ARCHIEF
Lab.
y.
Scheepskouwkuride
Technische Hogeschool
Deift
Introduc tian
The presant per presents a general form of the relatirnships between the characteristics of f lova around a ship among waves in direct and reverse f lova, within the limita
of linearized hydralynanitca.
Theorem (I)may offers a systematic
moans of obtaining approximate
solu-tIons for the problems in the
anti-symtric motions of the ship as *n
wing theory Theorem (It)is nevly
introduced in this per and it is applicable to the calculation of over-all forces acting on the ship. SOEne
interesting results are obtained by virtue of ita application, which are likely to be of practical values List of Symbols
Cartesian coordinates vith the origin o in the free surface of deep water, and oz vertically upwards, and
ox in free stream
direc-tion of direct flow free stream velocity length of the ship
time and circular frequen-. cy of oscillation,
respec-tively
Y linear displacements of each point of the ship
Z,., Z,.,- surface elevation of
regil-lar waves and its
ampli-ti.ide
j)L)ÇL,,.21%.vave nunber rate and
wave length of regular ve, respectively
X
heading anglesurge linenr displace-.
monts of the ship'o
e'
sway centre of gravity along the Z,,and heave z-axes52l/L,
2S/L ,te't angle of roll (angular
-
displace-e = -8displace-e" angldisplace-e of pitch monts about the e"
angle of yaw L, Y, and ¿ -axes) - 22 -ßA.,P4, f3., /3g. I3, /
4=
40eÌJ t0e"
1,
'
QX,.
Wv'
phase lag of surge, away, hsave,roll, pitch, and yaw respectively, behind regular waves at origin acceleratjon cauaecl by
potbntial xeaanee of velocity
f the 3hip
potential J
density and pressure change respectively, associated with «
'acceleratioxi of gravity
projection of the vertical-median plane intoX.E-planee § 1. Bc*indary Condjtjn and
P&d.ro-dynamic Forces Acting on a Shj Amon 'kLvO5
When a ship is slender, we may
asse that boundary condition la
satisfied, instead of on the hu.U.
surface itself, on the projection of this surface
into
the x.pi,ane,within tho frame of the linearized theory When the ship's form is
given by y z,i), the boundary
condi-tion written as
-$
-&
-ere+j
x.- X,, = -7 et,
Y=
-i-ii' tyv.x
(1,4)
and X.,, y.,,, z1,,denote the
Instan-taneous linear displacements of fluid particle due to regular waves Hence,
the complex amplitudes of relative displacements are given by
.Z,'
"x
e' -e'v
-.,,
When the, boundary condition is
symetric with respect to -plane,
the corresponding velocity and
acce-leration fields are symiiOtrio
Smi-lar].y, when the boundary condition is
anti-symmetric with respect to
X-plane, the corresponding velocity andProceedings of the 9th Japan National Congress for Appi. Mech., 1959
III-9. On the Reverse Flow Theorem Concerning
ve-?kthg Theory Thtsuro Banao z
V
Lt,
,acceleration fields are anti-symmetric. ibsequently, symmetric motions do not cause the ship to be acted on by any
anti-syisne trie force Reciprocally, the similar relation is settled in case
of anti-sy!mnetric motions. Therefore,
we see that hylrodynanic coupling forces are negligible. Hence, we classify the ship motions among ves in tuo kinds of motions: one isa longitudinal motion (symmetric motion), that is surging, heaving and pitching
oscillations, axiçi the other is a
later-al motion (anti-iytnmetric motion), that is swaying, yawing and rolling ose
tUa-tiens.
We show the expressions of vari-aus kinds of the hydredynamic forces an& moments acting on a ship among
waves ., These are needed for the
cal-culatton of the motion of a ship among waves.
The acceleration potential is available for the calculation of the flu.id f orc We can divide the accel-eration potential into the respective
part of the ship motions - the
dis-turbances due to surging, swaying, heaving, rolling, pitching yawing, and distortion of ocean waves caused by presence of the ship. If these are designated by ,.
+,'J+,,QA
and+,
the whole acceleration potential is given by(1.6)
where 4. and $ denote the symmetric and anti-symmetric parts cf + with respect to r -plane respectively.
The hydrodynainic forces are divided into the respective rts of the ship motions by refering to (1.6). We
classify them in two groupa to contri-bute to the longitudinal and lateral motions.
(i Longitudinal motion. If we
express the hydrodynamic forces and moments by the symbols,
Ç- r
r
4jr
forceA-ÀrA,4Or.,
,j heaving forcepitching_f
moment -0Fe ¡F
_(& where-;1e'-'s
_e"
-C-: _ei0t)F-Af(1.7)
and F,... - - - are complex
nbera and the real parts of the
right-hand side of the aboye expree-aion are to be taken, they are given
(ji lAteral motions We ex-press the hydrodynaiuie forces and moments by the symbols,
F
force rolling
moment r-Çr 'cF, UFqg (iou) yuwl.ng
moment
-- e'' where
Nov we introduce the pressure differ-ence ir. between right and left sides of the ship's surface (right side corresponds to the positive -axis).. If ,and t,. denote the values of 4'. on
the port and the starboard, the
pres-sure differee between both sides is
written as
ir. ?(+.,-t,) (1,12)
We can also divide ir0 into the respec-tive part of the ship motion.
The expressions
of
the forces are written as: -' -1T,. 224-t
- ¿5t;'
te dzd
(1.8)
s---;
F - F ¿ -;i.
ta
t.
da
(1.9)
Fo,-'ë
F8 -&S F, _2'jJ+.
t,
dxÀr
(iio)
-F,.
- F.. - F,, - ir.,-ir'P
(1.13)
--'ç-.-i F,.
1fr.
(1.14)
- F, )J Tt,,fT
- i/c.
ir0
t.
2
Rever.e Flow Theoreznc
There i. the relation
4'.=.- 1'/ -.
at
between acceleration totemtial
and
f luJ.d pressure p
. whre
is the
elevaiori of free surfFxce due to
d.ts-turbance.
If we take the novtng
coord.nate sytes advarcing with the
shIp, we have the cese of' e current
flow with the general velocity V or4
past the shIp along x -axis according
as the ship advances along the
nega-tive or onsinega-tive x-axis0
Weay say
the former direct flow and the latter
reversa flcw
If we Introduce an
artificial force
oportional to the
fluid vel.city into the fluid field
acooring to Rayleigh, the relatIc
between the veloctty and acceleration
potentiaì
occse
+.=
:: tp- V
L
within the 'eatr l.ction of linearized.
theory, where ¿t denotes the coeff
i-cent. cf the artificial resisting
force0
Both
and
satisfy Laplace
equation and the condition& to be
satisfied at the free surface are
face and the ship' s surface and its
locus in both flows and the surface
to close the fluid at infinity, the
l.15)
volume-integral vaniahes, because
I.
and 4.
satisfy laplace eqLkttion.
If
be fi-ite, 4. and 4 vanisi
atinfinity.
Renca. we have
(2.2)
(2.3)
at
= Owhere
and
denote the
correspond-ing quantities for the reverse flows
The reverse flow theorema are
based upon Green's theorem,
(2/.)
Theorem(I
-We write
, in place of ' and 4. in
pl.ce of i
The vçj].ujne- integral is
taken throuehout the whole region
occupied by the fluid and the
surface-integral
ver Its hounder.
In
g6ner-al, the potential ftnctIn
is
dis-continuous on tre locue of the ship's
surface.
Therefore, if the
surface-th.egrel is taker, over the free
sur-- 225
(2.5)
lo.
where ., is the ship's surface and
its locus in both flows.
On substitut ing (2,3)
andper-forcing partial integration
in x
the surface integral vanishes over
the free surface,
When we wabgtitute (2,2)for 'P. in the first
term of (2.5)and perform a partial
integra-tion in
, wo baie
(2/,)
(i
Longitudinal motion,
. and
are synmetric with respect to
xi-plane.
Then we have
IIt
''4 o j'J
(2,7)
(iii Lateral notIoi
4,
andI/n are anti-syonetria with
re-epect to x -plane, and il. and L.
disappear on the locus,
Then we have
*
(2,8)
This is the samd one with the
re-ciprocity relation in wing theory,
Theorem tII,
If t=10 and
in (2,4), webave
(2.9)
In +.he following anályaea, we must
notice that the frictional
coeffi-cient ¿k'
is taken to bs infinitecii.1
in final aoluttcns.
i. LongitntTh1 motion.
As t.
and-4. are sysetric with respect
to i? -plane
and diaaçeareon
the locus, we obtain, fron (2.9)
(.1o)
Substituting (1.1), and performing
partial integrations in x , we obtain
a reciprocity re].atiou as
(2,11)
ji. lateral motion.
Asand
ara anti-syzisietric with
respect to x
-plane, we have
= of
When we subatitute°''î.l) and then
7oj
(2.1)
Let
Let
and
Q'
Then we have, from (2.11)
226
-¿ f( el'dtt4. 1 If
-ijijt*".,d1GtZ
Using (3.1) and (i,e), we get
F,.z
By 'following the same procedure,
we obtain the relations between the varions kinds of the forces and nonante as shown in Table I.
Fron the above ana]ysia, we see that, if we have the pressure distri-butions due to swaying, rolling and yawing in still water, we can obtain
the exciting forces by means of a closed-form integral over the pres-sure distributions.
B,b1tcrathy
i) Flax, AFI., General Reverse Flow and Variational Theoreme in
Lift-ing-Surface Theory, Journal of the Aeronautical Sciences, Vol, 19,
No 6, pp361-3?4, June, 1952.
2) Hariaoka, T,, Theoretical Investi-gation Concerning aip Motion in Regular Waves, Netherlands ip Model sin, Symposium 1957, PP.266-235
(Member of Zosen Kiokai.
Transportation Technical Researc
Institute.
/
Coupling forces
F = -
L
FF
- '
F
-¿Ø
L 8&
- L
8k
-surging
rIJ$;t»0'X'
f)e'd.z
heaving
Llfj[('
*1(
pitching
O
Coupling forces
Ea- =
Ç
-
F«
-n
swaying
F
.-r
-
-'
J)'rre
rolling
LxiJ.ure1ti
1F
e"'°
=
-JJ
perform partial integrations in x. , we
obtain
JJ
w2zJf
(2q12)Ç 3. App..i.cations of the Reverse F1v Theorems
In the following analysis it is assumed that the ship is symmetrical
fore and oft. en the ship is maidng oscillations, there are the relations, between the acceleration potentials on the ship' s surface in direct and
re-verse f lows.
(x?)
t6tz,a)
W. -.
(3")
f,.t*x)11.i- xi)
iiii',
xë and
_ &-Then ve have, fron (2,11) and (3.1)
k
«g
Using (1,9) and (1,lO),we get