OFFSHORE TECHNOLGCY CONFERENCE 6200 North Central Expressway Dallas, Texas 75206
THIS PRESENTATION IS SUBJECT TO CORRECTION
The Role of Model Tests in the.Design of Single
Point Mooring Terminals
TECHNISCHE UNIVERSITErfLaboratorium 'mar
ScheepshydromechanIca
ArchiefMekelweg 2,2628 CD Delft
By . TebO15-788873-FaxO15781838J. A. Pinkster and G. F. M. Remery, Netherlands Ship Model Basin @Copyright 1975
Offshore Technology Conference on behalf of the American Institute of Mining, Metallurgical, and Petroleum Engineers, Inc. (Society of Mining Engineers, The Metallurgical Society and Society of Petroleum Engineers), American Association of Petroleum Geologists, American Institute of Chem.i-cal Engineers, American Society of Civil Engineers, American-Society of MechaniChem.i-cal Engineers, Institute of Electrical and Electronics Engineers, Marine Technology Society, Society of Explor-ation Geophysicists, and Society of Naval Architects and Marine Engineers.
This paper was prepared for presentation at the Seventh Annual Offshore Technology Conference to be held in Houston, Tex., May 5-8, 1975. Permission to copy is restricted to an abstract of not more than 300 words. Illustrations may not be copied. Such use of an abstract should contain conspicuous acknowledgment of where and by whom the paper is presented.
PAPER
NUMBER OTC 2212
ABSTRACT
This paper gives a broad outline of model tests with single point mooring
systems. This includes the purpose of the model tests, the information necessary to set up test programs, the scope of
tests, the characteristics simulated,
measurements carried out, possible
-sources of errors and the analysis of
results. Furthermore, examples of test results are given which.show phenomena
characteristic of s.p.m. terminals.
Finally, some of the phenomena observed during tests and a source of uncertainty in existing methods to calculate the behaviour of s.p.mvship systems are
discussed. INTRODUCTION
Single point mooring terminals are,
as the name implies, facilities of small horizontal dimensions, to which large vessels are moored by means of a bow hawser or by any other means which allows the vessel to rotate 3600 around
the mooring point. Generally, the single point mooring terminal can have two
References and illustrations at end of
paper.
functions. Primarily, it affords a safe
mooting-to the vessels in question.
Secondly, it can form a link in the
chain for the transport of oil.
The single point mooring terminal
can assume many forms as is shown in Fig. 1. The most common is the Catenary Anchor
Leg Mooring system (CALM) consisting of a flat cylindrical shaped buoy which is anchored to the sea floor by means of up to 8 chains. This system employs the properties of the catenary to supply the elasticity required when holding large tankers in open seas. The Single Anchor Leg Mooring system (SALM) consisting of a cylindrical buoy attached to a heavy base on the sea floor by means of a sin-gle pre-tensioned anchor-chain, obtains
its elasticity from the angle between
the single anchor leg and the vertical.
Enlarged version of the single point
mooring terminal are the Exposed Location Single Buoy mooring (ELSBM) and the SPAR.
The second of these does not only
ful-fill the function of mooring point and link in the oil transport chain, but is also used as a storage
unit-The types of mooring system
30 THE ROLE OF MODEL TESTS IN THE DESIGN OF SINGLE POINT MOORING TERMINALS OTC 2212
a correct interpretation is given of the results
Modern test procedures for single point mooring terminals are concentrated
on the following aspects:
Behaviour and system loads in extreme environmental conditions when the ter-minal is unoccupied. During these tests
the so-called survival conditions are
investigated. The system loads for
such a sea state combined with the pro-bability of occurrence of the sea state form the basis for determining the pro-bability of survival
or
system damage.Behaviour and system loads with the terminal occupied by a tanker. During these tests the upper limits (with
respect to environmental conditions)
for operating (transfer of oil) or the upper limits at which point the tanker must leave the mooring are
investiga-ted. The results of such tests combined
with the probability of occurrence of
limiting sea conditions form the basis for the evaluation of workability.
Behaviour and system loads under
envi-ronmental conditions which occur a large percentage of the time. These results, combined with fatigue and wear and tear data for the system components can form the basis for maintenance scheduling.
INPUT DATA FOR SETTING UP A TEST PROGRAM
In setting up a model test program
for a single point mooring terminal to be
placed in a certain location, the follow-ing environmental information should
preferably be known:
Water depth and tidal variation
Current: speed, direction, variations in speed and directions, de-pendence of speed and direc-tion on wind and waves
Waves : Probability of occurrence of a given significant wave height and period. Depen-dence of
significant
wave height on mean period. De-pendence ofsignificant
wave height on the direction of the wavesWind : Speeds and the relationship
between wind direction and wave direction and between wind speed and wave height Ideally such information should be obtained by wind, wave and current mea-surements taken at or near the proposed site over a longer period of time; say a
year or more. Generally, however, few
designers can afford the luxury or time to have iich measurements carried out.
and the SPAR primarily used in water
depths of up to approximately 150 ft.
Some of the systems can with
modifica-tions be used for even greater water depths, however.
Rigid spar buoys connected to the
sea floor by means of a universal joint are at present being designed. These
consist of a buoy at the surface rigidly
connected to a frame work which extends
down to the base. This type of mooring
is intended for water depths of 300 ft.
or more. Finally, there are the mooring towers which consist of a slender open
frame work fixed to the sea floor.
Unlike all other systems, this type of mooring terminal does not contribute to
the total elasticity of the system.
Generally, the tankers are
connect-ed to the mooring terminal by means of large circumference synthetic ropes
which are part of the operating equip-ment of the terminal itself. In one case where the vessel is permanently moored
to serve as storage space, the connec-tion consists of a rigid arm.
Single point mooring terminals can be, as may be gathered from this brief
review, complex systems which present a formidable problem to those who are en-gaged in their design. In the design of such systems a number of aspects must be taken into account. Firstly, the system must afford a safe mooring for the tanker
in sea conditions prevalent in the area where it is located. Secondly, when
sub-jected to severe loads, originating
either from the tanker or, for the case that the terminal is unoccupied, from severe sea conditions, the construction must not fail. Thirdly, the combined behaviour of the terminal and the tanker must be such that the loading or
dis-charging operation may be carried out for the greater part of the year.
In order to gain sufficiently reli-able data regarding the various aspects
pertaining to the total behaviour of
single point mooring terminals,
design-ers have frequently made use of model tests. These tests are carried out with
scale models of the terminal and the tankers in large basins in which the
environmental conditions expected in a
certain location can be reproduced. Such
model tests can provide information which may be inexpensible for an
effi-cient design, provided that:
- the correct parameters are investigated - the models and environmental
condi-tions are reproduced correctly
- the tests are carried out in a careful
In such cases, firms or institutes spe-cialized in collecting environmental
data on a world wide basis are often, 'consulted or published wave, wind and [current data are used. If environmental
data are totally lacking short term measurements are sometimes carried out
at the site or known data are
extra-polated
From the environmental data anum-ber of sea conditions with respect to wind, waves and current are selected
under which the tests will be carried out. At this stage experience gained from previous tests on single point mooring terminals or from experience gained with existing, similar
installa-tions is effective in reducing the
num-ber of different sea conditions possible
to a level which is acceptable: frOm the
point of View of limiting the number of tests while still remaining sufficient
to gain results representative: of the
particular systemin-that location. Besides information on the environ-mental conditions, the following
charac-teristics of the single point mooring must be known:
For instance for a CALM type system:
Buoy : dimension, weight,
centre of gravity, posi-tion of connecting point of bow hawser
Anchor chains rmumber, length, weight
per unit length, break-ing strength, elastic limit and elongation,, connecting point to
buoy
and pre-tensionBow hawser : length, weight per unit length, load Vexsts-elon-gation curve
Tankers moored to s.p.m.: size of tan ket(s), principal di-mensions
Loading conditions: transverse stabili-ty, period, of' roll,
lon-gitudinal Weight distri-bution, position of
bow
hawser connecting points
TEST PROGRAM
When the environmental conditions and the configuration of the terminal are known, the test program may be set up. Generally a limited selection of envi-ronmental conditions to be tested is made from the wide range of conditions
which may occur at the location. The selection is usually as follows: - For survival tests extreme
environ-mental conditions are chosen which have a probability of occurrence of
J.A. PINKSTER AND G.F.M. REMERY
681
once in 50 or 100 years. These
condi-tions are usually. with high winds,
waVesand current from the same
direc-tion.
- For tests in operating conditions with a tanker moored to the buoy, environ-mental conditions are chosen with a probability of occurrence of 1 to 10% or those conditions utder which it is expected that it will be possible to carry out operations or be able to remain moored to the terminal. Often those conditions will be selected which, from experience, are known to give high forces due for instance to the relative directions of wind, wave
and current.
- For tests under moderate conditions with the buoy occupied or unoccupied,
conditions are chosen which have a probability of occurrence in the region
of 50%.
The number of different sea states is
generally as follows:
Survival tests 'with buoy unoccupied: 1 to 3
Operational tests with a tanker moored to the buoy:.
3 to 6
Tests in moderate conditions:
1
The 'sequence of tests is often as follows:
One test in survival conditions and two
or three under operating conditions.
From the results of these tests it may be concluded that some characteris-tics of the system need to be altered for instance, the pre-tension
in
anchor .chains, length of bow hawser,arrange-ment of underbuoy hoses etc. The first tests would then be followed by two or three tests in which the effect of the alterations are checked. This part of
the program, consists of, as it were,
quick look tests and preliminary
optimi-zation tests. After the first part, a series of tests
Are
carried out underoperating conditions to investigate the influence on the behaviour and loads of
the following parameters:
- sea conditions with respect to wave
height and direction and. current and
wind speed and direction
loading condition tanker
underbuoy hose arrangement
etc.
These tests form the bulk of the program and may number from 10 to 30 tests..
Generally not all possible combinations
of parameter variations are tested,
however. After this part of the program, a number oftests are usually devoted to the optimization of some specific ele-ments in the system. These tests would
THE ROLE OF MODEL TESTS IN THE DESIGN OF SINGLE POINT
MOORING TERMINALS OTC 2212
Isually be carried out under both sur-,ival and operating conditions. The lumber of tests in this part would amount to 2 - 6 tests.
The above brief review gives an
outline of a possible test program. The following parts will discuss the actual information required and the procedures involved.
CHOICE OF SCALE
The choice of the model scale depends on a number of factors, the most important of which are:
water depth: each basin has a maximum
water depth.
accuracy of results: the larger the scale factor, the smaller the models, the lower the forces in the model and the accuracy with which for instance, pre-ten-sions may be adjusted. capability of generating the required
wave height and period at a particular scale in the basin. VM ,Vp = g ,gm p
1m'1p
= Assuming thatln
and that = where V it follows that: 12 =/E
vm 1m V m and = -E = ic-aT 1tm
_E
VpThe scale factor for weight and force becomes:
where
_E
xa3 FmA = ratio between specific gravity
of sea water at the
s.p.m.-location and the fresh water in the model basin
The scale factor for frequency becomes: a velocity in the model or prototype acceleration of gravity in model or prototype a characteristic length in model or prototype
a= a
1.rta = linear scale factor
= scale factor
of speed
= scale factor for
time
m
where w = frequency in radians/sec. or cycles/sec.
For tests in wind, waves and current it is normal practice at the NSMB to use scale factors ranging between 50 and 70. This range of scale factors allows accu-rate adjustment of such quantities as pre-tension in anchor chains, wave heights and current speeds etc. and assures model force and motion levels which may be accurately measured and
recorded.
SIMULATION OF ENVIRONMENTAL CONDITIONS Application of Froude's law of simi-litude results in the following scaling for the environmental conditions:
Waves:
For a given significant wave height -dw1/3 and mean period T the corresponding
values in the model are: -C1/3 and
--f-a
ATt
Current:
If the current velocity in reality equals
V , thus the speed in the models equals: cp
Taking the above into account a scale factor a for the model tests is chosen. This means that if the linear scale factor is a, all full scale linear dimensions will be reduced accordingly. What are, however, the scale factors for weights, period of roll, inertia,
elasticity and all other quantities of importance? This depends on the princi-ple of similitude between prototype and
model which is to be adhered to. This,
in turn, is dependent on the phenomena which determine the dynamic behaviour of the prototype and of the model. In reality, the dynamic behaviour of bodies
located in or near the water surface are dominated by forces due to the action of waves and forces due to the inertia of the body. If the body is far removed from the water surface the motions are dominated by friction forces and inertia, The law of similitude between prototype and model for the case that the behav-ior is dominated by the action of waves and the inertia of the body has been
formulated by William Froude and hence is known as Froude's law. This states that for dynamic similitude the follow-ing condition must be satisfied:
known as the energy spectrum since the energy present in the waves is propor-tional to the square of the wave ampli-tude. The spectral density of waves in reality has been determined from full scale wave height records. From large numbers of measurements various inves-tigations have deduced formulae Which give the value of S(w) if the signi-wave height tw1/3 and mean period T
are known. One of these formulations
is given below: -5 -Bw
S(w) = Aw
e 7.-4 where.: A = 172.8tw1/32
T B = 691.0 i7-4This particular formulation is of
the Pierson-Moskowitz type which is applicable to fully developed seas.
Other formulations have been given
among others, by Darbyshire,
Roll-Fischer, Bretschneider and Pierson Neuman and James. The choice of the
spectral density formulation to be
used for a particular test depends to a large extent on the location of the
prototype. For most investigations
where little is known concerning the
local conditions except the significant
wave height and mean period, the
Pier-son-Moskowitz formulation is often
used. The waves used in the model basin are generally long crested. This means there is no directional scatter in the waves. This is not the case in reality where waves of a particular frequency
may be progressing in a range of
direc-tions around some mean. This is
espe-cially true of wind driven waves. Long waves or smells generally tend to have
less directional scatter and to have
-longer crest lines: In model basin
long crested waves are usually gener-ated for the following reasons:
the directional properties of the waves at the proposed location are not known
- with uni-directional waves the In-fluence of variation in the wave
-direction on the behaviour of the s.p.m.-ship system are more prominent
and therefore give results which are more easily interpreted
In the model basins waves are adjusted by a method based on past experience
and a trial and error process. The
waves are measured by a resistance type wave probe placed in the position
V cp
/Tx
gind: the same speed scale as used for :he current speed applies.
Using these scale factors the
pre-?arations prior to the actual model :ests can be carried out- For the envi-:onmental conditions the preparations
mnsist of:
- adjustment of water depth - adjustment of current
- adjustment of wave generators - adjustment of wind
[these adjustments are carried out without
my models in the basin. later depth:
- the adjustment
of
the water depth in a basin is a straight-forward procedure requiring water to be added or let off. :urrent:- The adjustment of current entails
measurement of water speed in a number of pointiin the vicinity of the
posi-tion in which the models will be placed in the basin. For the case that tests are to be carried out in waves combined with current, the area over which the current is adjusted; must be large enough to ensure that the waves enter-ing the test area of the basin are not distOrted. An example of the horizontal and vertical current distribution
measured in the wave and current basin
is shown in Fig. 2. Erregular waves:
- After the current, the waves are
ad-justed. For open sea conditions the
waves are of an irregular nature.. This requires that for a realistic
simula-tion the model waves also must be irre-gular. Irregular seas are generally
characterized
by
their significantwave height and mean :period. The
sig-nificant wave height is defined as the
average of the one-third highest peak:
to trough values while the mean period corresponds to the mean time lapse between zero-up-crossings. The
signi-ficant wave height and mean period, however, give, only a rough description
of the sea state since the values give no indication as to the contribution of the various frequencies present in the irregular waves- This information
is given
by
the spectral density of the waves. The spectral densitySr(w)
of the waves is defined as follow:S (w) Aw = 15c a2
w-½w < w < w+kAw
The spectral density-Sc(w) is also
212 J.A. PINKSTER AND G.E.M. REMERY
THE ROLE OF MODEL TESTS IN THE DESIGN OF SINGLE POINT MOORING TERMINALS OTC 2212
2 PC°
S (W) = j
R (T) COS
WT dt7 C
An example of the spectral density of
the waves generated in a model basin is
given in Fig. 3. In this figure the
spectral density of the model waves is compared with the spectral density as
given by the Pierson-Moskowitz
formu-lation for the same significant wave
height and mean period. The agreement
is generally good except for the drop
off in the model spectrum at higher
frequencies. This is due to mechanical
limitation of the wave generator. In most cases this discrepancy is
accept-able since the distribution of the major position of the wave energy over
the wave frequencies is correct and
since, in general, the higher
frequen-cies have a negligible influence on the behaviour and loads in the systems
investigated. The failure to generate the very high frequency waves also
results in an increase of the mean period of the model waves, compared to
the required mean period. However, the fact that the spectral density of the
model waves matches the theoretical
formulation in the frequency range containing the major part of the total energy means that the mean period of waves within this frequency range is correct.
qind:
In the model basin, wind is usually
generated by means of fans placed some
distance away from the testing area. The wind speed is measured by means of an anemometer. The number, position and speed of the fans is such that the wind speed is reasonably homogeneous in the area where the models are to be located
The wind distribution is, however, not
up to wind tunnel standards since for instance the vertical distribution is not adjustable.
MODELS- OF S.P.M.''S AND TANKERS S.P.M's:
Models of s.p.m. terminals are
construct-ed of different types of materials:
wood, metal, synthetic foam, plastic etc. In practically all cases, components are
made as rigid as possible since the tests are aimed at the determination of rigid
body behaviour and not at the determina-tion of elastic behaviour of construcdetermina-tion elements. Centre of gravity of the models are determined and adjusted by means of
inclining tests in air while the mass distributions are checked by means of pendulum tests.
The model anchor chains for the buoy are
made to the correct length and weight.
The elastic stretch of the model chains
is smaller than is the case in reality.
To this end a small coil spring
compen-sating the lack of elastic stretch is
added. This method insures that both the
catenary characteristics and the elastic
properties of the chains are simulated
correctly. Tankers:
The models of tankers are generally
con-structed of wood. They are fitted with deck and superstructure. The longitudina3
weight distribution (mass moment of
inertia for pitch and yaw) is adjusted in air using the principle of the phys-ical pendulum. The transverse stability is adjusted by means of inclining tests. The adjustment of the natural period of
roll completes the preparations of the
ship model. In most cases stock models may be used and are available.
The bow hawsers of tankers moored to
single point mooring terminals are in
reality made of synthetic fibres which
have a distinctly non-linear load elonga-tion characteristic.
For the model tests the bow hawser gener-ally consists of a thin steel wire
attached to a system of springs which
provide the elasticity. The spring
pack-age consists of successively stronger springs mounted in series. Each spring
is fitted with a system which limits the stretch. As the load in the hawser is increased, the weakest spring first
reaches its stretch limit after which the stiffness of the hawser increases. This
procedure repeats itself as the second
weakest spring reaches its stretch limit. In this way the non-linear elastic
characteristics of bow hawsers may be closely reproduced. In Fig. 4 the elastic characteristics of a model hawser are compared with the full scale values. in the basin where the single point
mooring is to be tested. From the record of the irregular wave height measured in this point, the spectral density is computed in the following way:
If the wave height record is c(t), the auto-correlation function
R (T)
is cal-culated from:R
1T
c(T) = liM ,y, f
ot).0t+T) dt
oThe spectral density S(w) is obtained by Fourier transformation of the
nderbuoy hoses, floating hoses:
n some test programs, models of
under-luoy hoses or floating hoses have to be
zed. These hoses in reality consist of
.trings of large bore flexible hoses,
ach string of hoses consisting of dements with lengths of 30 - 40 ft.
mcdted together. The bore of these hoses
aries between 12 and 24 inches in real-ty. A hose element consists of a flex-ble middle section made of steel coils
aibedded in rubber and rigid end section :riding in a flange. Models of such hoses Lre made in a manner similar to reality ind consist of coil springs covered with .atex. The extremities of each model ?lement ending in a rigid part with a flange to which the next section may be :onnected. In model hoses the following )roperties may be reproduced: length, liameter, underwater weight and bending ;tiffness. In Fig. 5 the bending stiff-less of a model hose is compared with full scale data for a 24" submarine hose. then modelling underbuoy hoses, addition-xl items such as buoyancy tanks, beads Ind tie wires etc. are also reproduced )n scale with the appropriate nett
)uoyancy and elasticity. A complete set-ip showing a CALM and SALM single buoy mooring fitted with chains and underbuoy loses is shown in Fig. 6. In Fig. 7 a lumber of different types of s.p.m.'s :ested at NSMB are shown.
4EASUREMENTS
Measurements during model tests with
single point mooring terminals may
in-Forces in anchor chains and bow haw-sers. These are measured by means of transducers fitted in the appropriate
lines (see Fig. 8).
Motions of the buoy. These may include
surge, sway, heave, pitch and roll.
The linear motions are measured by means of a light pantograph system
(see Fig. 9) or a system of mutually
perpendicular thin wires connected to the top of the buoy and running to
fixed potentiometers.
The roll and pitch motions are measured by means of buoy-mounted potentiometers connected to a vertical taut wire which is used as a reference. The tension in the wire is held constant so that the buoy motions are influenced as little as possible. A new method of measuring linear buoy motions consists of a point light source fitted to the buoy and an optical tracking system which is homed on the point light source. In this way motions are measured without
applying external forces to the buoy.
-
Axial forces and bending moments in underbuoy and floating hoses. These are measured by means of transducers whichhave been constructed so that they may be fitted at the points where hose
elements are flanged together. The length of the transducers is such that they correspond with the length of the rigid parts of the actual hoses. In this way the discontinuities in the curvature of the hoses are retained
(see Fig. 8).
- Motions of the tanker are measured by means of pantograph systems and gyro-scopes (see Fig. 9). When the horizon-tal motions of the vessel become large,
they may be measured by means of a remote tracking system based on laser
beams.
TEST PROCEDURE
After all transducers have been cal-ibrated the model of the s.p.m. is placed in the basin and the pre-tension in the anchor chains is adjusted. Tests in ir-regular waves, wind and current are carried out according to the following
procedure:
The static values of forces and mo-tions are recorded in still water (no
waves, current and wind).
The current is turned on when the speed has stabilized the values of
the forces and motions are recorded.
The wind is turned on and when the system has again stabilized the forces
due to wind and current are recorded.
The wave generators are put into oper-ation. The waves are generated for a period of time corresponding to 70 minutes in reality. For the first 35 minutes no measurements are carried out since the starting-up phenomena may influence the results. Measure-ments are carried out during the
second 35 minutes of the 70 minutes
period. The 35 minute test period is sufficiently long for phenomena with wave frequency to be considered
sta-tionary. As will be discussed later,
this test period may be too short when considering low frequency pheno-mena, sometimes observed in the
hori-zontal motions of tankers moored to
s.p.m.'s.
RECORDINGS AND ANALYSIS OF RESULTS
Signals are recorded by one or more
13 channel magnetic tape recorders and/or
one or more 24 channel Ultra Violet paper
strip chart recorders depending on the number of signals to be measured.
Signals recorded on U.V. paper strip J.A. PINKSTER AND G.F.M. REmERY
THE ROLE OF MODEL TESTS IN THE DESIGN OF SINGLE POINT MOORING TERMINALS OTC 2212
wave train with the same spectral
densi-ty, all averages connected with the
measured signals would be the same. This
is, however, not true for the maximum
value of a signal. If for instance, the test duration is increased, the probabi-lity that a signal may reach an even higher maximum value increases also. On the other hand, if the test is repeated
in another wave train with the same spectral density but with the same dura-tion, then a different maximum value will be found also. The problem is to know the
behaviour of the extreme value of which only one is found for each measured sig-nal from each test. What we are in fact
seeking is the distribution of the ex-treme values or the probability of
occur-rence of some extreme value. The proce-dure by means of which distribution
functions for extremes may be determined
from the results of model tests is given
in (11). Briefly the procedure.involves_
the determination of the ratio between
the maximum value and root-mean square
value of a signal for all tests. These non-dimensional maximum values are used to construct the required distribution function of extremes which is valid for test length of 35 minutes. Based on this distribution functions estimates can be made of the extreme values with arbitrary
probability of exceedance for test pe-riods greater than 35 minutes.
Besides records of forces and mo-tions, visual behaviour of the tanker
and s.p.m. is recorded by means of film
either taken at model speed i.e. pro-jecting at the same number of frames/sec.
as the film was made at or with a high
speed camera at a rate of
IE
times theprojection speed. In this case the
pro-jected film will show the motions in real time. Records of the motions of
underbuoy hoses etc. are made by means
of underwater television equipment. ACCURACY OF THE RESULTS
For a given set of model and envi-ronmental conditions, errors,
uncertain-ties and inaccuracies in the results of tests come from the following sources:
the duration of the test scale effects
the sensitivity of the measuring de-vices
errors made in reading off values on
the U.V. paper charts
errors introduced by sampling and
digitizing signals recorded on magnetic tape.
iart are used for quick-look and check-1g purposes. From these recordings
Lx mum and minimum values are read off.
gnals recorded on magnetic tape are
.mpled at a rate of up to 32 samples second by computer. These values are .gitized and stored for further
analy-s.
For signals recorded during tests
irregular waves the normal statistical lalysis consists of determining the
alowing quantities:
mean value
root-mean square value maximum value
minimum value
significant value: mean value of the one-third highest peak to trough values
significant positive value: mean value
of the one-third highest zero to peak
values
significant negative value: mean value
of the one-third highest zero to trough
values
required the following characteristics
in also be determined:
distribution function of all digitized
values
distribution function of peak values distribution function of trough values distribution function of peak to
trough values spectral density response functions
le following additional treatment of bgnals may also be carried out:
filtering
combination of signals
As can be seen from the above, one
bgnal measured during one test can al-. ady yield a large amount of data. Al-lough all these quantities describe the . .haviour of a signal, the amount of data
too wieldy when it comes to using such
.sults for design purposes. In many lses the designer only requires a reli-31e value for the extreme of a particu-ir signal on which he may base the imensions of a particular construction 1ement. One would be tempted in such ise to use the maximum value recorded iring a particular test. This would,'
wever, be incorrect since the maximum
lime of a particular signal is a statis-ically unreliable quantity.
Model tests are carried out suffi-iently long for the process to become tationary ergotic. This means that if ae length of the test had been increased r if the test had been carried out in a
irregular with sharp edges. This means
that the points of separation of the air flovi are more or less fixed and the same
for model and prototype and that the scale effects will be small. They are estimated to be in the order of 0 - 10%.
Wave forces on the single point mooring
terminal:
If, the s.p.m. is constructed as a
cylin-drical body, an Impression of the impor-tance of frictional effects in the wave forces in reality may be gained from Fig. 10, taken from (1). This figure gives an indicatioh of Whether friction effects will play an important part based on the values of ca/a and ka for
the s.p.m. in question
where.: k = wave number
Ca = wave amplitude
a. = radius of the s.p.m. body If for instance it is required to know
whether frictional effects have, played
a part in results of tests on a 12.00 m
diameter buoy tested in. 8 second waves of 2.00 m amplitude,- then -this may be
checked. as follows: For 8 segond waves:
47r2 = 0.063 g
8.g
=.2 m Ca a = 6 mc a/a,=
0.33 , ka'= 0.38From Fig. 19 it is seen that the point
ka, c./a
is
in the region where inertiaeffects are dominant:in.the wave. forces. In this case it means that although there may be scale effect in the friction
forces in the model, these will not in-fluence the total hydrodynamic force to
any appreciable extent.
Current forces on the single point moor-ing terminal:
If the s.p,m. consists- of a .flat buoy,
the current flow around the buoy is three-dimensional, flowing under as well as around the buoy. That part of the flow which passes under the buoy, will
encounter.sharp corners which will re-sult in flow, separation in the model as well as in reality. This means that
ge-nerally the flow characteristics around such bodies match quite well with reality and consequently, scale effects due to friction will be small. They are esti-mated to be in the region of .0 - 10%.
If the buoy is of the slender, vertical
cylinder type, or if.parts of the con-struction consist of slender. elements, the flow around sudh- elementswill be of Duration of tests:
If the. test has been carried out for a
sufficient length of time, then the
processes involved have' become
station,-ary. Tests repeated under the same con-ditions should then give the same re-sults. Normally, using a standard test period of 35 minutes all mean values
(mean, root-mean square and significant
values, distribution) will reproduce within one or two-percent Maximum val-ues may, however, differ as MuCh"as
20-30%.. Depending on.the terminal in
ques-tion and the sea States at that locaques-tion, reproducability maybe worse with appre-ciable shift in mean values and variation
of 100% or more in- maximum values. This
phenomena ismainly due to large ampli-tude low frequency horizontal motions of the tanker which may occur in some sea
states. The-nature of the phenomena in-volved will be discussed furtheron in this-paper. Such low frequency motions
will not become, stationary within the
standard testing time of 35 minutes. If this is the case, a test may be carried
out for longer periods of time. Scale effects:
'Tests are carried out according to
Froude's law of similitude. This means that scale effects will occur in pheno-mena mainly dependent on friction effects
since these are dependent on equality of
the Reynolds number.
All signals measured during tests in waves, wind and current are to some ex-tent influenced by friction effects. In the following a brief review of the mag-nitude of these effects on various mo-tions and forces measured during::tests
with single point mooring terminals is
given.
Motions of the tankers:
Motions of tankers, induced by waves,
are for the greater part induced
by
hy-drodynamic Mass and inertia. forces. Scale effects: Negligible.
Current forces on tankers:
This depends on the direction of the current relative to the heading of the tanker. With current head-on the scale
effect is in. the order of 100%. The forces in thiscase are generally small,
however and not significant for the mooring problem. With current on the
beam, flow separation points are more orless
as they ate in reality. Scale ef-fects.: from 0 - 5 1.
Kind forces on tankers:
rhe above water shape of tankers is very
J.A. PINKSTER AND G.F.M. REMERY
8 THE ROLE OF MODEL TESTS IN THE DESIGN OF SINGLE POINT MOORING TERMINALS OTC 2212
--.11111111411111111111111 the two-dimensional type. In principle,
the model with these then show different points of flow separation to the full scale construction. In this case we must look to the local Reynolds
numberRe for model and prototype and determine the difference in the drag coefficients Cd' For circular cylinders
the drag coefficients are shown to a base of log Re in Fig. 11, taken from
(2). Model tests are practically always carried out at sub-critical Reynolds numbers. This means that the Cd values are always approximately equal to 1. Prototype Reynolds numbers are often in
the super-critical region. The Cd value in this region is, however, dependent on the roughness of the cylinders as shown
in Fig. 11. In the case of actual instal-lations, quite high roughness values may be reached due to marine growth
(bar-nacles etc.) and general deterioration
of the surface of the cylinders. This tends to increase the Cd values for the
i
prototype thus bringing t closer to the model values. In general, model values of the current forces will be somewhat higher with values being from 0 to 20% above those for the prototype.
Sensitivity of measuring devices:
Moments and forces: Bending moment and
force transducers are generally capable
of measuring forces with an accuracy
far in excess of the minimum accuracy required. They are accurate to approxi-mately 0.1%.
Motions: The accuracy of the measurement
of linear motions measured by means of
pantograph systems is dependent on the
frequency and amplitude of the motion, accuracy being less at higher
frequen-cies and smaller amplitudes. For the
normal range of frequencies with periods of 0.5 seconds to 3 seconds and ampli-tudes greater than a few millimeters in the model, accuracy of linear motions is approximately 1 to 5 %.
Angular motions measured by means of gyroscopes are accurate to approximately 0.1%.
Errors made in reading off U.V. paper charts:
2 - 5 cm. The error expressed as a
per-centage amounts to approximately 2 to
5%.
Errors induced by sampling and
digitiz-ing signals recorded on magnetic tape:
A signal recorded on magnetic tape as a continuous signal is sampled at a rate of up to 32 samples per second. Nor-mal sampling rate: 8/sec. A sample read off is digitized with an accuracy of
1/256 of the maximum band width avail-able for the signal. If the maximum value of a signal reaches the limit of the available band width then the accura-cy of each digitized sample equals
1
0.8% of the maximum value.
128
As may seen from the above brief review
in which some estimates of the uncer-tainties, inaccuracies and errors in-volved in model tests are given, the
major sources of uncertainty lies in the reproducability of the tests and in
scale effects due to friction. With
regard to the first of these, it is
noted that they are in most cases due to
low frequency phenomena. A longer test
period is required when this occurs. Friction effects have been estimated for many phenomena to be in the order of 0
to some percentage. In all cases the
model test results will be the same or higher than prototype results.
In general it is recommended to adhere to model test results without correcting
for possible scale effects.
EXAMPLES OF INFORMATION OBTAINED FROM MODEL TESTS
One of the most important results of model tests on s.p.m. systems is the
information that is obtained about the
general behaviour of a ship moored to a
single point in waves, wind and current. Ship motions:
In general the ship performs slow oscillating motions in the horizontal plane about a certain equilibrium posi-tion. This equilibrium position is deter-mined by the speed and direction of
cur-rent and wind and the height, period and direction of the waves. The equilibrium
position of the ship can be obtained from the mean forces which are exerted on the ship in a particular sea state and which
are dependent on the direction of waves, These are dependent on the width
of the trace of the signals in relation to the amplitude of the signal. The reading off error is in the order of
half the width of the trace which amountswind and current relative to the ship. to approximately 1 mm. With a signal - An estimate of the magnitude of the mean amplitude in the order of magnitude of forces can be obtained from (3).
:n general the mooring loads are largest
then waves and/or wind are at more or
.ess right angles to the current. A
:ypical equilibrium position of the ship
.n those conditions is shown in Fig. 12.
:f the current is strong (e.g. 3 knots)
Lnd the vessel is loaded then this
equi-.ibrium position is very stable which
leans that the slow oscillating motions
7elative to the equilibrium position are
nmall. This equilibrium position is not
rery sensitive to small changes in wave
'eight, wind or current speed. Since the
Lngle between the current and the ship's
:entre line can be considerable (100-200)
:he athwart ship's component of the
cur-:ent force on the ship is large, which
nay result in large mean forces in the
)OW hawser. Superimposed on these mean
forces are the oscillatory forces due
:0 wave induced buoy motions and tanker
notions. When the current speed decreases
to for instance 1.5 knots or the vessel
'raft decreases during the
un-Loading operation, then the equilibrium
position changes considerably. The
tan-cer takes an average position more in
Line with the bow hawser and the angle
petween the ship's centre line and the
:urrent may increase up to 450. In the
mme time the ships often swing about
:he equilibrium position. The amplitude
)f these slow oscillating swing motion
:an be considerable. The position of the
XYW hawser may vary more than 900
be-:ween the two extreme positions. The
rariation in the heading of the ship
Luring the swinging motion is shown in
'ig.
13. High bow hawser forces
general-.y occur when the ship has reached her
mtreme positions during the swinging
uytion. Often large hawser loads. also
)ccur when the horizontal motion of the
;hip's bow is largest. This is normally
Lear the average position of the ship
Luring the slow swinging motion. The
winging motion and consequently the
Lagnitude of the largest loads in the
pow hawser can be reduced by a reduction
Pf the length of the bow hawser.
[ow the mooring loads of the ballasted
dhip compare to the mooring loads of
the loaded vessel depends on to
many
Parameters with respect to sea
condi-.ions, sea direction, ship's size and
ype of s.p.m. system, to be able to
ve a general trend.
luoy motions:
..11 case a relatively small mooring buoy
s used (CALM or SALM system) the
mo-Acms of the buoy, when occupied by a
:anker are, except the vertical heave
Lotion, mainly dictated by the loads in
the bow hawser. From the measurement of
the buoy motions the minimum and
maxi-mum distances between the suspension
point bf the underwater hose of the
buoy
and the pipe line end manifold (PLEM)
can be determined. These data are
in-dispensible for a proper design of the
underwater hose system. The horizontal
motions of the buoy are normally largest
in extreme operational conditions when
the buoy is occupied by a tanker; the
vertical motions are largest in survival
conditions without a tanker moored to
the buoy. An example of the envelopes
of motion of the hose suspension point
of a CALM buoy in extreme conditions is
shown in Fig. 14.
Up to now a proper explanation for
all phenomena that occur with regard to
the behaviour of the system
tanker-single point mooring is not available.
A systematic analysis of all data
avail-able on this type of systems is
there-fore not yet possible. However, much
'effort is being put into this subject.
A short description of the main problem
of slowly varying motions is dealt with
briefly in the next section.
MATHEMATICAL DESCRIPTION OF
ENVIRONMEN-TAL FORCES
In order to increase the efficiency
in the design of s.p.m.'s methods of
cal-culation are being introduced with the
aim of establishing, at an early stage
in the design, the behaviour and loads
of the system. These methods of
calcula-tion involve on the one hand a
mathema-tical description of the important
characteristics of the s.p.m.-ship
sys-tem including non-linear restoring
for-ces and the inertia and damping of the
buoy and ship for various modes of
mo-tion and on the other hand a
mathemati-cal description of the environmental
forces acting on the elements of the
system.
Due to the non-linearities of the
system equations of motion are
inte-grated on a step by step basis using
small increments of time. As has been
described before, the environmental
forces are due to:
wind
waves
current
Wind forces:
The formulations for the lateral and
longitudinal wind forces and yawing
moment are of the following type:
J.A.
PINKSTERAND G.F.M.
REMERYTHE ROLE: OF MODEL TESTS IN THE DESIGN OF SINGLE POINT MOORING TERMINALS OTC 2212
2
Fw
= hp
V A C
w w dwIn this formulation the coefficient Cdw is determined from model tests in wino tunnels for different. angles between. the heading angle of the vessel and wind (3). Current forces:
The formulation for this type of force is similar to those for the wind forces:
F = 1/213 VAC
c
c
cdc
The value of the current force, coeffi-cient Cric is determined .by oblique towing rests or
by
tests in current for different angles between vessel andcufrent,(3). Both wind and current for-ces are Constant values for a constant speed of wind and current..
Wave forces:
The forces due to waves may be split-up
into two components
wave forces and moments which are pro-portional
to
the wave height (1st or-der wave forces)wave forces and moments which are pr&-portional to the square of the wave height (2nd. order wave forces or wave drifting forces).
The 1st and 2nd order wave forces in re-gular waves may in principle be
calcu-lated from the pressure distribution on the hull usingBernouilli's equation:
a(
p= -pgz -
pa -
kplvl.v
where cP is the 1st order velocity
poten-tial. The 1st order wave force is found
by integrating the pressures acting on
the hull whereby the 2nd order contri-butions of: the pressure components are neglected..The mean wave drifting force
in regular waves is found by integrating all second order pressure contributions. In determining the 1st order wave force
only the components pgz and acp
are taken into account..
All
three atcomponents of the pressure contribute to the mean Wave drifting force.
1st order wave forces:
The first order wave forces induce ship
and
buoy
motions .with wave frequency. For ship S the, motions due to these for-ces may be calculated from first prin-ciples using strip-theory (4) or, in the caseof
Ships at zero forward speed,a
method based
on
three-dimensionalpoten-tial theory. (5').
Luoy motions may be calculated using the
potential theory method
or,
in the case:the buoy is -slender or composed of slender elements which are small in
re-lation to the wave lengths,
by:a
finite element theory based on the, relative motion principle (6).2nd order wave forces:
In irregular.waves the height of the incoming waves is a slowly varying quan-tity. Since the wave drifting force
is.
proportional td the square Of the wave height, this Will also show slowlyVary-ing or low frequencTcomponents (see
Fig. 15). As may be seen from this figu-re, peaks in the wave drifting force are
associated with the occurrence ofgroups
of higher waves. In (7) it was shown that If the period of the wave groups
coincides with the natural period of the
horizontal, motions of the moored. vessel,:
large amplitude Motions- can occur. In principle the components of the 'wave drifting force in irregular, waves have frequencies from 0 to infinity, however, the :main components are concentrated between the frequency O'and the frequen-cy of the waves from Which the 'force
originates,
Moored ships generally Constitute mass-spring systems with natural periods for the horizontal.motions in the Order of magnitude of- 50 to 500 seconds. 'These frequencies are outside of the wave' frequencies and in the range of the frequencies of the drifting forces. Damping in the horizontal motions is generally low. These two characteristics combined with the frequencies of the slowly varying wave drifting forde can produce the large amplitude low fte-. quency motions in moored vessels..
These motions may
in
SOtecasescomplete-ly dominate the loads imposed on the system as is Sh0wn
in
Fig. 16,in
which results of the yawing motion of the tan-ker and force in the bbw hawser areShown. As may be seen, the force-fluctu-ation due to the ship and
buoy
Motionwith wave frequendy are small compared with the low frequency force and motion
oscillations.
CALCULATION OF WAVE DRIFTING FORCE
Under certain conditions with the
ship head-on,to Waves, it is possible to calculate the mean wave, drifting force in regular waves from. strip-theory -(8). In the general case with waves coming from arbitraryditectiOns,..cal-culations based on'three,dimensional potential theory,may be used (5).
UP to
the present the mean- wave drifting force in regular waves has usually been ob-tained from model testsThe equation for the mean wave drifting
fol-for these effects. This conclusion has been based on the undertainties which exist concerning the drag coefficients of the prototype. A brief review of the methods of analysis has shown how
re-sults may be used for design purposes
provided that the statistics of extremes
is applied. From the brief review of the
phenomena which determine the behaviour of moored vessels, it has been shown
that methods developed to calculate mo-tions and forces in s.p.m.-ship systems should include the influence of the low frequency drifting force in irregular waves. Methods to calculate these forces
are, however, not yet fully enough
de-veloped to yield the consistent results necessary for design purposes. At the present time, model tests are the most
suitable means to obtain quantitative results concerning the behaviour and
loads of Single point mooring terminals.
NOMENCLATURE
: linear scaling factor
: velocity
: acceleration of gravity : characteristic length : force
: ratio between specific gra-vity of salt water and
fresh water
: frequency
: mean period
: significant wave height
: spectral density of
irregu-lar waves
: small frequency interval : coefficient in theoretical
wave spectrum tormulation
: auto-correlation function : time shift : test duration : wave height : wave number : wave amplitude : radius of a cylindrical body : Reynolds number : drag coefficient
: specific gravity of salt
water
: specific gravity of air : characteristic area for
current force
: spectral density of the drifting force in irregular waves : velocity potential a 1 w,p T w1/3 S (w) Aw A,B Ca a Re Cd lowing form: 17(w) = kpg L R (w)a2
where R(w) is called the wave drifting force coefficient obtainable from calcu-lations or model tests. Based on certain assumptions the mean value and the spec-tral density of the oscillating part of the low frequency wave drifting force in irregular waves may be calculated using
equations of the following type: Mean value: co
f =
pgf
S (w) R2(w) dw Spectral density: Sf(p) = 2p2g2f
srmsc(w+p)R4(w+u/2)dw
oThese expressions are derived using
ba-sic assumptions given in (9 ).
In the case of a rectangular barge moor-ed in head seas, the results obtainmoor-ed using the above equation4 have been
en-couraging (10).
Recent model tests have shown, however,
that with very large vessels moored in head seas, the mean wave drifting force in regular waves does not contain suffi-cient information to give an accurate
estimate of the low frequency behaviour.
This seems to be due, in part, to the fact that the mean drifing force in regular waves does not take into account the distribution of the force over the length of the vessel. At present re-search into these effects is being car-ried out at the Netherlands Ship Model
Basin.
In calculation methods used for
deter-mining the behaviour of the
s.p.m.-ship system, most of the above described components of the environmental forces
have been included. Generally, however,
the low frequency wave drifting force is conspicuous through absence. From the examples given above it may, however, be concluded that inclusion of this force
is a necessary requirement for insight into the behaviour of ships moored to
s.p.m.'s. CONCLUSIONS
In the aforegoing, the steps
in-volved in carrying out model tests with single point mooring terminals have been reviewed. Based on estimates of the errors due to scale effects, it has been shown that generally the results of model tests should be used without correction
co a
692 . .
,proto.type
-thOdel-.:drag_
current
'-.force
Van OortsmerSsen, G.: "The'inter7,
action between :a vertical cylinder
..andregularwaves'"::PiOdeedinge'Sym-.
posiUM on Off
Hydrodynathics.-'
publication
No:I25.N.-S.M.:;Bage-hingen, 197-1;
FluiclDynamiO'brag".,
Published by the author,.. 1965
_ 3..Remevy,
,G;F:I.m,',andAran.-.0or,tmerssen,
-G'.:7The.reLein;-WaVe;.,Wind:'and
:FOkc07.5h,OfshOre.:StrUctuteearid.
their -role'lWthe'Designitihg
Sisteitts"4-0TC-paper-No.-:t741. OTC
,4,':-Flokstral C.:-
"ShipmotiOh..inregu7,-iarWaVes" unpublished repOrtythe
..
THE ROLE OF MODEL TESTS IN,THE'DESIGNi OF"ISINGLE=POINT-MOORING -TERMINALS OTC
2212
. ,
vertiOal
-dietance,'below.-In[P4tat*fiikcj'fdrd'
: IireSeure.
-
Nethe#linde_Ship Model
se:eih,Van. Portmerssen, G:: Some aspects of
..;.very large Offshore' Structlires".
Ninth Symposium on Naval
Hydrodyna-..
:mibe.:Paris 1972.
.6. nooft,"J=1).:."HydrOdynamic aspects
_ _Of Semi-Submersible Platforms".
Ph .b Thesis. Technical U. of Delft.
G.P.M. and Hermans, A.J.:
"The- SlOw Drift oscillations of a
M6Ored Object in Random Waves". OTC
Paper No..1500. OTC 1971,
Gerr.itsma, J: and Bedkdiman, N.:
"Ahilysis%of the resistance increase
in-Waves:of a Fist Cargo Ship".
Re-port No
334, LabOtatorium voor
Scheepsbouwkunde, Technical T. of
Delft.,1971.
9. HsU,.F:H. and Blenkarn', K.A.1
"Analysis of-peak-Mbbring'Farce
Caused by Slow Vessel Drift
,Oscilla-ti6ns in Random Seas". -OTC Paper No.
1159', arc 1970.
10.'Pinkster,
Frequency
Pheno-mena associated With Vessel e moored
at-Sea"
SPE paper No..V 4837. SPE
Spring Meeting Amsterdith 1974:
11. Remeryi'G.F.M.: "Model testing for
the design of off shore structures".
Proceedings Symposium on offshore
hydrodynamics. Publication No.
325,\ \ \
\
1\
%\\
`...,
/r\/
,....,"
I ,/
---./ -.... . .-,.....-\\\\NN\\\\\\\\\\-\\\NN\N\NN\ \\
\\\\\\\\\\\\\\\\\\\\\\\\\\\\\
EXPOSED LOCATION S.B.M. SPARFig. 1 - Examples of s.p.m. terminals.
":" , / .
/
. .., c\-\ C". \ N. \--. \\.N.\\\ \ ... \ N.\\ \\\\NN\
RIGID ARM MOORING
ARTICULATED MOORING TOWER SPAR BUOY
-
Er"
/
,
...\\\.\\\\"\\\\.\\\-\\\\\NANANA
\\ N \
\ \\ \ \ \ \ \AN \\ \\ \\N \\
CATENARY ANCHOR LEG MOORING
HORIZONTAL DISTRIBLIIT.IPN-.Rosit.ion buoy
- ,
r:-: 0 ,. 500'-: ' ..-15.00.:DISTANCE_ IN .LON.Q)JUDINAL. DIR:E-CT,If_.:t1IFT'TH.,,--;BAI.N^ i,tyrii
-'C'PERPEN[5:1COL:?tol.- .1..6 cuiRk6.14.90.0i'ECA-0.0-.:..:=
,
... . --.. ..--:.,,,,*4,-,,.:-,._...-..2,-,:i!,:...,... .
..
.Fig. .,,- Eiample o!' n current distribution ad,'.usted. model*bAsin.
sdale Ve.Iues. -'
,...,.,,
- Compri'son of :.pectral density of model waves
-0.75
600 40 20
2.5
ELONGATION in metres
Fig. 4 - Comparison of the load-elongation properties of a model bow hawser
and of an actual bow hawser.
Full scale values.
20 1
z.
MODEL PROTOTYPE
PROTOTYPE
2 x16" NYLON LINES LENGTH 40m
MODEL BENDING TEST
/
/
/
/
-______ 1 2290 lb. 12500 lb. ---1 i I I I i 10 20 30 DISTANCE in feetFig. 5 - Comparison of hose bending stiffness in model and prototype
;f4,71 ,'"74 ..,#.:*7.1". 27 t'32.4.. 41917 1r"
0
:c-
,' - ...orTm="1"!?rC4114k*":"' --t. '
Fig. 7 - Examples of
'.m. ' s tested at thèNS
,OV=,
-Fig...
8--
Transducers for themeasurement of hose and ...anchor chain toads..
Fig-
9 -
Pantograph systems for the measurement of linear.motions.
1.5
1.0
0.
CD0.2
0.1 1 C-)
0
U. DU'Ka
Fig. 10 - Wave forces on cylindrical bodies (Ref. 1).
k.= SAND-GRAIN SIZE
d= DIAMETER
7Viscous effects
become important
---T- a L
Line of maximum
wave steepness
_
_01
A% I ,2 I, A.I Gravitation
I effects
! become
1important
_
nl
/
= 9/10- .
INlemsonoursion...-2/10
21.1111111WriMOo
.4
kid =7/103
kid =4/103
k/ d=2/103
kid= 5/104
k/d= 0
k/d=
11111.11-111=
k/dMiketaiii
NI
NI 0/ A
=. A A . ,-,
A 234 5 6 6
1,10
C. REFig.
8 -
Transducers for the measurement of hose andanchor
chain loads. --k., -,
'+.4.. .. ' .,..=.-. 3a; .. :-17., r4 . -,7 I tr. ak -.;;; ' ... if '':,,z`'''''-'."-, -tJe..r.,"'"?,:yr 3 ''" ..-,,,, ,... ',tr,_ .14, "4.4.':- '''.."`4:42" 11;11+- ,":* _L.
inkkaP
0.2 0.1 a 10 5 RE
74- 11 - Influence of surface roughness on the drag coefficient of cylinders (Ref. 2).
I .
Viscous effects
become important
( )--a-- a L
Line of maximum
wave steepness
A'Gravitation
I effects
I become
I important
I_
ikid =7/103
kid=4/103
k/d= 2/103
k/d=5/104
k/d= 0
- II =
.1 Ilik..-" ...kid =2/102
=9/103
`1111-1111111.111,Ig.
kid1111111M1
irt
in4
2 34 5 6 Bin5
23 4 5 6
81(16 23 4 5 6 8
i0.25
0.50
0.75'Ka
Fig. 10 - Wave forces on cylindrical bodies (Ref. 1).
k.= SAND-GRAIN SIZE
d = DIAMETER
1.5 1.00.5
CD' . . :. ,.. .. , , . . .... ., .
),?.. r:Me.:nn rtisi Lion -tr.:1 cal, of n':.'?adecl,tarker in wind
woven
8n!
current. when il.nore:i. to O -s,r).01,,,
;;.}.
.':
. ' . .. CURRENT MOORING POINT -typical. 'OfWAVE
DIRECTION
2E0
-2
OPERATIONAC
\
-...,\
....\
SURVIVAL' -*N.
1 --..---- )Fig. 14 - Motions of the suspension point of the underbuoy hoses of a CALM buoy.
WAVE HEIGHT
SQUARE OF WAVE HEIGHT
time
Fig. 15 - Record of an irregular wave and the square of the wave height.
,-
--Yawing m6ti2ns and bow hawser loads typical
- .