ARCH1EF
Deift
Skìbsteknîsk La
ratorium
t
Danish Ship Research Laboratory
MEDDELELSE
APRIL 1980
BULLETIN NO. 45
PREDICTION OF WATER LEVEL MOTION AND
FORCES ACTING ON A DIVING BELL DURING
LAUNCHING THROUGH A MOONPOOL
BY
NIELS FL. MADSEN
Technische Hogeschoof
w
ADDRESS: HJORTEKRSVEJ 99 DK-2800 LYNGBV DANMARK
SKIBSTEKNISK
LABORATORIUM
Danish Ship Research Laboratory
PREDICTION OF WATER LEVEL MOTION AND
FORCES ACTING ON A DIVING BELL DURING
LAUNChING THROUGH A MOONPOOL.
by
Niels Fi. Madsen
nkcFo -oqesc -' -- t
NOMENCLATURE
ABSTRACT
INTRODUCTION 2
METHODS TO CONTROL THE BELL MOTION 3
The Bell Compensator 3
Subsurface Diving Gear 3
Bell Guided by Cursor 6
Moonpool Diving System 6
THE THEORITICAL MODEL 10
Equations of Motion for the Bell 11
Equilibrium of Liquid in a Moonpool 12 Solution of the Equations of Motion 17
The Computer Program 18
MODEL TESTS 19
Hydrodynamic Coefficients 19
Model Tests in Waves 26
NUMERICAL RESULTS 38
Water Level Motion in Fixed Moonpool 38
Influence of Winch Strategy 49
CONCLUSIONS . 57
REFERENCES 58
APPENDIX A. Data Sheets for Program Belirnoon
APPENDIX B. Post-Processing Time Histories
APPENDIX C. Example, Program INPUT/OUTPUT
a = Fourier components.
n
g = Acceleration of gravity.
h = Draught of moonpool.
h' = Equivalent length of added water column below moonpool.
k = Stiffness of hoist rope / winch.
m = Mass of diving bell.
p = Froude-Krylov pressure at bottom of moonpool.
t = Time.
u = Bell motion relative to ship.
y = Bell motion relative to earth.
w = Wave motion relative to earth.
y = Liquid motion at bell position relative to earth.
z = Ship motion relative to earth.
Ab = Projected area of bell perpendicular to the flow direction.
A = Choke area. c
A = Cross-sectional area of moonpool.
CD = Drag coefficient for bell.
C = Added mass coefficient for bell.
m
F = Hoist rope force.
Fa = Damping force from arbitrary damping device.
F = Damping force at bottom opening.
F = Restoring force. r
F = Wave force. w
H = Wave height (peak to peak).
Ç)
V = Volume of bell.
p = Damping coefficient for arbitrary damping device.
Y = Damping coefficient for damping at the bottom of the
moonpool.
= Natural frequency for bell oscillations.
= Natural frequency for moonpool oscillations.
= Frequency of n'th Fourier component.
4' = Phase angle of ntth Fourier component.
P = Density of water. d( )
dt
d2( ) 2 dtABSTRACT
This report describes a numerical method for the determination of forces acting on a tethered subsea unit such as a diving bell during launching. The launching or retrieving operation is assumed to take place either exposed to the open sea or through a moonpool.
The liquid motion in a moonpool with a bell in it is studied in detal, and a mathematícal model for the system is established. The bell
motion and wire force are investigated for a number of operating situ-ations and for different strategies for rope force control.
Model tests have been carried out in order to verify the mathematical model, and the hydrodynamic coefficients have been measured for models of three typical diving bells in tubes with different diameters.
1. INTRODUCTION
The ability to launch and retrieve diving bells safely in a rough seaway has become one of the important aspects of offshore activities. The safe
launching or retrieving depends on systems having the ability to withstand
the hydrodynamic forces on the bell caused by large, relative velocities and accelerations between the support vessel and the surface waves.
If the weight of the bell in water is too small compared to the hydrodynamic forces there is a risk of slack wire with subsequent jerk forces which may
lead to excessive vertical accelerations of the bell, collision between the subsea unit and the offshore vessel, or the hoist wire may even burst.
The report revíews briefly some existing design concepts which are intended to minimize the hydrodynamic forces or to prevent the bell from being exposed to excessive forces due to slack wire.
A theory has been developed for the prediction of water level motion in a
moonpool and the forces acting on a diving bell either situated ín a
moonpool or exposed to the open sea. A special attention has
been given to devices for control of the hoist rope force, and the theory is able to predict wire forces during the period of slack wire followed by a sudden jerk in the rope.
Model test were carried out in order to confirm the theory, and the hydro-dynamic coefficients have been measured for three models of diving bells, situated in tubes with different diameters. For one of the diving bells a comparison has been made with full-scale measurements.
2. METHODS TO CONTROL THE BELL MOTION
A variety of solutions has been suggested or employed in practice to minimize the bell motion and to minimize or eliminate the risk of slack in the hoisting wire.
For some of the systems, which are briefly outlined below, safety and / or the ability to dive under rough weather conditions can be further increased. Slack wire will not occur or the consequencies of slack wire
with subsequent large vertical bell accelerations will be less severe, if the hydraulic bell winch system is fitted with a device for maintaining a certain minimum tension, a relief valve to limit the maximum tension or a
device for maintaining constant wire force or if the equivalent spring stiffness of the hoist rope and winch is sufficiently small.
Safety also depends on the complexity of the system. As a general rule,
systems containing a minimum of moving parts submerged in salt water should be preferred.
The Bell Compensator
The bell compensator as described in Ref. (1) and roughly sketched in Fig.
i has been claimed to have the ability to eliminate the heave motion over
a total heave of 13 metres. The solution is, however, limited to the case
where the weight can be placed on the sea floor approximately vertically below the diver's work site.
Subsurface Diving Gear
The diving system of Fig. 2, known as Subsurface Diving Gear, Ref. (2), can be built into one of the columns of a semisubmersible or in the bottom of a mono-hull vessel. This system has the advance, that the bell does not pass the air/sea interface at all.
Cc2)5.TA%-)T TL5 to
V)C44
"-J-4cST Rc'PE
'.' I -Ca/
,-otr
C_41C.L) tEL* F4 L
\'E_l C H -rFigure 1. The Bell Compensator. A system for compensating the heave motion of the bell.
Figure 2. Subsurface Diving Gear. The diving bell does not pass
the surface at all.
Bell Guided by Cursor
Fig. 3 shows a system where the bell is trapped in a cursor (3). The
bell is exposed to the open sea, but the bell is enforced to follow the motion of the cursor.
Noonpool Diving Systems
The conventional moonpool approach as shown in Fig. 4 has the advantage that the outside waves will appear in a filtered version, the short waves
being filtered away more effectively than the larger ones, so the motion left in the moonpool is relatively slow. Furthermore, waves with large
amplitudes are damped more efficiently than small waves since the damping is nonlinear. See Fig. 9.
However, the natural frequency of the liquid oscillating vertically in the moonpoon will often coincide with frequencies contained in wave spectra met in the North Sea.
Within draughts of 5 - 15 metres resonance occurs at sea-states from Force 3 to Force 6, and the water motion may be amplified by a factor
3 - 5 or even more.
For this reason the designer will often prefer to introduce a device which has the ability to increase damping such as choke decks or flanges
as shown in Fig. 5, an airtight casing above the moonpool as described in Ref. (4) and Fig. 6, or the arrangement shown in Fig. 7, Ref. (5), in which damping is provided by horzontal baffles and the perforated wall.
In addition, the buoyancy of the bell is decreased by use of an air injection system.
Finally, Fig. 8, Ref. (6) shows a moonpool arrangement where the bell is guided by a cursor. After the bell and cursor assembly has reached its
lower position the bottom door is opened and the bell can then be released from the cursor. At this moment the pumping effect of the water column in
the moonpool caused by the heave motion of the ship will only be small since the roof of the cursor nearly fills the cross-section of the
Figure 4. The moonpool approach.
¿2
)
Figure 5. Moonpool fitted with choke decks for damping the liquid motion. The moonpool has been installed in a leg of a Semisubmersible Support Vessel.
Figure 7.
,a. r
r t
4-jr
C,A.! L)(i
Figure 6. Moonpool with an airtight casing.
t L L) c r C.- -.
£...
\' I T -4' j_T
E_LT E Z. C. . E.
.LE r--E5.
Moonpool with damping chamber and a system for air injection.
7.0 f- ,.o
5.0
3.0 £ 2.0 L Figure 9. -I- 1-c.'
-.Moonpool wave to outside wave versus wave frequency showing the effect of wave height and draught of the moonpool. The height of the moonpool wave is
calcu-lated by use of the numerical procedure described in this report. The figure also shows frequencies met in the North Sea for different significant wave heights.
Figure 8. Moonpool with cursor.
o
0.6
4.0 4. E. 2.o3. THE THEORETICAL MODEL
The wave motion and the ship motion are assumed to be known
as
determi-nistic functions of time.
We only consider the vertical components of
the wave motion w(t) and the ship motion z(t) at the location of the
moonpool.
So, the motions of the moonpool and the point of suspension
of the hoist rope are given by z(t).
The system consists of a tethered unit which may either be situated in
the open sea or in a moonpool, or the system may consist of a moonpool,
only.
For the case where a tethered unit is included it is possible to
study the bell response on different devices built into the hoisting winch.
The system bell - moonpool is described mathematically by the two degrees
of freedom, bell motion and water level motion in the moonpool.
The bell is restricted to
be fully submerged for two reasons:
- It is not expected that slaiuining alone may cause
a slack wire when the bell is handled through a
moonpool since the high frequent wave components
are filtered away.
- For a partly submerged bell the prediction of
hydro-dynamic coefficients including a coefficient for
slam-ming is believed to be highly inaccurate.
However, the effect of slamming could, of course, be included in the
equations of motion for the bell.
For a further discussion of the problem of penetrating through the splash
zone, see Ref. (7).
The bell is treated as a point mass with concentrated forces acting on it. The wire force must keep equilibrium with acceleration forces, gravity forces, buoyancy forces and hydrodynamic forces.
According to Morison's formula, the hydrodynamic forces acting on the bell can be calculated by:
FH = pV (1+C ) -
pv C ii ApAb C
('Cr-r)I-7I
m m
where y and y are the liquid motion and bell motion, respectively. p is the density of water, V is the volume of the bell and Ab is the projected area perpendir'iilar to the flow. The virtual mass coefficient and drag coefficient ar denoted by Cm and CD, respectively.
For the case where the bell is situated in a moonpool, y is recognized as the water level motion, and Cm and CD are values which are valid for the bell in the moonpool.
Application of Newton's second law leads to the following expression for the force in the hoist rope:
F = nrJ + mg-PVg - pv (1+C) + V Cm i + pAb CD
(VY
HT-I
where g is the acceleration of gravity and m is the mass of the bell.
The bell motion and the force in the hoist rope depend to a large extent on the response of the hoist system. A number of standard strategies for
rope force control has been included in the computer program, and any new device may easily be added. At present, the following possibilities exists:
- Inelastic winch / wire. The bell is subjected to a given
motion u(t) relative to the ship. The bell motion is de-termined by:
- Elastic winch / wire. The bell motion is determined
by the wire force:
F = k(z + u -
y)
where k is the combined stiffness of the wire and winch. The program includes the possibility to simulate slack wire by putting F equal to zero in case that the
right-hand side of equation (4) is negative.
- Ability to maintain a certain minimum tension in the hoist
rope. Such a device is introduced by adding a value to u
in eq. (4) which gives the specified tension.
- Relief valve in the hydraulic system. The device is in-troduced by subtracting the value from u in eq. (4) which
gives the specified tension in the rope.
- Constant tension winch. The bell motion is determined by
the constant tention T:
F=T
Equilibrium of Liquid in a Moonpool
The moonpool geometry is shown in Fig. 10. The moonpool has a constant
cross-sectional area At over the draught h. The moonpool may be fitted with choke decks or beams welded to the wall in a direction normal to
the flow. The effects of such damping devices are included by adding an
equivalent damping of the water level motion, and the hydrodynamic
coeffi-cients for the bell must be adjusted to be valid for themodified moonpool.
The liquid in the moonpool consists of three parts:
- the constant part determined by A and h minus the
volume occupied by the bell,
- the variable part determined by At and the water level motion y in the moonpool,
- the added mass determined by A and an equivalent
length h' of an imaginary water column below the bottom opening.
Fukuda (8) suggests the formula:
which is included in the computer program.
The momentum for the above three contributions becomes:
P = pA
(h + h' +y) S
-
pViThe last term is explained by the fact, that the momentum in the surrounding liquid caused by the bell moving upwards with the velocity is equivalent
to that of the same volume of water moving downwards with the same velocity.
The equilibrium equations are derived by using:
= kall external forces,
or (h + h') +
pA2 + pAy
- pV =4 L
-w I I-L----J
Figure 10. The moonpool geometry.
y
h
The external forces acting on the water column in the moonpool are:
- Restoring force acting at the bottom opening
(10) Fr = -ypg A
- Wave forces. The Froude - Krylov hypotheses is assumed,
i.e. the pressure p at the bottom opening is equal to the dynamic wave pressure and the excitation force from the waves then becomes:
F =pA
w t
The dynamic pressure is evaluated by Fourier decomposing the wave motion:
w(t) = Z a cos ( t - 4' )
n n n
n
where a, and 4, are Fourier amplitudes, frequencies
and phases, respectively.
When the sea is deeper than a half wave length, the dyna-mic pressure becomes: 2
n
p(t) = pg
ae -
(h - z) cos ( t - 4, )n n
n
- Damping force due to energy loss at the bottom opening. The
bottom opening is regarded as a tube which has an abrupt enlargement, see Fig. 11, and the flow is assumed to be stationary. When the flow runs out of the moonpool the velocity is approximately uniform over the cross-section of the moonpool. At the abrupt enlargement, the flow forms
turbulent eddies in the corner which result in an energy loss.
Sufficiently far away downstream from the enlargement, the velocity will again be uniform.
/
p-tcQ
L) Q L.-,.- ,
ec'rrc-/
W L_L.
cr
"JE-Figure 11. Idealization of the flow at the bottom opening of the moonpool.
Figure 12. Proposed damping coefficients for the bottom opening.
o
The radial accelerations over the horizontal surface (the bottom surface of the ship) are very small, a fact which leads to the experimentally supported evidence, that the pressure at the horizontal surface is equal to
that found in the bottom opening.
Using the above assumptions, the momentum equation for a
steady flow, the equations for continuity and energy conservasion for a constant density flow and letting the larger diameter go to infinity, the total force becomes:
F=-pA (-)
-J
where the factor y = i for the flow running out of the
moon-pool. See Ref. (9).
When the flow runs into the moonpool, the flow forms a
contraction just above the bottom opening, after which the stream widens again to fill the moonpool, as shown in Fig.
lib. The damping force caused by loss in the turbulent
eddies between the contraction and the wall of the moonpool follows eq. (14), but with values of y being dependent on the geometry of the bottom opening, see Fig. 12. The
usually accepted values for y are taken from Ref. (9).
- Device giving additional damping. An additional term allowing for quadratic damping due to damping giving devices such as appendages or choke decks are also allowed for.
The general expression is:
F p A -
-According to Ref. (10), p. 23, the damping coefficient due to a choke deck can be derived as:
= 1)2
where Ac is the open area, andoK can be approximated by:
A 2 = 0.598 + 0.4 (i-)
C
Collecting all force contributions, eq. (9) is rewritten by:
pAt y + pAt S2 + pAt (h + h') =
(18) v(1 + Cm) (j - + p Ab -
--Y +
2 pA
(S -
)' -
-
y p + p AtSolution of the Equations of Motion
Numerical techniques are used to solve the initial value problem consisting of the two non-linear second order differential equations
(2)
and (18) and the intial values y(t),t), v(t) and c(t).
By substituting from eq.
(2)
into eq. (18), the differential equations can be written:= f (y, y, , ) (equilibrium for liquid)
(19)
= g (y, y, Çr,
î,
) (equilibrium for bell) Furthermore, we introduce the parameters:(20)
r=y
s =v
such that eq. (19) can be rewritten by:
y=r
(21)
= f (y, y, r, s) = g (y, y, r, s,
which is a system of first order ordinary differential equations the solution of which is performed by use of fourth order Runge-Kutta formulae, see (11).
k
=
m+ PVC
m
This formula can be used to estimate k by use of vibration tests if Cm is known or to measure C if k is known.
Neglecting the influence from the bell and non-linearities due to the variable mass in the moonpool, the natural frequency for undamped free moonpool oscillation becomes:
()
g m
h+h'
The Computer Program
The above theory has been programmed and tested on several examples.
The input data for wave motion and ship motion may either be results from model tests or results from a seakeeping program.
The output from the program is given as time histories for motions, velo-cities, accelerations and forces. The numerical results can then be post-processed by use of SL's standard programs for spectrum analysis,
statistics, plots, etc.
The initial values for motions and velocities are to be specified by the program user.
For the cases where the wire force is determined by the stiffness of the hoist wire and winch system the bell will vibrate with a small amplitude
Model tests were carried out in order to verify the numerical procedure and in order to obtain values for the hydrodynamic coefficients for typical diving bells in moonpools with different diameters.
Hydrodynamic Coefficients
The three typical diving bells shown in Fig. 13 were manufactured on the scale of 1:20. The main characteristics of the three bells are given in
Table 1. The bell denoted by III is especially interesting since data
from full-scale measurements are available for this diving bell (7).
The models were tested in open-water and in four plastic tubes having the inner diameter 127, 144, 173 and 194 mm.
Added Mass Coefficient C m
The added mass coefficients were measured by use of vibration tests. From eq. (22) we have:
k m (23) C
m
PV
The diving bells were attached to a spring with stiffness k = 61.50 N/m and the natural frequency b =Wb/2U was read from the signal from a
force gauge connected to the spring. 4. MODEL TESTS
Table 1. Diving Bell Data.
Bell Mass (kg) Volume (ms) Projected Area (2) i: 5 504 4.568 3.020 II 6 608 4.160 3.834 III 5 200 4.576 3.611
Figure 13. Diving bell I, II and III.
Table 2. Added Mass Coefficients for Three Diving Bells Shown in Fig. 13. Bell Draught (m) Tube diam. (m) Frequency (Hz) Cm 0.65 0.127 1.140 0.89 0.65 0.144 1.176 0.77 0.65 0.173 1.205 0.67 0.65 0.194 1.220 0.63 1.246 0.55 0.55 0.194 1.223 0.62 0.75 0.194 1.209 0.66 0.65 0.127 1.014 1.34 0.65 0.144 1.061 1.07 0.65 0.173 1.106 0.86 0.65 0.194 1.126 0.77 II 1.150 0.68 0.55 0.127 1.029 1.76 0.75 0.127 0.993 1.45 0.65 0.144 1.147 0.93 0.65 0.173 1.211 0.72 0.65 0.194 1.224 0.67
co
cc
1.232 0.66The measured values for Cm are summarized in Table 2. The natural
frequencies are obtained as the average of three independent measure-ments each being the average taken over about 25 cycles.
As a test on the accuracy. tests have also been performed with a sphere
of radius 54 mm and the mass 835 g. The natural frequency b = 1.142
gives Cm = 0.55 which is ten per cent above the theoretical value Cm = 0.5 for a sphere. The discrepancy is assumed to originate from the boundary layer around the sphere.
For diving bell No. III vibrating in open water, the measured added mass
coefficient Cm 0.66 could be compared to the full-scale value Cm = 0.9 0.25% which has been evaluated by Mellem (7).
The following conclusions may be drawn from Table 2 and Fig. 14:
- The added mass coefficient Cm increases approximately with the projected bell area to the cross-sectional area of the tube as:
C m
1.9 ()
2.25 (24)- =
1 + C m- Cm depends on the tube length for the ratio
being close to 1, but not for small ratios of
Drag Coefficient CD
For a diving bell moving with constant velocity in a fluid at rest, equation (2) can be rewritten by:
2F (25) CD
1.8
1<.
Table 3 shows the measured drag coefficients based on the projected area
given in Table 1.
Q O
02
03 o5 O 01os
oo TTJO
Figure 14. Increase in added mass coefficient versus blockage
ratio.
The experimental test set-up is shown in Fig. 15. The diving bell is attached to a servo winch by use of an articulated rod.
The servo winch is trigged by a tringular signal such that the
bell has a constant velocity over a total length of 0.30 m when moving upwards or downwards . The force is recorded by use of a ring gauge
fitted on the connection rod.
A typical force signal is shown in Fig. 16. The drag coefficients for upwards and downwards velocity are recognized from the nearly stationary
Fig. 15a. The servo winch which is used to give the specified motion of the
bell.
Fig. 15b. Diving bell I in one of the tubes.
Table 3. Drag Coefficients for Models of the Three Diving
Bells Shown in Fig. 13.
Bell Frequency (Hz) Tube diam. (m) F F up down (N) (N) C up C down, D D 0.30 0.127 0.424 0.485 3.47 3.97 0.30 0.144 0.294 0.312 2.40 2.55 0.30 0.173 0.242 0.240 1.98 1.96 0.30 0.194 0.164 0.175 1.34 1.43 0.20 0.052 0.054 0.96 0.99 0.25 0.072 0.082 0.85 0.97 0.30 - 0.104 0.113 0.85 0.92 0.35 0.138 0.139 0.83 0.83 0.30 0.127 1.004 1.039 6.47 6.69 0.30 0.144 0.571 0.623 3.68 4.01 0.30 0.173 0.312 0.329 2.01 2.12 0.30 0.194 0.260 0.268 1.67 1.73
U
0.20 0.078 0.078 1.13 1.13 0.25 0.121 0.113 1.12 1.05 0.30 0.168 0.173 1.08 1.11 0.35 0.251 0.225 1.19 1.06 0.30 0.144 0.554 0.658 3.79 4.50 0.30 0.173 0.260 0.346 1.78 2.37 0.30 0.194 0.208 0.249 1.42 1.70 III 0.20 0.061 0.078 0.94 1.20 0.25 0.095 0.104 0.94 1.02 0.30 0.147 0.156 1.01 1.07 0.35 0.164 0.208 0.82 1.04For ce
Figure 16. A typical signal from the force gauge. The figure also shows the position of the diving bell.
F
down upThe drag coefficient CD = 1.08 for downwards motion of bell III in open
water corresponds to CD = 1.47 based on a projected area taken as the
cross-section of the pressure hull, instead of the entire projected area.
This value could be compared to the full-scale value CD = 1.9 12%
obtained by Mellem (7).
The difference is partly explained by auxiliary equipment below the diving bell from (7).
Fig. 17 shows the drag coefficients versus bell to tube area Ab/At. The
drag coefficients in Fig. 17 are the average for upwards and downwards
values.
From Table 3 and Fig. 17 the following has been concluded:
- The drag coefficient CD increases approximately with the projected bell area to the cross-sectional area of the tube
as:
CD Ab
(26) = i + 9.2
CD
n=
- CD is nearly the same for upwards and downwards motion.
- CD does not depend on velocity.
Model Tests in Waves
2.25
The testing arrangement is shown in Fig. 18. The tube with diameter
173 min is fixed with the opening 1 m below the water surface. SL's large
model basin was used for these tests and the waves were produced by a digitally controlled pnumatic wavemaker.
Three signals were recorded and stored on disk for further analysis:
- outside wave
- moonpool wave
- force acting on diving bell I situated inside or outside the tube.
Figure 18. Testing arrangement for tests in waves. The diving bell is shown both inside and outside the tube.
Tests were carried out with two regular waves:
Wave height (peak to peak)
H1.60
m Wave frequencyC=
0.660 rad/s.Wave height
H1.73
mWave frequency w= 0.890 rad/s.
and the irregular wave spectrum in Fig. 20 with significant wave height
1.35 m and the peak period 7.76 sec. A list of runs is given in Table 4.
The time histories are shown in Fig. 19.
The small ripples on the wire force signals are due to the elasticity in the hoist string.
Table 4. List of Runs in Large Model Basin. Data are given in full scale.
The frequency of wave I was chosen to be close to the natural frequency of the water column (m = 0.680), and for this case it was not possíble
to perform measurements with the bell in the moonpool.
For resonant excitation the wave amplitude was enlarged by a factor 4.7, and the moonpool wave was very stable.
The moonpool wave shows a kind of unstable beating, which is also met in the theoretical model, when being exposed to excitation frequencies away from the resonance frequency, see Fig. 19 b and c. The enlargement factor is only 0.3 for wave II which has a frequency that is 30 per cent above the natural frequency of the moonpool.
When comparing wire forces in run Nos. 958/959 and 960/961 it should be noticed, that the hydrodynamic forces acting on the bell decays exponen-tially with the distance from the water surface. Thus, being reduced to
the surface, the variable part of the wire force must be multiplied with a factor 2.5, and the variable part of the wire force then is smallest when the bell is in the moonpool. The draught and diameter of the
moon-pool could of course be optimized to meet a given set of wave spectra in a much more favourable way.
Spectra and response amplitude operators for force and moonpool waves are shown in Fig. 20 and 21. The response amplitude operators (RAU) should
be taken only as an illustration of the filtering effect of the moonpool since the RAO-analysis is only valid for linear systems.
RUN NO. Wave Height (m) Wave Frequency (rad/sec.) Remarks
957 1.60 0.660 Bell outside 14 m below surface. Resonance in moonpool.
958 1.73 0.890 Bell inside 12 m below surface.
959 1.73 0.890 Bell outsidemoonpool 12 m below surface.
960 Irregular wave
0. 838 (peak) Bell outside. 12 m below surface. 961 JH1/3 = 1.34 Bell inside moonpool 12 m below
2.00 UT51D( UPV (n) 2.50... 0.00. d -2. 50... 0.00 C -2. 00_ ¿0 .00
Ai AAíÀÀAÄaAAAAAAAIAIA AAAAAA
y,,
y,,,
J I . 25 S, \; Figure 19a.Measured Values. Bell outside 14 m below surface. H = 1.60 m
= 0.66 rad/sec T1n IN OINUT(s 1N)'. I.UIVE 1)1) 2 50 2.50 1111 IN F1INUTES J J 3.15 3. 15 J r' TESTS (resonance). SKI 5ST[KN 15K LFB0RPT0R I UM DIVING SELL 00E SCALE Ii LYNG6'I DRNMPÇ RUN 957 0RWN -5.00... TitlE IN rUNUTES FACE UP) i .00 0. 00 00 -.00 -2. 00 5. 00_ 2.00... .10 i. 00...
2.00 1.00 0.00 -1.00 -2.00 -2. 00_
f
OUTSIDE IJPVE (li)I
«
1.00 MOONP. IJVE (rl) -1.00 2.00j FOMCE INN) '10 0.00 1.00 -1 . 00_ Figure 19b.J
Measured Values. AA
hAlA 1111111
fof
111
1
TITlE IN MINUTES 0.50A
A
A A
A A
A &
£A £ £
.
£ &
à £
A A A
£ A
A A A A à A A
A &
s,0D,.y,v,v,y,Iy,vvvyv,vTv5!vvvvT
V175 1VVVVV'V50
TIME IN MINUTESBell inside 12 m below surface. H = 1.73 m
= 0.89 rad/sec.
TIllE IN MINUTES
ÍLRBÛBATOR J UM
DIVING BELL TESTS
OMOEM SL- SCPLE Ii 20.000
1.25
II
11 11!
VI s 1.25 rigure i...Measured Values. Bell outside 12 m below surface.
A
111111
11ff!! 1 11
TitlE IN r1JNUTES 2.00.. tlUTSIUE IJAVE uu 1 00... 000II
doIfpy
-i. 0o -200... 1.00. rl0NP. llAVE 1)11 0.50.A A
-L
A
T
-o.5o_ - I. 00.. 2.00... fOACE (KNI .10 i . 00 0 00 C 00 -2.00..,..
-AA £-AA*-AA-AA-AA-AA-AA4lh-AAA*4Ê-AA-AA14I-AA
VYV2YVVVWVY
y
ww'
y,,
--V YVVVVVVVVVV
50 TitlE IN IIJNUTES 2.50 TitlE IN MINUTES 3.75 H = 1.73 m = 0.89 rad/sec. SKI BSTEKN 15K DJVJNG BELL TESTS OFIOEFI SL-LAB OHR T OH J UM SCALE i. 20.000 LYNG6'! DANNARK HUN 959 DRWN2.00 OUTSIOE WOVE IF1 1. 00
000k.L
Lé
L_ L
LL
L*
L AAAA
MLAaLL
l
ALi'
k
'
i
'!
Wr
'
!.
IV''
YI
Y'
' I !.
!
J t Y
-1.00 -2. 00 4.00 1NP. 0000 (II) 2. 00DALA
!OYV
Vvv.v5VyVyy
-2.00 -4. 00 FMCE INN) 1.00 0.00 -:o.00 -l.00_ -2. 00_ 1 .75 Figure 19d.Measured Values. Bell outside 12 m below surface. 111,3 = 1.34
= 0.838 rad/sec.
peak
TIllE IN MINUTES Tirio IN MINUTES
3.50 TIME IN MINUTES SÇJBSTEKNJ SF LR5OBPTOHIUM 5.25 DJVJNG BELL TESTS 0000M SL- SCALE u 20.000
2. OO_ OOQA
£AA
AAIa*i.
gj
AL
A AAL
a&L AA
'1
'''V', I I I
'
i
I r' ii'
'
' '
'2Si
T
'II' I
"
O 00UTSIOE UPVE IN)
00 Figure 19e. TitlE IN MINUTES r10NP. UVE In) 1.75 3.50
Bell inside 12 m below surface. H113 = 1.34 m L)
= 0.838 m. peak SJBSTEKNJ s"; [ABURRIDA J UM ...-L'YNGBT OANMAMI(
DIVING BELL TESTS
0MOEM SL- SC8LE i RUN 961 DARUN -'L OO_ TIME IN MINUTES FOMCE KHI Measured Values. TitlE IN MINUTES 2.00... 'lo i i .00__ 0 00 -1.00 -2. 00 -2. 0Q_ 'LOO 2. 00 5.25
(N LQQ
r
cL 2.00 Li D (n 0.50 0.00 0.00 0.00RUN 960
0.00RUN 960
¡¡1
I 3.75 FEQ. T-FERK S 7.58 T02 5 7.36 SIGN.VAL. 1.3L1E+00 TEST TInE 7.00 1.50 PRO/S Uis: 2.00
t'
:i
Q-z
0.00 T-PEK s 9.27 TO S 9.21 SI .VPL. 2.95E+00 T S TIME 7.00\
SKI BSTEKN 15K
LPBOI9PTOP .1 UM
DIVING BELL TESTS
OFlOEFl SL-SCRLE L 20.000L'NG6 ORNr1RFlK Figure 20a. Power spectra. OFlPN 0O3l3 0.00
RUN 960
0.75F FlEO. 1 .50 1 .50 CN 0.75 FREQ. RPO/S LOO DtI
a: N. (fI 1-PERK S 7.50 102 S = 7.60 SIGN. L. 2.16E+00 TEST TI E 7.00N '-1.00 i O
-(nz
w 2.00 w D (n t-0.00 2.00 0.00 T-PEAP S 7.50 102 S 7.29 SJGN.VIRL. i.32E+OO TEST TIME 7.00 0.00 RUN 961 ST .VRL.9.t5E-00
TI
TJME = 7.00 E ('J> 2.00
a-D D E 0.00 0.00 RUN 961 9.47 STGN.VRL. 2.36E+0B TEST TIME 7.00S}KIBSTEKNISK
LAB OHR IOPiIUN
LYNG8Y 04NMA9K
Figure 2Db.
DIVING BELL TESIS
090E9SC9LE 1: 20.000
Power spectra.
O9RWN 8003130.0.
0.75 1 .50 RUN 961 FfiEQ. 990/S Np-L00
T-PER( S 8.27 T-PERPÇ S D 102 S S.2'4 102 5 0.75 F9EQ. 1 .50 990/S 0.75 F9 EQ. 1.50 990/S2.00
I . 000.00
E E 2.5CLz
0.00
HPO iiii,,
i'' t
i r t i i i i r r r i r r iSKIB5TENJSK
DIVING SELL TESTS
LBDRTOH JUM
/
L'INGBI oRNr1RRFigure 21a.
OVIOF9 SL-SCALE 1 2 ORPLN 8 0.000 00313
0.50
0.00
RUN 960
I . 001.50
2.00 FREQ. t APD/SEC0.50
1.00
1.50
FF9EQ. t VIRO/SEC 2.000.00
RUN 960
2.00 -10 1 .00 0.00 4.00 w
> 2.OIL
0.00 RUN 961 HAD 0.00 RUN 961 0.505 J55TEKNIS
LAOHATOH JUM
1.00 1.50 FREQ. ( RFLJ/SEC 2.00 0.00_ tII
ii
i i iI 1111 t
i iiii i
iiii
i 0.50 1.00 1.50 2.00 FFIEQ. ( HAD/SECDIVING BELL TESTS
060E6SL-SCALE 1: 20.000
5.
NUMERICAL RESULTSThe numerical method has been tested on a number of different examples, some of which will be shown here.
Water Level Motion in Fixed Moonpool
As a test on the accuracy of the method, the program has been tested on the model test series from the previous section of this report, Fig. 22 a-e.
Fig. 23 shows a comparison between measured and calculated results for
run No. 957 previously shown in Fig. 19a. The agreement is very satisfactory.
For the measured values, the velocity and acceleration are obtained by numerical differentiation of the moonpool wave motion after having smoothed the signal by use of the low-pass digital filter shown in Fig. 24
For the run Nos. 960 and 961 the outside wave has been approximated by 99 Fourier terms, the highest frequency of which being 1.5 rad/sec.
The best agreement between measured and theoretical results was found for run No. 957. For this case, the amplitude of the moonpool wave is
much larger than for run Nos. 958-961, since the wave frequency has been chosen to be close to moonpool resonance. The idealized model of the
flow at the bottom opening as shown in Fig. 11 is thus believed to be a
better approximation for large amplitudes than for the small ones of run Nos. 958-961
Discrepancies between measured and predicted results may also be due to model scale effects such as:
- wall friction - laminar separation
- damping from the wave probe
- formation of axisyrmnetric surface waves in the moonpool.
A comparison between the measured and calculated moonpool wave for run No. 960 is shown in Fig. 25. The calculated moonpool wave is both
shown for (y , 3 ) = (1,0) which is the theoretical value for the bottom
damping and for (y , = (1,1) which is twice the theoretical value.
The validity of Morison's formula is found to be excellent both for the bell inside and outside the moonpool.
The results shown in Fig. 26 are obtained by using the measured moonpool wave from run No. 961 as input to the computer program. The figure also
00 LOO -t .00 -2.00 URVE M0TII3F Ut)
AA AAAAAAAAAA AAAAAAAAAAAAAAAAA
5.00.. t'ARTJOLE rtflTttON li) 00 I . 25 Figure 22a.Numerical Results as Run
957.
Bell outside 14 m below surface. H
1.60 m = 0.66 rad/sec. (resonance) TitlE IN MiNUTES So TIME IN MINUTES 2.00 WtME FOFICE tFOJt 10 2.50 TItlE IN MINUTES
li
i LP5ONRTOHIUM 3.75 D1VN BELL TESTS 0RUE-2. 00_. i .00 0.50 t. 00_. 0,00_ :o.00 -2. 00.. FfFtT1CLE r10T10 (It] o.00 A
L
L
A AALA
AA.
A AALA £AA.AAAA
i p y"
iyryyvyyyv.9vvflvvflvvflyyyv.o
-0.50 (flaE FOF.CE UÇUI i . 25 Figure 22b.Numerical Results as Run 958. Bell inside 12 m below surface.
1111f IN FUMiJTES lIftE 1M IUMUTES
2.50 T1rE IM MJMiJTES 3.75 H = = 1.73 m 0.89 rad/sec. SFIBSTEKNISK LIRBODRTOPLI UM LS.KG8'( UPNMRIIK
DIVING 8ELL TESTS
2.00 SR n0T1 rtj I . 00 o co -1 00 -2.00 1 00 O 50 0 00 -0. 50_. -1 . 00_ 2.00...: .10 0.00
I
IAAAAA
AAA
AAA AA
AA
AA
u1111111
2j
7
1121711171
11
;.177111
1
o 0.10 0. 00 PRftTICL[ r10TJ04 II)WIflE I09C{ (KNI
I . 25
Figure
22c.
Numerical Results as Ruii 959. Bell outside 12 m below surface. H = 1.73 m
= 0.89 rad/sec.
TINI IN MiNUTES TINE IN tIINUTE
2.50
TINt IN rilNuTEs
rì
SFc I OSTERN J SR LP500PTOO I UtI
DIVING BELL TESTS
5L-2.00 UTSI0E UPVE (11) 1. 00
000AM4
£ £ .,.T
''11
V1.'5 wvv!r!
V
y -I .00 -2.00 H113 = 1.34 m = 0.838 rad/sec. peak 1111E IN luNUlESSKI AST EKrJ 15K L A B D B A TO A JIJ M LING8'Y
OPNMAMK
DIVING BELL TESTS
00ER SOPLE li ORIIUN
-4.00 11(10 IN MINUTES 2 . 00. UlME FISIICE (KW) .10 I . 00_. 0 00 1000 1. 75 3.50 5.25 -1 . Fi;ure 22cl.
Numerical Results as Run 960.
-2. 00..
TIrIO IN luNUlES
Bell outside 12 m below surface.
9. 00..
MNP. IJRVE
2 0O_ i .00.. 0 00 -1.00 -2. 00.. 9. 00.2 2.00... 0 00 -2.00_ -4.00 1.00 0 00 -1,00 0.0 OUTSIDE I4Í1VE ill) 00 LJOUIIJ MOT (M) 2.00
lUME FOMCE (liN)
.10 TIME IN MINUTES
A.
LAAA
LLLAAAAAAA
',T,'''Y51,
U''!'''
TIME IN MINUTES 1.75 3.50 5.25 -2.001 Figure 22e.Numerical Results as Run 961. Bell inside 12 ni below surface. H113 = 1.34 m LI
0.838 rad/sec. peak 1111E IN MINUIES ' SKJBSTEKNJSK
DIVING DELL TESTS
OMOEM
SL-LRBU9RT0D1UM
I. 00 0. 50 o 00 -0.50 -1.00 3. 00 2.00 I. 00 C 0G -1.00 -2.00 -3.00 2.00 t. 00 O 00 -t .00 -2.00 2.00 I . 00 0 00 -1.00 -2.00 t .00 .10 0.50_ 0 CII 0.0 Measured values - - - - Numerical results
OUTSIDE WAVE ¡II)
U1E FONCE (KN)
TINE IN SEC.
1111E IN EEC.
15.0
SKIBSTEKNISK
DIVING BELL TESTS
ORDERSL-LABORRTOH JUN
SCALE It 20.000LINGS'( DANMARK Figure 23. DRAWN 600122
DIGITAL FILTER DESIGN
TYPE OF FILTER
LPCUTOFF (ON) FREQ.
( HZ ) 1.500S1MP. JNTERVFL
( SEC ) 0.OLIONO OF COEFFS.
161.FILTER CODE (INDEX)
18.(Model scale)
- r -
r-
- - -2.50 3.75 5.00 FAEQ MSKJBSTEKNJSK
LP6ORRTOR JUM
LING6Y DRNMRflFigure
24. ORDER SL DRAWN 8001210.00 2.00J t1NF. WPVF UI) I . 00 0.00 TillE IN llINUTES
-Calculated with P = O Calculated with 3 =SKIBS TE N IS L RB BRAT OR IUM
DIVING BELL TESTS
ûR0 SCALE LING61 CANIIARK RUN 960 ouN 1. 0U_ OuTsI0 IJAVE (Ii
Measured moonpool wave.
9 .1J0_ o jio PP.MTICL M0I (MI 0 00 -0. - i . oo i.00.. DMRG F6F(CE (KNI -io o. so_ 0. 00 1111E IN MINUTES WIBE FORCE (NH) TIME IN MIMJT5 dy
Y V
VV Y Y Y Y
' !
Y '
Y 0! Y YV '
' Y
Y!CY V V '
TIME IN MJN(.TES-AAAAA AAA&
£AA
', V V V y V Vy y
V -2.00 .00 Figure 26.Calculated wire force based on measured moonpool wave from Run 961.
TIME IN MINUTES 6.00 -i. 00__ -2 .D0_ I.00_, MRS 0-So-1Z9C (liN) SKJ5STE)(NJS
DIVING BELL TESTS
LRB O FIR T OFIJ UM -$.-Uo--2. 00_ 10 i. oo__ 0.00 2.00 '(.00 6 .0D
Influence of Winch Strategy
The influence of the response of the hoisting system on bell motion and wire force has been studied numerically for a number of different winch
types.
The diving bell III with Cm and CD taken from Ref. (7) is suspended 8 m below the still water level in a moonpool built into a ship with the draught 10 m.
The cross-sectional area is 30 m2 and the bottom opening is not protruding into the flow.
The wave height is 3.4 m and the wave frequency is 0.6 rad/sec. The total
vertical motion of the ship at the point of suspension is 1 .4 m and the
ship and wave are 30 deg. out of phase.
The initial values for the moonpool wave motion are y(0) = 1.5 and (0) = O
and the simulated time was 20 seconds.
The above parameters were chosen such that slack would occur in the hoist rope after 5 seconds unless any action was taken to prevent the wire from being slack.
The following cases were studied, see Fig. 27 a-f.
Bell fixed.
Bell in wire with stiffness k = i . 107N/m. The wire
becomes slack, and the bell undergoes several sudden
jumps.
The maximum wire force is 43 . 104N which is nearly
eight times the dry weight.
C Bell in flexible wire (k = 1 . 106N/m). The bell
accele-rations are less severe. The maximum wire force is more than halved compared with case b
d . Bell in stiff wire and winch fitted with relief valve
Bell in stiff wire and winch fitted with a device to maintain a mínimum wire tension of 1000 N.
The bell undergoes small vibrations after the moment,
where the winch has stopped.
Bell suspended in constant tension winch with the tension
.00.4 MONP. WAVE (M) 2.00.. 0.00 -2.01LO.O -4.00: WAVE M5TJtN (M) 0.0 ShIP MT1tN ((1) BELL M(TJ0N (rl)
'4.00 BELL ACC. (tl/SEC2)
2.00 WIRE F(FLCE (W 'iP. 010 10.0 TIME IN SEC. TIME IN SEC. TIME IN SEC. TIME IN SEC. TIME IN SEC. TIME IN SEC. 20.0 20.0 20.0
SKIBSTEKNISK
DIVING BELL TEST
OADEASL-LRB O F1R T O Fi UM
L1NGBL DRNMAAK
Figure 27a.
Fixed bell.
OHAWN 800130'.. 20.0 ' I 5.0 0.0 10.0 15.0 5.0 10.0 15.0 20.0
LOO
0.00 -t. 00 -2.00 4. 00. 2. 00.. 0.00 -2.0O -'4. 00 1.. i: 1cfso...E 0.00 -0. 5cLE -1 . O0_ k50 0.00 -2.50 -5.00 0.00 -2.50 -5.00 0.0 0.0 WAVE t1OTIN (M) MNP. 1-JAVE (M) 0.0 SELL MTJN (M) 5.00 WIRE FORCE (KN) 2 50 ' I 5.0 10.0 TIME IN SEC. TIME IN SEC. t I t 10.0 TIME IN SEC.2.00... SELL VEL. (ti/SEC)
i . 00_ 0.00_ k
V-.4
T 1 --.
-i.0cL.0.0 5.0 10.0 15.0 20.0 -2. 00 TIME IN SEC.5.00J bELL ACC. (M/SEC2)
' I ' I
i
J 0.0 5.0 10.0 15.0 20.0 TIME IN SEC. 0.0 5.0 10.0 TIME IN SEC. 20.0 20.0 2G.0 15.0 20.0 OROEhSL-SKIBSTEKNISK
DIVING BELL TEST
LABORPTOI9IUM
2.00 WAVE (WTIN (M) 1.00 0 00 -1.00 0.0 -2.00 8.0 SHIP IWTIt1 (M) -1 i -0.0 _LI.Q .13.0 8.0 -q.00.... 2. 00 0.00: -2.00.. _LLQO_ i.00_.
j:
kR 5o 0 00 -0. 50.. -1.00.. MWN'. URVE (M) 0.0 BELL MtTIN (M)2.00.! BELL ACC. (M/SEC2)
lia. (it0__ 0.00: - V T -, -l.0O.0.0 5.0 -2. 0O_
cD
10.0 TINE IN SEC. TIME IN SEC. 10.0 TIME IN SEC. TIME IN SEC.2.00 BELL VEL. (M/SEC)
1.00 0.00 -1.00 0.0 5.0 10.0 -2.00 TitlE IN SEC. 15.0 20.0 20.0 20.0 15.0
'20.0
I -. _I__J 10.0 15.0 20.0 TINE IN SEC. 2.00 WIRE F0ACE (KN)A
A
n
g g i i i i i g -1.00 0.0 5.0 10.0 15.0 20.0 -2.00 TIME IN SEC.SK1BSTEKF'SF
OJVJNG BELL TEST
OffiJERSL-LRBÚFRTOHIUM
L'YNGB'Y DANtIARK
Figure 27c.
Flexible wire.
DRAWN 800128I ( 10.0 u i g 15.0 0.0 20.0 i r 5.0
2.00
1.. 00
URVE MtTItTh (ti)
0.00 P1IÍh.
-i.00..EO.0 5.0 10.0 15.0 20,0
-2. OQ.E
TINE IN SEC.
8.0 J SHIP MTIN UI) --q.o ..0.0 5.0 10.0 5.0 20.0 -8.0 TIME IN SEC. q.00 tIONP. L1RVE (M) 2.00.. -2.00.EO.0 5.0 10.0 15.0 20.0 -q.00 TIME IN SEC. 1.00. BELL MTJ6N (M) kP.51o4 0.00: - I I I I t I I I I I -0.500.0 5.0 10.0 15.0 20.0 -1. TItlE IN SEC.
2.00 BELL VEL. Ui/SEC)
LOO
0 00
--1.00 '.0 5.0 10.0
" '
15.0 20.0-2.00
TIME IN SEC.
2.00....6 BELL ACC. (M/SEC2)
--i.0O..0.0 5.0 -10.0 15.0 -20.0 -2. 00.. TIME IN SEC. 2.00 UIIiE FRCE (KN) I1Cco1
I A I I I I J I I I I J I I I I0.OI
-1.00 6.0 5.0 10.0 15.0 20.0 -2.00 TitlE IN SEC.SKIBSTEKNISK
DIVING 8ELL TEST
0A0ESL-LR5OI9PTOI9IUM
Figure 27d.
Stiff wire
2.00 1.00 0.00 -1.00 -2.00
6.0 ... Sill? MTItTh UI)
-1
-a1tp 4
-8.0
4.0Q_ MINF. I.JRVE UI)
2.Q0..
Q 00
-2. O0...0. O
-9. 00_
BELL I(TJ0N UI)
i:
kP5o4
0.00-0. 5Q
-l.00-8.0 BELL VEL. II/SEC)
-1 a'p.0
0.0 -9.0 -6.0
l.00.. BELL ACC. (M/SEC2) 0. 50.. 0.00: -0. 50 -i. QQ_E 2.00 WJI9E FI9CE (KN) i 5.0 -2. oo..E 0.0 0.0 0.0 0.0
WAVE tItTIN UI)
J I 5.0 5.0 10.0 TIME IN SEC. 10.0 TIME IN SEC. TIME IN SEC. t -J- t 10.0 TIME IN SEC. TIME IN SEC. '
i
-t 10.0 TIME IN SEC. TIME IN SEC. 1 15.0 15.0 15.0 20.0 20.0 20. 0 20.0 20.0 0.0 I i 20.0SKISTEKNISK
DIVING 6ELL TESTS
OflOEhSL-LRSOI9RTORIUM
LThGBY OANMRAK
lIIl*lii4
gv, , , iv, 'V,
Figure 27e. Stiff wire
2.00 WAVE MT1N (M)
i 00
0.00-1.00 0.0
-2.00
6.0 SHIP MOTIN (M) 0.0 -4.0 0.0 -6.0 2. 00... t: .1100-0.00: -2.QcL 2.00...: l.00-0 l.00-0l.00-0-i. 00_i
-2.00_
cU
q.00: t1ONP. WAVE (M) 2. 00.. 0 00 -2.00..0.0 -q.00-BELL FrnTJN (rl)2.00..1 BELL VEL. (ti/SEC)
i.00-0 00: -i. 00.. 0.0 -2. 00 BELL RCC. (ll/SEC2) .0 5.0 1111E IN SEC. 10.0 TIME IN SEC. TIME IN SEC. 10.0 1111E IN SEC. TINE IN SEC. TIME IN SEC. 20.0 20.0 20.0 20.0 15.0 20.0 ' i ' ' i '
0.01
-9.0 0.0 5.0 10.0 15.0 20.0-8.0
1111E IN SEC. 6.0 .. WIRE F0RCE (KN)q.0J
SKIBSTEKNISK
DIVING BELL TESTS
ORDERSL-LPBOARTOFfl UM
L'(NGB'Y DANMAIiK Figure 27f. Constant tension winch.
r I J- I -r
6. CONCLUSIONS
The launching / retrieving procedure for a diving bell has been studied theoretically and experimentally.
A variety of solutions to minimize the necessary wet weight of the diving bell to avoid slack in the hoist wire has been reviewed briefly,
and a special attention has been given to the moonpool approach.
A numerical símulation procedure has been developed for the prediction of the non-linear water level motion in a moonpool and the forces acting on the diving bell.
The necessary hydrodynamic coefficients for this procedure were measured for models of three diving bells in tubes with different diameters.
Both the added mass coefficient °m and the drag coefficient CD appeared to increase with the blockage ratio in a systematic way.
Model tests were carried out in regular and irregular waves with one of the diving bells situated in a tube. The moonpool wave and wire force were predicted theoretically using the measured values for Cm and CD, and a good agreement was found in most cases.
A number of simulated operating situations showed that the wire force and bell motion depend very much on the control strategy for the winch response.
The present investigation confirms that it is possible to treat the problem of launching a diving bell through a moonpool theoretically in a satisfactory way. Only moonpools with smooth wall were considered in the numerical examples, but more complex configurations may be treated by modifications of the input parameters or by slight modifications of the theory.
(8)
"New Diving Bell Compensator for Heavy Seas",
Ocean Industry, March 1979.
"Rough Weather Diving System",
Ocean Industry, February 1977.
Busby, R.F.: "Houlder's Semisubmersible Support Vessel",
Journal of Naval Architects, January 1976.
Kuo, C.: "A Controlled Handling Method for Effective Offshore Supported Operations",
OTC Paper No. 3318, 1978.
(5) Huges, D.: "MOOnpOO1 Design for Diving Support Vessels", Underwater Systems Design, October 1979.
British Patent No. 1226319, Norwegian Patent No. 19814.
Mellem, T.: "Surface Handling of Diving Bells and Submersibles in Rough Sea",
OTC Paper No. 3530, 1979.
Fukuda, K.: "Behaviour of Water in Vertical Well With Bottom Opening of Ship, and its Effects
of Ship Motion",
Journal of the Society of Naval Architects of Japan, Vol. 141, June 1977.
Massey, B.S. : "Mechanics of Fluids",
Van Nostrand Reinhold Company, 1975.
Prandtl, L.: "Strömungslehre",
Friederick Vieweg & Sohn, Braunschweig, 1965.
Ralston, A. and Wilf, H.S.: "Mathematical Methods for Digital Computers",
Wiley, New York / London, 1960. REFERENCES
A program to predict water level motion and forces acting on a diving bell during launching through a moonpool.
The following data sheets may be taken in any order. The last data sheet must be followed by l:EODI
Moonpool Data
Name of data sheet, check No.
Draught of moonpool (m)
Cross-sectional area of moonpool (m2)
Bottom opening protruding into flow YES/NO Damping coefficient
I for quadratic damping
Wall friction included (Blasius), model scale only YES/NO Kinematic viscosity (m2/sec) (only if wall friction)
Start amplitude of moonpool wave (m), pos. upwards Start velocity of moonpool wave (m/sec)
MOON,
New data sheet (PRO) BELLMOON
INPUT (file name)
#TEST (file name)
\
L
Name of data sheet,Check No.
Mass of bell (kg) Volume of bell (m3)
Projected area (m2)
Added mass coefficient Cm
Drag coefficient CD
Start position of bell (< O and rei, to ship)
Start time for launching / retrieving (sec.)
Bell motion determined by constant tension winch Tension of constant tension winch (N)
Bell motion determined by constant velocity Launching / retrieving velocity pos. up (rn/sec)
Connection type bell-ship inelastic
Connection type bell-ship as elastic rod Stiffness of connection (N/rn)
Initial elongation pos. downwards (rn)
Connection type bell-ship as elastic wire Stiffness of connection bell-ship (N/rn)
Specified max. wire force (N)
Ability to specify min. wire force YES/No Specified min. wire force (N)
:BELL, CTENSIO C. VELO (INELAST I ROI) WIRE
The bell is fixed until the wire becomes slack or the specified
min. or max. wire force has been exceeded.
new data sheet
new data sheet
new data sheet
new sheet if NO new data sheet
(t
Name of data sheet, Check No.
Ship fixed
Regular ship motion: z = a cos (t-4,) Amplitude a (m)
Frequency (rad/sec.)
Phase
4, (deg)
Irregular ship motion
Irregular Ship Motion (Only to be filled-in if ship motion = IRREG)
Name of data sheet, Check No.
N
Irregular ship motion: z = a
cos 4t-
4)
n= iNumber of Fourier terms N (max. 300)
The following data may be output from program RHARN.
:SHIP,
FIX
REG
IRREG new data sheet
f :FOUSH,
new data sheet
new data sheet
new data sheet Frequency (rad/sec) Amplitude (m) a n Phase (deg) 4, n
\
Irregular wave
Irregular Wave (Only to be filled-in if wave motion = IRREG)
Name of data sheet, Check No.
N
Irregular wave: w = Z a cos t- 4' )
n n n
n= i
Number of Fourier Terms N (max. 300)
The following data may be output from program REARM.
new data sheet
new data sheet Frequency (rad/sec) Amplitude (m) a n Phase (deg) 4'n Check No.
Name of data sheet, :WAVE,
Density of water
Still water
(kg/rn3)
new data sheet STILL
Regular wave;
w = a cos (t-
4i) REG Amplitude a (m)Frequency (rad/sec)
Name of data sheet, Check No.
Start time for integration (sec.)
Stop time (sec.)
Time increment (sec.)
Accuracy of solution e.g.
iO3iO6
Max. lines to be printed (number of time steps)
Type of response to be printed
:OUTPU,
EOA
The following possibilities exists:
WNO Wave motion (m)
PMO Particle motion (m), i.e. moonpool wave or liquid motion at the bell position if no moonpool
PVE Particle velocity (m/sec)
PAC Particle acceleration (m/sec2)
SMO Ship motion (m)
SVE Ship velocity (m/sec)
SAC Ship acceleration (m/sec2)
BMO Bell motion (m)
BVE Bell velocity (rn/sec)
2 BAC Bell acceleration (rn/sec )
FWI Wire force (N . iO)
FDR Drag force (N . iO)
FMA Mass force (N 103)
RNO Relative motion (m) Moonp. wave - ship.
Max. 6 types for upright A4 format.
Max. 7 types for output to be used as plot data file. Max.1O types for wide paper format.
The time increment gets halved up to 10 times to obtain the desired accuracy. The required step size will especially be small for the case of slack wire. If equidistant time steps are required, a sufficiently small initial step length may be chosen, or result lines for intermediate time steps may be deleted.
Time history No. Name of time history
Min. of max. value at y-axis
Give input to plot file #IN
The following possibilities exist for time history names:
WMO Wave motion (m)
PMO Particle motion (m)
PVE Particle vel. (ni)
2
PAC Particle acc. (rn/sec )
SMO Ship motion (rn)
SVE Ship vel. (m/sec)
SAC Ship acc. (m/sec2)
BMO Bell motion (ni)
BVE Bell vel. (m/sec)
BAC Bell acc. (rn/sec2)
FWI Wire force (KN)
FDR Drag force (KN)
FMA Mass force (KN)
ENO Relative moonp. wave (m) (between moonpool wave and ship)
NEW New text to be defined by the user.
The output from program 1tBELLMOON" stored on a symbol file must contain
a max. of 7 time histories and 2500 time steps. All lines except those
for the time solution must be deleted.
Two possibilities exist:
Post-processing by use of the SLAFO database.
The data are transferred to SLAFO by use of the program REALSL. The time solution must be given
for equal time steps.
Plot of time histories by use of the program THIST:
(at present only available for interactive use).
(PRO) THIST
TS S
Viewport (= i for scale 1:1)
X-length of frame e.g. 21.-29.7-42 cm Y-length of frame e.g. 21.-29.7-42 cm
Text identifying plot
Length of x-axis ( x-length of frame minus
Length of pos. y-axis (cm)
Start time (sec)
Stop time (sec)
Number of time histories on file (max. 6)
Number of time histories to plot (max. 6)
>
5$43 $3 $333
$3333
DIVING
ELL - MOONPUOL
VERSION 05.02,1980/NM
s s s s s s sss sss 533 s $ $ s $ 3$ £$ $3 $ 3$ 3$ $ $3333$ SS $33$ $33$ $33333333$ SS S $
FAM'ETRS OF THE PRO8LEM:
DATA FO
SHIP MOTION;
THE SHIP IS FIXED.
DATA Qk SELL:
MASs OF SELL (KG)
VOLUME yF SELL (M3)
PRO1)ECTc.D AREA UF SELL (M2)
ADDED MASS COEFFICIENT
CRAG COEFFICIENT
STMRT POSITION OF
LL (i1)STAtT TME FOR LAUNCHING/RETRIEVING (SEC)
LAUNCHING/RETRIEVING VELOCITY (M/SEC)
8ELL 1NtLASTICALLY ATTACHED TO SHIP
CMT FO WAVES
DENSITY OF WATER (KG/M3)
REGULAR WAVES.
sAVE AMfLITUUE (M)
MVE FREQUENCY (RAD/SEC)
WAVt. PHASE (DEG)...
DATA FOk MOONPOOL:
DkAUGrT 0F MUONPOOL
(M.)CROSS-S.CTIONAL AREA
OFMOCNPOOL (M2)
OTTUM OPENING PROTRUDING INTO FLOW
CAMPING COEFFICIENT FOR OUACRATIC DAMPING
START AMPLITUDE OF LIUIO (M)
STT VELOCITY UF LiUIU (M/SEC)
DATA FQ
OUTPUT CONTROL:
START T1M
FOR I,TERATION (SEC)
STOP TI-E (SEC)
TIME INUREMENT (SEC.) ACCURACY OF 5OLLiTIO
RESUL1 S:
RESULTS FOR FR
MOONPOOLCSCILLATIONS
EQUIV. COLUMN LENGTH OF ADDED MASS (M),
NATURAL FREQUENCY (RAD/SEC)
NATURAL PERIOD (SEC)
5504.0000
4,5680
3.0200
0,6100 1. 970012.0000
0.0000 0.00001000.0000
0.8650 0,8900 0.000020.0000
9.2400 0.0000 0,0000 0, 0000 0, 0000300.0000
0,2500 i0000E-04
1.24630,6795
9.2467
0.000
0.5O
0.ò4'. 0.0018,914
O,7b1 0,004b.969
0.679
0,010 9,057 0.544 0.016 9,172 0,3830.02
9.306
1N.Mfr Ai'4() MAXDuM VALUES;
MOTION (M)
PAkTICL. MOTION
(M)FMRTICL
VELOCITY (,'i/SEC)FMFT1&L.
MCCELERATICN (1/SEC2)
SiI
1OTION (M)
SiiW VELOCITY (M/bEC)
StiIP ACCLEkATIOF
(M/5EC2)L#.T1Vt. MOTION (M) MOONP. WAVE - ShIP
LL ¡'lOTION (M)
BELL VELOCITY IM/SEC)
EELL McELERMTI0f
(il/SEC2)hI. FOC
(P'N)CRA,
FQkCE AT BELL
<N)SASS