects, are becoming relatively more important. Since the fluid velocities
are highest near the peaks in the
wave group, peaks in viscous contri-butions to the drift forces will also
tend to co-incide with the peaks in
the wave groups.
In order to investigate this effect,
a simple model for the viscous con-tributions in the horizontal drift
forces has been investigated and some further comparisons between the
measured and computed drift forces, including viscous contributions, on the slender semi-submersible carried
out.
VISCOUS COMPONENTS OF THE DRIFT
FORCES IN IRREGULAR WAVES
The model used to describe the
vis-cous contribution to the drift forces
is based on the assumption that
Morison's equation for the drag force
on a vertical cylinder in waves can
be applied to the surface-piercing parts of the columns of a
semi-sub-mersible. See reference [6] through
reference [10] . For the case of waves
without current it can be shown that, as a first approximation, the viscous
drag force contribution to the drift
forces is confined to the splash zone on a column. The viscous drag terni is determined from the following equation:
ç (t)
Fvdft)
p Cd5 v(t),Iv(t)
D dZ
in which:
v(t) = relative horizontal velocity between the
fluid and the column
D = column diameter
Ç(t) = relative wave elevation
Cd drag coefficient
This contribution to the drift force
could be evaluated for each column in
the time-domain based on the
un-disturbed wave elevation record, the
frequency domain motion
characteris-tics of the semi-submersible and an assumption regarding the drag coef-ficient in the above equation. The summation of the drag force on each
column results in the estimated
vis-cous drag force contribution to the
drift force. The total drift force is found by adding the viscous and potential contributions.
The results of thes computations are
shown in Figure 22 for the slender
Semi-Submersible I in irregular head
seas. In this figure the wave
eleva-tion record, the potential part of
the drift force and the viscous part of the drift force are shown in the
top three traces, The lower trace
shows the sum of the viscous force
and the potential force compared with the total measured force.
It is clear that the result of adding the viscous contribution is a clearly improved correlation with the
measured force. In order to show the overall effect of adding a viscous
contribution to the potential
contri-bution spectra of the low-frequency
surge force in irregular head seas
and sway force in beam seas on Semi-Submersible I are given in Figure 23
for three different sea conditions. Each figure shows the drag
coeffi-cient Cd used for the computations of
the viscous force contribution. The Cd values used for the computations of the viscous contribution in some
cases had to be adjusted in order to achieve a reasonable fit with the
measured data. This clearly is an
unsatisfactory aspect of the
simpli-fied model for the viscous effect
which will need to be refined in the
future. An important effect not
accounted for is for instance, the
shielding effects due to the
proximity of the columns. However,
the above results tend to confirm
that there is a significant viscous effect in the drift forces on
semi-submersible type structures which, in irregular waves without current seems to be concentrated in the splash zone of the columns. The analysis has been
based on a rather simple model for the viscous contribution which has
not been verified to any great
extent. In the next section some
results of ongoing detailed research
carried out at the Deift University of Technology into such effects is
described.
VISCOUS EFFECTS IN DRIFT FORCES
ON A FIXED VERTICAL CYLINDER
In the previous section it was indi-cated that the most significant
vis-cous contribution to the horizontal
drift force on a semi-submersible
seems to originate from the splash
zone of the columns. In order to gain
more insight in such effects, model
tests have been carried out to deter-mine the distribution along the
ver-tical of the mean horizontal drift force on a single vertical cylinder
in regular waves. The work is part of an on-going Ph.D. project.
See reference [11]
The model tests were carried out in
Hydro-mechanics Department. This facility measures 80 m x 2.75 m x 1.25 m and
is equiped with a single flap
hydraulically operated wave-maker
capable of generating regular and
irregular waves. The basin is fitted
out with a towing carriage with a
special low speed carriage control
for the simulation of current effects by towing.
The model cylinder which had a dia-meter of 0.075 m is shown in Figure
24. At scale 1:100 this could be re-presentative of a column with a 7.5 m
diameter. The splash zone and the
sub-surface part are independently
attached to a central core through
force transducers measuring the
horizontal force on each of the two
sections.
Model tests were carried out in regu-lar waves with and without current.
For each test the vertical position of the cylinder was adjusted so that the through of the wave passing the cylinder passed just above the sepa-ration between the splash zone part of the cylinder and the sub-surface part of the cylinder. This ensured
that the sub-surface part of the
cylinder was fully submerged at all
times. Results of measurements in
regular waves without current of the mean horizontal drift force on the splash zone and the sub-surface zone
are compared with results of
calcula-tions of the relevant contribucalcula-tions
to the drift forces based on
3-dimen-sional potential theory and the
ap-plication of the pressure integration or near-field method in Figure 25 and Figure 26 respectively.
According to the near-field theory
for drift forces, the splash zone
contribution is dependent on the
square of the relative wave elevation
around the cylinder while the drift force on the subsurface element is due to the non-linear pressure con-tribution in the Bernoulli pressure
equation. For this reason the results
of mean force measurements have been divided by the square of the
undis-turbed wave amplitude. Results are
given for the model scale.
The model tests were carried out for a range of wave frequencies
corres-ponding to the longer waves for a
semi-submersible. At scale 1:100 the
wave frequencies tested in the model correspond to 0,3 r/s to 0.8 r/s at
full scale. This is a range of
frequencies relevant for extreme sea
conditions.
The results shown in Figure 25 and Figure 26 confirm that the greatest discrepancies between the potential computations and the measurements of
the mean forces are found for the
splash zone of the cylinder. The
measured mean forces are consistently
significantly larger than the
com-puted values. For the sub-surface
part of the cylinder, differences
also occur between measurements and
computations. In a relative sense
they appear to be of the same order
as for the splash zone part. However,
the absolute value of the forces is
considerable lower and the
differen-ces between measurements and
compu-tations are less consistent.
It can be concluded that these model tests poit to the splash zone
contri-bution to the viscous part of the
mean drift force as being the most
important one.
FINAL REMARKS
In thís paper we have shown some
results of an extensive series of
model tests on two semi-submersibles
which confirm differences between
computed and measured mean and
low-frequency horizontal wave drift forces in regular and irregular
waves.
Application of a simple model for the viscous contribution to the drift forces indicated that irregular waves
without current the major source of the viscous contribution was to be
found at the splash zone part of the columns of a semi-submersible.
Model test in regular waves with a
fixed vertical cylinder representing a single column of a semi-submersible
or a TLP confirm that the largest
discrepancies between computed and measured drift forces are indeed to be found in the splash zone.
Further experimental investigations are required in order to be able to formulate a more detailed model for the viscous effects which can also
take into account such aspects as the interaction effects due to the proxi-mity of the columns of a
semi-submer-sible.
REFERENCES
Hooft, J.P. : 'Hydrodynarnic
Aspects of Semi-Submersible Platforms' , Publication No.
400, Netherlands Ship Model Basin, 1972
Newman, J.N. : 'The Drift Force and Moment on Ships in Waves'
Journal of Ship Research, 1966 Faltinsen, 0M, and Michelsen,
F.C. : 'Motions of Large
Struc-tures in Waves at Zero Froude
Number' , Symposium on Marine Vehicles, London, 1974
Pínkster, J.A. : 'Low-Frequency Second Order Wave Exciting Forces on Floating Structu-res' , Publication No. 650,
Netherlands Ship Model Basin, Wageningen, 1980
Pinkster, J.A. and Hutjsmans,
R.H.M.: 'The Low Frequency
Mo-tions of a Semi-Submersible in Waves', Boss'82, Boston, 1982
Pijfers, J.G.L. and Brink, A.W. : 'Calculated Drift Forces
of Two Semi-Submersible Plat-form Types in Regular and
Ir-regular Waves', Paper No. OTC
2977, Offshore Technology
Conference, Houston, 1977
Huse, E. : 'Wave induced Mean
Force on Platforms in
Direc-tion Opposite to Wave
Propa-gation' , Norwegian Maritime Research, Vol.5, No.1, 1977
Standing, R.G. , Brendling, W.J. and Jackson, G.E.:
'Full-scale Measured and Predicted
Low-Frequency Motions of the
Semi-Submersible Support
Ves-sel 'Uncle John' ' , First
In-ternational Offshore and Polar
Engineering
Conference,Edinburgh, 1991
Ferretti, C. and Berta, M.:
'Viscous Effect Contribution to the Drift Forces on
Float-ing Structures' , International
Symposium on Ocean Engineering Ship Handling, Gothenburg, '80
Chakrabarti, AK.: 'Steady
Drift Force on Vertical
Cylin-der - Viscous vs. Potential',
Applied Ocean Research, Vol.6, No.2, 1984
Dey, A.K. : 'Experimental
In-vestigations of Viscous Mean
Drift Forces on a Fixed Verti-cal Circular Cylinder in Waves
and Currents Part I', Report
No. 928-M, Ship Hydrodynamics
Department, Delft University of Technology, 1992
9.14 20 57 59.44 3 05 Dimensions in m OC 05 9.14 5.49 5 .49 9 14 22.86 i .83 22.36 22.86
Fig. 1 - General arrangement of Semi-Submersible I.
14.0 25.0 73.5
-I I I I I I ---JL__
--Dimensions are given in metres
25.0
r--i
__L_
L90.0
15.0
Fig. 2 - General arrangement of Semi-Submersible II.
9.0
28.5
10.5
13.5
/
/
E
Tre ransducer
xi
Fig. 3 - Test set-up for tests in regular waves
45
450
Force crCsducer
Servo unit Feed- foGard control svs tern Feed-back control system Vessel:
Mass and damfling characteristics Waves Drift forces Relative wave elev. Horizontal motion
Fig. 5 - Block diagram of control system for
tests in irregular waves
F (Wave drift force) w
Motions
FB (Force from control system)
Flg.
6- B1ok diagram
of forces actitig on thetructure.
Horizontal motions
relative wave elevazon Vessel
Force
= 3.1 in
=7.0 s
dir
= 1800 5.00 Wave o . . . . :.\; 100.00tf Measured restraining force a
0-",\
i/
\ ', \\ ¡ d 'I 100.00 ti 100.00 ti f'°
'V \fi
III ej 0 50 100 t in S Correction force b m .I"
'"J
'i V Total force a + bI
,i'\
\
'j 'J A ;V \i 'I
V' A z_f.
\J\ /JJj
Fig. 7---Example of measuredrestraining frce(aorrectjofcfor
motions(b) and total drift force record(a+b) m
5.00
20 o CN C -4 X i., 3J VC C e
Wave dIrection L8O degrees
Wave charactertstics: 5.49 ni
wl/3
= 11.30 s
System of restraint based upon:
15-10 S k Sorings
-
springs motion + + 1,-
sprinas motion relative wave 0 0.25 0.50 0.75Wave frequency in rad/s
Fig. 8 - Spectra of drift forces obtained for different restraining
-20 -lo o 20 lo o
Calculation
O
Regular waves. 0.5 1.0 in rad.sec.1 1.5Fig. 9 - Mean Surge drift force on Semi-Submersible I in regular head
waves
Fig. 10 - Mean sway drift force on Semi-Submersible I in regular beam
wave s
o 0.5 1.0 1.5
-20 -lo o ('1 culat±c'n L O Reu1ar wa',es o D o
L
O 0.5 1.0 1.5 C')in radsec1
Fig. 11 - Mean surge drift force on Semi-Submersible I in regular head
waves including effect of bracings o
-50 N -25 rd N o
50
N E s-.-A25
rd N -s-. o I cuìatiouO Q L Reii1ar waves (ascenrig wave height)
8
o
s
o
0.5
1.01.5
w rad / s
Fig. 13 - Mean sway drift force on Smi-Submersib1e II in regular beam
waves
o
0_5
1.0
1.5w radis
Fig. 12
- Mean surge drift force on
Semi-Submersible II in regular
head waves
Cajcuiation
O Q Re1ar waves. (ascending wave height)
s
o
i
o '-, o
5.00 - Wave
4JMç5' = 3.09;
= 7.12 s
--m0
-5.00 1- Measured
Calculated 10.00 -Force t f O-- :
-10.00 J
-. 5.00 - Wave A j O ti.
riI'!\\
i\/\
c'.tJ\t\At!\
e\-H.,i',
r,'n O
v \!
\i
.J\/\_
4J
= 5.85 'n;
= 11.30 s
10.00-tf O .--10.00 5.00'no
-5.00 10.00-tf O -10.00-Force 0 50 100 t in seconds/
--Wave 1 A !í\At
/1A1-AA-Al
A R ;V\ r\ 1\ I!'\
/;
\J\\!U\il\l\j/\ij/\J\/
4J'
11.24 'n;
- 1425 s
Force r.r
N ;-/
Fig. 14 - Low-Frequency surge drift force on Semi-Submersible I in
5.00 -, 100.00 tf 0 -100.00
I
0 50 100 tin s
Fig. 15 - Low-Frequency surge drift force on Semi-Submersible II
in
irregular head seas, 1-Is 3.1 m, Ti = 7.1 s
5.00-nj Wave
¡ H
A ÏAfl
iL,
AIHth
m H
Vj
-S.00 Force 0 50 100 tin s
Force - -' ____:----___-
'N___'/T
-/
----
Measured Calculated"z-= 5-5
m T]=ll..3s
dir
= 1800
Fig. 16 - Low-Frequency surge drift force on Semi-Submersible II in
irregular head seas, Hs = 5.5 ru, Ti 11.3 s
O,'
Wave.
... . -5.00-
Measured= 3.1 in
Calculated=7.ls
dir
= 180°
100.00T
tfL..
100.00-5.00 -5.00 100.00
T
tf O -100.00 NForce
I II 050 100
t in sFig. 17 - Low-frequency surge drift force
on Serai-Submersible II in
irregular head seas, Hs 10.3 ra, Ti 14.5 s
Wave J\Ì
/rN-c -
- - -;---
- - -.f j ( f1¡ f r 4JWj = 10.3 in- Measured
= 14.5 s
Calculateddir
= 1800rj N A
5000
3 rj10000
oMeasured
Calculated
Measured
Calculated
O c)rad/s
Fig. 19 - Spectral density ot surge drift force of Figure 16 on
Semi-Submersible II
10000
N L I' 5000 I' I'l1 I t I J t I V 's I'I t-O O0.25
0.50
()rad/s
Fig. 18 - Spectral density of surge drift force of Figure 15 on
Semi-Submersible II
10000
ii
ij'
j jil
I I i t ' 50004.- t I I t Ij
00.25
rad/s
Measured
Calculated
20000
rl
ji
iii
0.50
Fig. 20 - Spectral density of surge drift force of Figure 17 on
Semi-Submersible II i i
15000 -
I i i I I N cf5.00
in O
-5.00
25.00
Fig. 21 - Wave set-down in irregular waves
T
J
Wave
CD = 0.80
\f
Force Calculated (potential part) a
Fig. 22 - Low-frequency surge drift force on Semi-Submersible
I in irregular head seas
j
- - - MeasuredCalculated (viscous part) b
tf O -25.00 25.00 tf -25.00 25.00
-Force Total calculated
a +b
tf O -
-=---25.00
0 50 100
160
0
400
O
)4easured durino riiodel test
Calculated, otential contribution only Calculated, viscous effect included
Head seas beam seas
4000
2000
O
Fig. 23 - Spectra of low-frequency drift forces on Semi-Submersible I
H5 = 3.09; T1 = 7.1 s C =0.60 D \ H5 = 3.09; D T1 = 7.1 s \ \\ Rs = 5.85; T1 = 11,3 C =0.20 s H5 5.85; T1 = 11.3 s CD = 0. 75 H5
11.24; T1 = 14.1
CD = 1.00 s H5 = 11.24; T1 = 14.1 = 0. 1 5 s o 0.2 0.4 o 02 0.4 W in rad/s CL) in cad/s Cn N 200 160 80 o 800 400 o 400 - 200 oloo
80
60
40
20
2750 75MEAN DRIFT FORCE [NIM21
UPPER DUMNY CYLISIIER UPPER TEST CYLISOER
FORCE TRANSDUCER
LOWER TEST CYLINDER
FORCE TRANSDUCER
LOWER SliMilY CYLINDER
Fig. 24 - Arrangement and model set-up of fixed vertical cylinder
HIGHEST SET OF WAVE AMP.
NTEMEDIATE SET OF WAVE AMP.
(L) LOWEST SET OF WAVE AMP.
O
A
O
Fig. 25 - Mean drift forces on the splash zone part of the cylinder
0 1 2 3 4 5 6 7 8
OMEGA R/S1
MEASURED(I) MEASURED(H)
POTENTIAL THEORY A MEASURED(L)
O O O
60
40
20
o
-20
MEAN DRIFT FORCE [NIM2]
0
1 2 3 4 5 6 7 8OMEGA ER/SI
0 MEASURED(I) O MEASURED(H)
- POTENTIAL THEORY
0 MEASURED(L)Fig. 26 - Mean drift forces on the subsurface part of the cylinder
80
-s HIGHEST SET OF WAVE AMP.
NTEMEDIATE SET OF WAVE AMP.
(L) LOWEST SET OF WAVE AMP.
O O O
O