REPORT No. 25S
October 1957STUDIECENTRUM T.N.O. VOOR SCHEEPSBOUW EN NAVIGATIE
AFDELING SCHEEPSBOUIV - PROF. MEKELWEG - DELFT(NETHERLANDS' RESEARCH CENTRE T.N.O. FOR SHIPBUILDING AND NAVIGATION
(SHiPBUILDING DEPARTMENT - PROF. MEKELW'EG - DELFT.)
*
EXPERIMENTAL DETERMINATION OF
DAMPING, ADDED MASS AND ADDED MASS
MOMENT OF INERTIA OF A SHIPMODEL
by
Jr. J. GERRITSMA
ADDED MASS AND ADDED MASS MOMENT OF. INERTIA
OF A SHIPMODEL
by
Ir. J. GERRITSMA
Publication No. 8, Delfl Shipbuilding Laboratory
Swmpsis
The damping, added mass and mass momentof nertia of a shipmodcl, performing forced heaving or pitching
Oscillations in calm water, are determined cxperimentally.
Th influence of model spccd, amplitude and frequency of th motions on these quantities has bcii sttided. Tb2 coupling terms in the casc of a combined heaving and ptching motion are considcrcd for one model pced.
Some of the experimental results are corn pa red w t Ii calculated valucs, vhic ii hav2 bcen publish2d rccentl s
I,,troi! /1db 1/
Our knowledge of the hydrodynamic forces and moments acting on a ship in waves, based on
ex-periments, is rather small.
Concerning the heaving antI pi telling motions,
which will be discussed in this publication, some experimental data on damping and mass as a func-tion of frequency have been given by Haskind and
Rieman
[1]
and by Golovato [2]. In both cases amathematical shipform was
forced to performheaving motions in calm water, to obtain the neces-sary information.
Theoretical in vestigations on damping and added
mass have contributed only a few practical results in the low frequency range which is of interest for
ship motions.
1 he calculation of added mass in the high fre-quency range (ships vibrations), provides less dif-fic tilt i es.
Free surface effects arc negligible in this case and
the
resulting boundary condition
facilitates thecalculation of hydrodynamic effects considerably.
Such a boundary condition does not hold in the low
frequency range, which complicates the theory.
The influence of free surface effects on damping
and added mass, prevents an extrapolation of ii gIl
frequency values to the low frequency range.
Con-sequently, the calculation of the coefficients of the differential equations, describing the heaving and
pitching motions, is usually based on simplified ;ind rather coarse assumotions [3, 4].
So! vi ng the thus fou 11(1 differential equations for
amplitudes and phase lags, fairly large differences
Earnetimes are found between calculated and mea-sured ship motions.
To investigate the origin of these differences, it
scems necessary to comoare each of the calculated
coefficients of the equations with measured values,
as each of them contributes to the amplitude and
phase of die resultitig motion.
in addition to tile comparison of calculated and
measured shipmotions, tile knowledge of tile
mag-nitudes of the various coefficients, and the
in-fluence of hull line modifications on these
coeffi-cients seems interesting.
When sufficient knowledge of this influence is available it will perhaps be possible to predict the
effect oii shii,motions of certa in ii till Ii tie nlodi fica-tions with more accuracy.
This would reduce the number of model tests in
waves, when the determination of an optimum per-formance in rough water is the ultimate goal.
Tile data oresented in this article do not hive the pretention to be complete in this respect; they are coil fined to one shinform, namely the Todd
60-series parentform with a blockcoefficient C, .60. Also tile exciting forces and moments due to the waves are not considered. It is intended to determine
the exciting forces 2nd moments of this model in the Ilear future and to complete tile research with
two models of tile same series with blockcoeflicients
C, .70 and C .80.
Measit I/nc ,i,iI/otIs
There are a number of methods to excite a ship-model ill calm water, which have been published
recently.
They will be discussed here briefly.
First, tile work of Haskind en Rieman [I ] must
be mentioned. In their paper a method to obtain
damping and added mass for the forced heaving
motion has been given, as well as tile experimental
results for a mathematical shipform at zero speed. A method to determine the damping and added
mass moment of inertia for the pure pitching motion
and the coefficients of tile so called cross coupling
terms for a combined heaving and pitciling fllOtiOil
is also indicated, but no experinientai results have
DOUBLE GUIDES ON BALL BEARINGS
SPRING
GUIDE
PURE HEAVING MOTION
HEAVE POT. METER
A
PIVOT
/
PITCH POT. METER
PURE PITCHING MOTION
SPRING B
GUIDE
PITCH POT.METER
COMBINED PITCHING AND HEAVING MOTION
C
Iig. I it rrafl genie,,! oJ Is!
'2a. i9
1,
/ 24Q
A sketch of the test arrangement is shown in
Fig. 1.
Fig I a shows the arrangement in the case of a pure heaving motion; the model is free to perform heaving oscillations, but is restrained for pitch by
a vertically guided rod.
The exciter consists of a spring connected to
the model via the guided rod, whereas on the other end of the spring a harmonic motion is applied by means of an eccentric.
Amplitude of motion, phase lag between the
motion of the eccentric and that of the model, as
well as the frequency of the excitation are measured.
This gives the necessary information to compute
damping and added mass, as will be seen later.
A modification of this method is possible with the use of an electronical dynamometer instead of the spring, as proposed by Sr. Denis { ].
The elccrronical dynamomerer can be regarded as a spring with a high spring constant.
Golovato
[2]
used a six component strain gagedynamometcr to study the hydrodynamic forces
and moments of a mathematical model performing
pure heaving motions. The six component dynamo-meter was used in this case to measure the moments
due to heave as well (coupling terms).
His tests include a variation in model speed. Finally Grim [ I used eccentric rotating weights
to excite the model. On each end of the model
a
rotating weight
is located; the weights werecou pled by the driving mechanism, but t heir phase differed 180 degrees to obtain a sinusoidally
vary-ing moment.
Each of these methods has its own advantages and
disadvantages.
The electronical dynamometers appear to be very
sensitive with respect to vibrations of the towing carriage, which leads to a certain amount of noise
on the registration and necessitates hand fairing.
Particularly when measuring phase angles, inaccu-racies may occur in this way.
An advantage of the method is the fact that the
amplitudes of model motion and exciter are almost
equal, which simplifies the study of non lineair
phenomena.
The system of the rotating weights, of which
some rnodi fications are know ii, has the ci isad vantage
that the exciter is driven by a motor which is placed in the model.
Due to the model motions, it is sometimes
diffi-cult to obtain a pure sinusoidal excitation, as the
size and therefore the power of the motor is limited
by the dimensions of the model; moreover, the
exciting moment is proportional to the period
squared and this necessitates relatively large weights
at low frequencies to get reasonable shipmotions. The system using an electronical dynaniometer
as well as the one using rotating weights have been
tried in the Dcl ft Sluiihuilding Lahuraory, hut the
just mentioned disadvantages led to the preference
of the system with a spring exciter (as shown in
Fig. 1).
The test arrangement for pure pitching motion
is analogous to that for jnire heave and is shown in
Fig. Ib; the arrangement for the combined heaving and pitching motion is given ill Fig. ic,
In each case, the motions are measured electron-ically via microfriction potentiometers, whereas the
phase lag of tile model is defined with respect to a
certain position of the eccentric.
Motion, phase and an accurate time base are re-corded on a "Sefrarn" pen recorder, capable of 20
cm per second paper speed.
We will now proceed with the derivation of the
analytical expressions which are used to determine the various coefficients of the differential equations from tile measurements.
For the pure heaving motion, the following well known differential equation is valid (see Fig. Ia)
lIZ
+
hz + cz
FehV (1) where: aii
/?C =
'S1+
k.= kr
mass of model added mass waterplane areaspecific gravity of fluid spring constant of exciter vertical displacement of model
The unknown coefficients a and b (mass and
damping) are solved after substitution of the
solu-tion:
= z0
,I(oI--Separating the real and imaginary parts, one finds:
kr
C - -
cos a zo 2 (2) (1) and: b= - sin (I
(liZ11 k r (3)Ihe amplitude of heave zo, the phase lag be-tween tile motion of tile eccentric and of the model,
and the circular frequency II are to be measured,
which allows a and I) to be calculated.
A sinlihar procedure holds for tile pitching motion (see Fig. 1 b). Tile model is
free to pitch but is
restrained for heave.
The pivot is located ill
the models' centre of
gra v t y and the spring of the exciter is connectedto the model at a distance 1 from the pivot. The differential equation for this case is given by:
A'1' + B'1' + C'j'
Mt"t (4) where:A = I + ,v
C = ' K + k 122
M = k. lr
in which:I mass moment of inertia of the model
ii,, added mass moment of inertia
K moment of inertia of waterplane
y pitch angle The solution will be:
i
and the values of A and B (respectively inertia and damping): C 1, r cosfl
A =
1Iii()2 (5) B L sin fi (6)Pitch amplitude i/(J, phase lag / and circular fre-quency '' are to be measured so that A and B can be determined.
Finally, for the case of combined heaving and
pitching motion, we have the following coupled
differential equations:
cl
+ bz +
CZ + (I'/' + ("I' + '/'A '' + B; + C', ± Dz + Fz + Gz = Me""'
(7)
a, A, h, B, F and M are already defined,
whereasci, D, c' and E are the coefficients of the coupling
terms;
further:
C = ;' S, + I
C = ' l2 S + k 1- + ' K
= G = ;'/, S.,+ k 1.,
where 1, = horizontal distance between the models'
centre of gravity acid the centre of the waterplane area.
The solution of (7) is given by:
= z c'"'
,,,
Substituting these expressions, the coefficients of the coupling terms can be found:
(z1/r) ( acn + c) sin F
(z 'r) boi COS F1' + .6. SW
+
011/'i)!?+
-f-+
or (8)where ' and arc the phase lags and
;' - &
For a cheek F = "
F can be substituted
to show the symmetry in the expressions for c and F, a' and D.
Here again, the phase lags ;' and , the amplitudes
'j
and z, and the circular frequency ii can he
measured.Assuming a, A, I, and B to be the same as in case
I a and I b, the coefficients of the coupling terms
can be determined.
Test mogra Hi
The model is of the Todd 60-series parentform
with a blockcoefficient C .60.
The main oarticulars are as follows:
Length (bp)
L 2.438mB read t ft B 0.325 nm
Displacement
L=61.9
kgArea of waterline plane So= 0.561 rn2
Mass moment of inertia of
the model I 2.25 kgmsec
Moment of inertia of
waterline plane K 0.170m1
The pure heaving and pure pitching tests have
been carried out at four model speeds: FR = .15, .20, .25 and .30 (FR. is the dimensionless Froude number)
Tests at zero snecd and at FR .07 S were tried
but these did not give reliable results because of
serious tank-wall effects.
At each of the four speeds the frequency is varied
between 0) 3 and oc = 13, and the amplitude of
ti-ic eccentric between I
and 4 or
cm. At low
frequencies tile waves generated b the model mo-tions may travel faster than the model itself.
This effect combined with that of reflections
from the tank walls gives a large scatter of the
experimental Doints in the range cc < 3 (lower
for high speed and higher for low speeds of advance). Frequencies higher than cc
± 13 are not
im-portant from a practical point of view although
tile)' are of interest for theoretical work.
lit hiis range however the inertia forces ire \cr
Vfl'. (' z0/r
( y,,/r) ( _A,t -I- C) cos F ( ', r) B" Sin F
+
('i z111r
k 1, cos ;' -I--- G r
(z,1/r) ( a"r -I- c) COS F --f- (
r) b' sin i
+
(,)
.6. cos /
-1- gy r
,.;:!,/
/-- (
c'0/r) ( --fln-l-C) sin ('i '
r)B' 'c cos(I) r
+ k 1
sin '(I
large compared with damping forces and therefore a determination of the damping cannot be
accom-plished here with reasonable accuracy.
The combined heaving and pitching motion is
studied for one speed only, viz.: FR .20. This test covered the same frequency and ampli-tude range as mentioned above.
Fest results
Fig. 2 shows the test results for the pure heaving and pure pitching motion at FR. .20.
On a base of frequency w, the phase lags and /,
and the amplitudes of motion divided by the am-pl it ude of the eccentric r : z/r and j '/r, are shown. In the tables I
and 2 the ordinates of the thus
found curves are summarized for all the speeds
con-sidered.
TABLE I
A iupliliiili' aiiil Jil.)ase for pure bc'a vi u in olwii
o is given in degrees
TABLE 2
A iii />li1ol(' (1/1(1 Jibase for pure J)ite/iiui& motion
is given in dcgrccs per cm; fi in degrees
Fig. 3 shows the phase lag and motion amplitude
curves for the combined heaving and pitching
motion.
The coefficients a, b, A and B are calculated,
using the data of tables I and 2 and the formulae
(2), (3), (5) and (6); the result is shown in the
Figs. 4 and 5.
For an easy conversion to other model scales, the
various diagrams are provided with dimensionless scales; the dimensionless damping coefficients for
heave and pitch are respectively:
h ./ gL
Instead of the quantity a in -I- -, the values
of ii and u/nz are shown in Fig. 4.
and B \/ gL
AL
2.4 5.3 9.0 12.8 17.4 25.6 44 95 44 62 72 FR = .15 FR = .20 FR = .2 a FR = .30 a a z0/r a 0.519 2.0 0.527 2.5 0.518 2.8 0.512 3.3 0.539 5.4 0.553 6.4 0.548 6.6 0.539 7.3 0.568 10.1 0.592 11.1 0.592 11.2 0.576 11.7 0.624 15.3 0.654 15.6 0.666 15.0 0.632 15.5 0.722 19.0 0.759 18.6 0.770 18.4 0.721 18.6 0.894 22.5 0.937 21.6 0.919 22.4 0.902 23.0 1.226 30 1.267 29 1.192 30 1.250 32 2.318 49 2.361 47 2.150 49 2.163 50 3.166 135 3.198 129 2.890 128 2.946 132 1.335 166 1.367 166 1.306 166 1.261 169 0.774 177 0.764 177 0.753 176 0.705 180 = .15 FR = .20 FR = .25 FR -: fi 1.7 0.244 1.7 0.243 2.1 0.2 So 4.8 0.261 4.4 0.260 6.1 0.265 9.2 0.288 8.2 0.284 9.9 0.291 14.5 0.333 13.0 0.327 13.5 0.330 20.5 0.406 18.5 0.398 18.0 0.395 29 0.544 27.3 0.523 25.9 0.517 44 0.807 45 0.799 44 0.856 86 1.149 88 1.151 92 1.227 140 0.773 140 0.755 141 0.703 163 0.448 159 0.446 162 0.414 172 0.289 169 0.285 172 0.285 (I) F i1 0.241 3 0.258 4 0.283 5 0.3 33 6 0.409 7 0.528 8 0.742 9 1.138 10 0.800 11 0.443 12 0.2 92 V.) 2 3 4 5 6 7 8 9 10 11 1235-. 30-. 2.5_ 15_ 05 0 0 _150° 120° 4 -J 4
I
0. 90°-
60° 30° 0 6 Blig. 2. iea.curel Jib,, of
''''1''''
iii Jihie for Jitive /,l1,i,i au/ Ju,i'e /iiIhiiit ,,,,)IIO,,l.2 U, UJ. 06 04. 02_ I PITCH FR. 020 -r..LQcni a- 20
.- ao
x-4.0 I I A x I Ij
/
I
I
I I A PNASE AMPLITUDE I I _I80 _150° _120° 0 4 -J Ui 0. 90° 4 60° _30° 0 I 0 I 2 I 3 1 4 I 5 I 6 I Iwsc
B 9 I 0 1 T II 12 I 13 I 4 5 4 Is 3 2 10 5 4 3 212. 06. 04_ 02 C) 08 06. 0 4 02 PITCH0 HEAVE FR, =020 U- 3.0 0- 50 0 I 2 3 4 5 6 =sc
PITCH AND HEAVE
FR =0.20 £ -r -2Ocm
.-ao
0- 50 - T JO II 2 13 14 15Fig. 3 ten, ii rd 'nines sf 1 55! 1:/tIm/c and /h, for so so bi,,:/ hen: 'ins ,,,,I pIc'iin owl:,,,
-
900-
60° - 30° 800 - 150° 0 - 60° 30° 0 240° 0° 180°-
20° 0 I 2 3__i,_
-,n__--__
10 II 2 3 14 IS 6 --asc3 --40 'I' Vt ....20 /vgL B A 1% 0
OhllI,l
0 05 10 15 2.0 3-1 05 HEAVE V/kp_.l5 -I / 17I
b 0 0 2 3 4 5 6 7 8 (J-_ flC 9 10 II 2 13 0I0/
15 20-sL
.//
---HEAVEV/v3O
-'-5 -- 9 - 40_ / -\ - - - S 3_ -A -7-6 .0 0 o 2 3 4 5 6 789
0 II 2 3 o as toF IS'I
2.0 9'tc m 40--- -V/ HEAVEI23
67S9 0
II 12 13 0 05 10 5 20005-.
:
I,/fl
B I0-3
I Q5 0 I I T 2 3 4 5 6 7 (aJ -SC -8 r 9 0 II 12 3QSLO
S 20 o o o. 0 15 20 010 I-Q05 F 9 a PITCH V/11 -20 _I.O .25 II"I
I . 4-.I'
N
/
10 0 0 o I 2 3 4 5 . 6 7 r B 9 tO r II 12 3 o 05 10 2.0 0101 F 9 -PITCH S F 1.0 -\\1
/B
1'\._
0 0 0 I 2 3 4 5 6 75CC
9 10 II 12 3 0 (5tOtiy
5 20Ig. 6. CorfJuii'n Is of cou/ilin /er7sls for eon,Io,,rI be, /s a,,1 JiiIehiii ..J k9sc 008- - 10-0.04- 0.6 - D +1 +1
-0 -0
- d - 1CALCULATED004- 0.6-
d:D - 1.0-0.08- 1.4 -I I I 5 I I I I0
I 2 3 4 5 6 7 8 9 10 II 12 3 (a.) SEC' I I I I I [ I I I I I I j I ¶o
0.5 .0 1.5 2.0::
0.6-kqszc 'j 6 -0000 \CALCULATED0
II I 2 T 3 I 4 5 I I ¶ 6 7 8 (A)-
SeC I 9 I 0 III I 12 I 130
I I I J I 0.5 I I j I I 1 I .5 I I I I J I 2.0 I I I .0Similarly Fig. S shows ii,
ud /'d/I instead of
A = I +
ii.
As the quotient i/1 depends on the distribution
of weights in the model (I) and not on
hydrody-namic properties, thc value of I in the denominator is taken as I (0.2SL) in instead of the actual I
of the model.
As a dimensionless frequency parameter (I;
where B breadth of model, is taken.
\Vith the data of Fig. 3, the now known
coeffi-cients a, I,, A and B, and formula (8), the coeffi-cients of the coupling terms e, F, d and D can be
d etc rm in ed.
These ire plotted in Fig. 6 on a base of frequency.
Ihe d llleflSiOIl less scales are foti nd by multiplying
g
I and
D withA and e, F with
Discns.siu,, (If the results
As mentioned above, the results for very low
frequencies are not reliable. In this range, the waves
generated by the models' own motions may travel
faster
than the model
itself; conseq uently, themodel is not oscillating in calm water, but in her
own waves.
This phenomenon causes a large scatter of the
experimental points, particularly the measured phase
lags are very sensitive in this respect. When the
generated waves travel faster than the model, the
relation between speed of the iiioc1e1 .ind period of the oscillation is given by:
2iV
< ¼
where: V model speedT = period
as shown by Brard 17].For the model in question we find for the
limit-ing case (see table 3):
TABLE 3
2. V/'T= '/
ALAt a speed and period given in table 3 the
dis-tortions of die fluid surface do not cover the area
.ahead of 1ic model.
This relatioll is verified experimentally and good
agreement is found. Also reflections from the tank
walls are important;
it isthought that even at
slightly higher speeds than given in
table 3 (orhigher frequencies) some in fluence exists, but a
quantitative knowledge of the effect is not at hand.
Furthermore the phase lag is small at low
fre-quencies and an error of some degrees affects
con-siderably the accuracy of the coefficients h and B, as can be seen from formulae (3) and (6).
In general it seems advisable to disregard the
surements in the range m < 3 or 4.
The influence of speed on added mass and added
mass moment of inertia is shown in the figures 4
and 5.
For t" > 6 a five ocr cent. variation, with respect to the mean value of a
in +
ii. is present.Simi-larly, a three per cent variation in the value of
A = I + p, is found.
In both cases this variation due to the speed of
advance is less at higher frequencies.
The damping coefficients also show some
depend-ency on soeed, see Fig. 8. To study the combined
effect of speed on damping, mass and mass moment of inertia, the magnification factors and determined
for the pure heaving and pure pitching motions
(see Fig. 7).
In the case of pure heaving motion, the influence
of speed on the magnification factor is fairly large
for " < 7.
It is remarkable that the curves for FR
.15and FR .30 and those for FR = .20 and FR .25
coincide.
in the case of pure pitching motion, one curve is
valid for all model speeds, except at resonance. In both cases a mean circular frequency: w 7.05 is found at 90 degrees prase lag, corresponding to a
natural period of T 0.89 seconds for pure heave
and pure pitch; the mass moment of inertia of the model is taken as I = in (0.2 5L).
These periods agree with those found from in-cl ii n g tests; it must be mentioned however that these latter are difficult to measure.
The maximum values of the various terms of the
differential equations give an impression of their
relative magnitudes.
For the case ') 7 and FR .20, table 4 gives
the necessary information, assuming unit displace-men t.
(1 meter of heave and I radian of pitch.)
TABLE 4
P) actual value of model
FR 0.075 0.15 0.20 0.25 0.30 o 6.7 3.3 2.5 2.0 1.7 heave pitch
= 565 kg
= 164 kgm')
216 kgB"i =
51 kgm C. 561 kg C= 172 kgm
'--16 kg
D-' =
2 kgm ('I')=-61 kg
Em =
11 kgm=-32 kg
G=-32 kgm
Fig. 7. Ala.ii)i',Iion fiIors JHI 1,11,' /,e,, iut i,,? /?urr /ü/iIiin ,,zoiIi,,i 2
0
HEAVE
Fr.I5
//
//
/
/
/
'.. PHASE
N
800 0 50 20° 90°-
I
a. 3d 0 Fr.2O Fr.25 Fr.3O .___--
-.-/
/
0
2 3 4 5 6 8 9 U..) _- sec0
II 12 0 I I 0.5 .0 1.5 2.0o
z
0
I-(.90
PITCH
12 Fr=f2-
180° I50 _120°_90°
dDFr.30_._
//
/
. 4.PHASE//
/
/1/
//
0
234
5 U) 6 7 B 91011
120
0.5I I I j .0 - .5 I I I 2.0/,f,iiI!JI,II.l UU/ lii l'/' /lP/'/ 1 /I,.J 11l I' I Jo i,tiii,iI llII) I o. I ci 0I so
0
i I I I I i i I LI I II 01 6'8
Ths,..'f)
L 9 S V £ 10
\.
E 9-L
- 6500
- -010\
0 0 0 F/
/
OE J 0 d SI-'.d 00 000 000N
/
1
-
H.LId
013 SI 01 500
I I i I i i i j I j LI I II 01 I - 6'9
I DS C) S I V £ I0
I 9----
L I N\<\aiv1nD1vD
:E1
0 w $ OS --
0Ed
0d
''-'
/
0 -Sikd
AVH
DIt may be concluded from table 4 that generally,
the coupling terms are not negligible.
Particularly their influence on phase lags may
be important as mentioned by Korvin-Kroukovsky [4].
Haskind derived from theoretical work the
fol-lowing relations between the coefficients of the
coupling terms of a symmetrical shipform (see also
[1]):
cE=d=D0
for V=0
and:
.- ti,
1 forV / 0
The last mentioned relation is confirmed qualita-tively by our experiments for a' and 1) although the actual model form has some asymmetry (see Fig. 6).
Finally, the linearity of the motions seems well
established for moderate amplitudes of motion (see
Figs. 2 and 3).
In any case, the use of the linear differential
equations may be regarded as a good approximation. The coefficients, found experimentally, are
com-parable with those calculated by
Korvin-Krou-kovsky [4].
In [4] a comprehensive account of his calcula-tions is given for a 5 ft. model of the same lines.
As for the details the reader may be referred to the paper concerned. The method used for the cal-culation of added mass is based principally on the
well known work of Lewis, whereas the calculation of the velocity dependant terms is based on work by
Holstein and Havelock.
The results are summarized below:
--I/ L
=
l .c.sI1
-
111 L + 1/2L u J Sk9Ed - 2/2 L - 1/ L1D=k1
L'i
SI.''SI - /2LS the sectional area at a distance from
mid-ship section;
= the coefficient of accession to inertia
forthis section and
k a coefficient for free surface effects.
The resulting dimensionless parameters are:
Dg
AL
AL
- 0.02!
ii. ni - 0.85,
/1,/i
0.75 andThese values may be compared with the
experi-mental results in Figs. 4, 5 and 6.
The calculated "/n' agrees fairly well with the
average experimental value, except at low
fre-q uencics.
This
is not the case with the calculated "
Iwhich apparently is too large ,w hercas the calculated coefficients ii
and D are only comparable when
only the order of magnitude of the absolute values is considered. The coefficients of the velocity dependant terms, Ii, B, e and F are calculated withthe following formulae, using the well known strip theory: -I- I/ L - - I: i + / L .1
N()I
- '/ L -4- iI I, eF =
.1N()Sd
-
2/2Lwhere N () is the damping force due to unit
ver-tical
velocity. The expression for N ()
is givenin [4].
Good agreement is found for damping in heave
(sec Fig. 8) except at high frequencies.
The damping in pitch shows significant differ-ences between calculation and experiment (see Fig. 8).
In general a qualitative agreement with
Have-lock's calculation for a submerged spheroid is
found [8].
Havelock determined the damping in heave and pitch for a submerged spheroid with the aid of a two dimensional strip theory and with a three
di-mensional theory.
It was found that the strip theory is valid for
heave in the practical range of frequencies, whereas for pitch a correction factor is needed which is < 1 for low frequencies and > I for higher frequencies.
Finally the calculated values of e and £ arc also given in Fig. 6. Here again the order of magnitude
is correct hut no fu rtller ag recmcii t is fou n ci
Lis/ of niuli, s1',,,hoI
hreadth of model
C,, blockcocfficicnt
jJ( = Froude number = V./ gL = acceleration of gravity
I = miss moment of inertia of model K = inertia of waterline plane
= spring constant
L length of model
in = tiass of model
r amplitude of eccentric
S1, area of waterline plane
where k, = 0.75
where
k, - 1.20
1 period of excitation
V = spccd of model = displacement of heave
amplitude of heave
a, fi, ,', = phase lags
= displacement of pitch
lash toil, M. I). a rid Riema,,, I. S.: "A met hod of deter ni ii rig
pitching and heaving characteristics of a ship". Bulletin de
lAcadinije des Sciences tIe URSS, Classe des Sciences
tech-niques, 1946, no. 10 (translation Russian-1)utcl, by ir. G.
Vossers)
2 c;olorrilo, P.: "A study of tIre forces and moments on a surface
ship performing heaving oscillations". 1916, 1'.M.B.,
report nr. 1074.
3, lVeinblu in, G. and SI. De,,,,ji, M. "On tIi niot ions of sIr ips at
sea". S.N.A.M.E.. 950.
Korsin - K rook ossky, Il. V.: "In vestigat ion of sIr p iirtt ions in
regular waves". S.N.A.M.K., 1911.
5/. Denii, 'ii. and Piers,,,,, W'. I.: "On t lie iiiotsons of ships in confused seas". S.N.A.M.E., 1913.
Grin,, 0.: " Berec liii u ug de r do rcls Sc hw i rig u ,,gcn ci nes Schi ffs
-korpers crzeugi er I, ydrod yrrr,,iiscIrcn K r.i ftc'', .S.T.G.,
1913.
l3raru!, l(.: 'Introduction i l'tudc th,eorlquc dir t.sngage en
niarche". AIMA, 1949.
llarIork, 7'. 11.: "'YIie dau,,isu,g of Irc.ive and pitch; a
conipiri-son of t wo-d iniensio,i.r I .r rid ti rev-dimensional calculations''.
T.1.N.A., 1916.
Ref ereizees
'Iii amplitude of pitch
H. = added mass
= added mass moment of inertia
= displacement of model
2r
(I) = circular frequency