1.
Introduction
Estimation of the flow field and the hvdrody-namic forces of an obliquing ship is important to grasp mainly the manoeuvrability of a ship
and many investigations were performed. As to
the estimation of lateral force, Fuwat) Mizoguchi2' and Matsumura et al showed
methods to use the separated vortex and the slender body theory, and these methods are
now in practical use in the still water surface. From the observation of ship-side wave profiles. however. Matsumoto et al41 reported that the local wave effect near the bow appears
clearly in che lateral force distribution. Then in
order to estimate accurately the hydrodynamic forces
acting on an obliquing ship,
it is necessary to take account of the free surfaceeffect in such calculation.
Nishiyama treated the lateral force of
ellipsoid from the standpoint of the linearized
wavemaking theory, and Hanaoka and
>onaka investigated the lateral force of thin
Kvushu tíniversitv
Kawasaki heavy Industries. Ltd.
103
wing under the wavemaking effect. Recently Hon et al8' presented a method based on the low speed wavemaking theory, and Song91
obtained the wavemaking lateral forces and wave patterns about an obliquing ship based on
the newly developed slender body theory, and
moreover Xia-Larsson10 presented a method
to use vortex distribution on the yacht hull and
Rankine source method..
This paper presents a method to calculate
the flow field and the hydrodvnarnic forces of an obliauing ship using vortex distribution on the hull
center plane and Rankine source
method on the assumption that the ship hull. is a thick wing of small aspect ratio.
2.
Basic Equation
We describe the basic equations to represent a ship hull advancing straight with a speed V
and a drift angle '. As shown in Fig.1. two kinds of coordinate systems are used. One is O-xyz coordinate system fixed to ship hull and the other is O-XYZ coordinate system fixed in
space with X axis in accordance with uniform
flow V Then we assume the potential flow
Deift University of Technology
Ship Hydromechanics Laboratory
Library
Mekelweg 2, 2628 CD Deift
The Netherlands
Phone: +31 15 2786873 - Fax: +31 15 2781836
s. On the Flow Field and the Hydrodynamic Forces of an Obliquing
Ship
Kuniharu NAKATAKE, Member Atsushi KOMURA* iVIember Jun ANDo , Member
Katsumi KATAOKA, Member
(From T. WestJapan. S.N..1. Japan. iVo.80, .4ugust 1990) Abstract
This paper presents a method to calculate the flow field and the hydrodynamic forces of an oblicuing ship under the free surface effect. We treat the ship hull as a thick wing of small aspect ratio. Ship hull is represented by the source distribution on the hull surface and the vortex distribution on the center plane of the hull. The strength of these singularities are obtained from the boundary condition on the hull arid the Kiittas condition. In order to obtain the wave flow, we use Kvushu University method. This is a kind of the Rankine source method and does not use th finite difference operator to satisfy the radiation condition. Since the flow field is calculated using these singularities, the wave pattern, the pressure distribution and the wavemaking lateral force and resistance acting on the hull are obtained. Using this method, we calculate the flow field around Wigley hull with drift angle. The wave pattern
and the hydrodynamic forces are compared with the experimental results. The agreements are
104
Kuniharu ìAKATAKE. Atsushi KOryIURA, Jun ANDO, Katsumi KATAOKA
z.z
V
_---;----..---.-.. -..--.
-.:--.
...-:.
Fp
Fig. 2 Bound vortex distribution
F.p.
A.P. Fia'. io Coordinate systems
around the obliquing ship hull and denote the
flow velocity vector around the hull by q and
the uniform velocity
vector by qu
In order to express the flow field around the
obliquing hull, three kinds of singularity
distributions are utilized. One is source distribution m on the hull surface to express the hull shape, second one is bound vortex '7
distributed on the ship center plane Sv with
constant strength in the longitudinal direction
and stepped strength in the draftwise direction,
which represents the lifting action originating from obliquing (vide. Fig.2) From bound vortex distribution, there should exist trailing
vortex which, we assume, sheds from eachstrip with angle to infinite rearward (vide Fig.3). We call above vortex system the nonlinear vortex model in contrast to the linear vortex model (i.e.
=0). The third
one is source distribution °pon the still water surface Spto express the free surface wave.Then we denote the velocity vectors due to singularity distributions m, 7 and F by q5, q and qp, respectively, whose mathematical
expressions are given in Appendix. m and 7
qn=0
(5)A.?.
Fig. 3 Vortex system on one strip
are assumed to be splitted into two parts, i.e. m0 and 'fo which represent the double-model flow, and m and 7 which do free surface effects. That is,
mm4j±m,
77±7
(1)Then total velocity vector q is written as
q= q0 + (2)
where
q0q±q+q, q1q.q5q1
(3)In Eq.(3), q,.o, q,.,o' qi and q1 express the velocity vectors due to singularities mo, 'fo,
mand y, respectively. Here, we represent
the vector component in each direction by each suffix, for example, in case of q, (q,., qy, q) are
components wich respect to 0-zyz coordinate
systems and (qx, qy, qz.) are with. respectto O-XYZ coordinate systems. Then, among above components. there hold the following relations.
/ qx
qy
\qzl
/ cos
= sin!?
sin 9coso
0
/q,.
o qy (4)
1/
\q,.J
Next we deal with the boundary conditions to determine the singularity distributions.
Firstly, the boundary condition on the hull
surface S becomes
where a is the outward normal vector to 5. Secondly, as the Kutta's condition, we adopt the equal-pressure condition on both face and back sides at the trailing edge. namely
Lastly, on the still water surface, we satisfy the double-model linearized free surface condition given by DawsonLi). Expressing this condition
using gravitational acceleration g and O-XYZ coordinate system, we havi
A.p
(six
( Six
ai
ax
)
qoxqoy a y a x 7(aqiy
qoy aqoyix
2 oxax)
ax)
Hqav(
/ aqoyqy±gqz
/ioY\
a)
aqo±
J 2(
aq0 go xo y a Y 1qoxax)
ao
)oY
2(
ao
aori ZO
(7)After obtaining the singularity distributions
m, '7 and Ffrom Eq.(5) through Eq.(7), we calculate the wave elevation ' the wave
resistance R, the wavemaking lateral force RL
and the wavemaking yaw moment M about the
OZ axis by the following equations.
= (V2qxqy2qoxqix
2qoyqiy)/(2g) (8)R=
-
ffSg (pk) nS
RLff(p)nydSs
SgM ff (pk)
(y±x)
d55 (9) whereppo=0(V2
q2)/2
In Eqs. (8) and (9), we define water density
the force acting in the dYrection of the
uniform flow R and the force acting in the perpendicular direction to the uniform flow RL.
The word "wavemaking" indicates that the
forces include the free surface effects in
addition to the forces due to the doublernodel
flow.
Calculation Method
At first, assuming the free surface as the
rigid wall, i.e. qi = O, we obtain unknown singularity distributions rn0 and 'fo from the
hull surface boundary condition Eq. (5) and the Kutta's condition Eq. (6) - Though rn0 and Yo are included in Eqs. (5) and (6). we can not
solve both equations at a time because Eq.(6) is nonlinear equation. Then we obtain mo and
'7o iteratively using Eqs. (5) and (6) until
converged values are obtained. Yo is obtained
from the Kutta's condition making use of Newton-Raphson method.
Next we perform the calculations taking into account the free surface effect. Since rn0 and Yo
are known, unknown values are m, 7 and
0p which should be obtained by solving Eqs. (5) and (6) and the free surface condition Eq. (7). Assuming at first m and y as known values, we obtain F making use of KUM (Kyushu University Method) 12) Then using known p, we obtain m and '/ iteratively
as before. After repeating above procedures several times, we obtain converged values of
7 and
p.Lastly, we calculate the wave elevation, the wave resistance. the wavemaking lateral force
and the wavemaking yaw moment from Eqs. (8)
and (9).
Calculation Results
We perform numerical calculations for
Wiglev model whose half breadth y is expre-ssed as
BI
72x211
(z21
Y'L)
1)
where L, B and d are ship length, maximum breadth and draft, respectively, and B/L=O.1
and d/B=1.O.
At first, in order to check the validity of thick wing model used in the present paper, we calculate the normal force of the wing of small
aspect ratio and thickness in the infinite fluid domain and compare the experimental results13) which were for the rectangular plate
wing of aspect ratio 0.2. Since our thick wing model cannot cope with complete plate wing, we
(lOI
r-106
Kuniharu NAKATAXE. Atsushi KOMURA, Jun .Ao, Katsumi
KATAOKA
adopt the thin wing of thickness ratio B/L
0.02 and the aspect ratio 2d/L=0.2. Fig.4
shows the comparison of the normal forcecoefficient c.,(=N/ 0.5
p V2 (2 L)}N:
normal force) of this wing against the drift angle ¡9 . In Fig.4 the experimental results'3 and the results calculated by the linear modelare also indicated. In case of small aspect-ratio
wing, we know that the present nonlinear
model is more suitable for the normal forcecalculation of the wing. Next we calculate the
flow field and the
hydrodvnamic forces ofWigley hull taking into account the free surface
effects. The mesh division of the hull surface
are 44 divisions in the longitudinal direction
and 10 divisions in the draftwise direction on
both sides as shown in Fig.5. The still water surface is also divided into 35 divisions in the main stream direction and 20 divisions in the
lateral direction, and Fig.6 illustrates the mesh
Ø: preet ieUiod LLneac-ode! ci.'
°5r
00
F.P.-: Expriiea
10.0 20.0 30.0Fig. 4 Comparison of normal force coefficient
Tz X
Fig. 5 Mesh division of hull surface
z
A.P.
division in case of j9 10°.
Then we show the singularity distributions obtained by numerical calculations in case of
Froude number F,0.267.
Fig.7 shows thesource distributions of the ship hull advancing
straight and
we find that the wave effect
appears near the bow. Fig.8 shows the source distributions of the ship hull advancing with
drift angle
9 = 10°. With
drift angle, the source distributions differ between the faceand the back sides and the free surface effect appears near the bow. Fig.9 shows the vortex
distributions on the ship center plane in case of /9 5°, 10°. We learn the vortex strength in-creases with increase of drift angle and decreases a little in the calculation with free
surface effect. Fig.10 shows the source dis-tributions on the still water surface in case of
¡9 10° and we find the source strength on the face side becomes larger than that on the back
side.
In Fig.1 1, thewave patterns are displayed at
U*
,uuauu
uwuum
--e
Fig. 6 Mesh division of still water surface
l-0 A.P. F.P. F?. -0.2 -0.4 -0.6 -05 -,.'... -l. Exclu n Fr,. jrl.c. Ef c nclulri Frs. Sczrfac, Effect
Fig. 7 Source distribution on hull surface (F=0.267,
r
-1.0
ER
c.
On the Flow Field and the Hydrodynarnic Forces of an Obliquing Ship 107
4r 22
i, 2. 1.8 1.6 1.4 1.2 1_O 0.8 0.6 Face Side Exc ud i ng ER V -20 t -22. Back Side Free Surface Effecto
1 -1.0
Fig. 9 Comparison of bound vortex distribution
-0.6 -1.0 -1.2- -1.4- -1.6-rny -1.8- -2.0--22. z 0.0 Face Side Including Free
Fig. S Source distribution on
0.05 -4,c.y/V 0.1 hull Surface -z--d surface 0.0 Back Side Effect (F,=0.267, 3 =10) 0.05 - 47t y/V 0.1 ox ox cx cx oc ß=5. X Exctudin $ =10 cx cx cx
d
cx Free Surface Effect
Oc
Oc Including cx
108
Kuniharu NAKATAKE, Atsushi KOML'RÂ. Jun ANDO, Katsumi KATA0KA 02
0.1
0.0
0.1
0.2
Faca SideFig. 11 Comparison of calculatedwave patterns (ß =
0, 5°, 10°) 0.2 0.1 -0.0 -.
0.1
Fiz. 10 Source diszributon on still water surface ( =10°)
FQ.267 in cases of
9 0°, 5°, 10°, wherethe solid lines and the broken lines express
elevation and depression of wave height. respectively. With increase of drift angle, the wave height on the face side becomes larger
and, ori the other hand. the wave height on the back side decreases. We think these
phe-nomena agree with real ones. Fig.12 shows a
comparison of calculated wave pattern in case of 9 =10° wich the experimental
one. The
positions of che crests and the troughs of
calculated wave pattern almost coincide wich the measured ones.FigJ3 shows the pressure distributions on the ship hull surface, where the solid lines
c_l Cu ti
Fig. 12 Comparison of wave patterns =10e)
L.
Sack Side
1.0-o Face Side Back Side cace Sice
T:TT;--;;
show the positive
pressure and the broken
lines show the negative pressure. We learn thathigh pressure zones increase with increase of drift angle and the free surface effect appears near the bow.
Lastly we describe about the hydrodynamic
forces and moments which are obtained by integrating the pressure distribution on the ship hull
surface. Fig.14 shows the
wave resistance coefficient Cw(Rw/0.5 °SV2, Swetted surface area) at ¡9 0 compared with
experimental vaiues1 . The agreements of both values are satisfactory. Fig.15 shows the wavemaking lateral force coefficient CL ( RL/0.5 °SV2, RL: wavemaking lateral force)
in case of 9 50, 100 and F'ig.16 does the
wavemaking yaw
moment coefficient C(=
dO
ZO
-EdD.,,,..,.,A
Cw. ._CaIe.j0,
Fig. 14 Comparison of wavemaking resistance coefficients
A.?.
Fig. 13 Calculated pressure distributions on hull surface
s
2.0 x1O 4.0 CA. 30EaeIudIr' Fe.. rf.ce t1.ct
InIiin F.. S..i,f.e. EU.ct
to
M/05p V2L2d, M: wavemaking yaw moment).
In tfiose figures. we indicate the values calculated for the double model flow. The free surface effect gives rise to fluctuation of CL, C1 with change of Fraude number. In order to examine the calculated results, we indicate the
experimental values°
at F=0.181 and we
know present calculation method gives the near
values o experimental ones on the whole.
LSi(F,..O.1t.3.tO' )
3
-Eaa.rIeflt 1S)(,,,_o.11..ß-5 I
Fig. 15 Comparison of waveoì.aking lateral force
coefficients
On the Flow Field and the Elydrodyriamic Forces of an Obliquing Shtp 109
Back Side A.?. Y.?.. Sack Side A.?.
Y.?.
Face Side A.?. Y,?.
Face Side A.?.
A.?. T.?. A .P.
0.20 0.2 0.20 Ft, 0.3e
0.20 025 o-30 . - F1, 0.35
Y.?.
Saca Side A.?. Y.?.
Sack Side A.?.
Ezc(uding Free Sijrface Effect
Including Free Surface Effect
ß S de A.?. Face Side A .P. Y.?. 3 =0 [7/(í Y r. Y.?. ß=5.
r
110
Kuniharu NAKATAKE. Atsushi K0MURA. Jun .ANDo. Katsumi KATAOKA
to
S-10.
S
-5-0.20 0-25 0.30 Fn 0.35
Fig. 16 Comparison of '.vavemak-irigyaw moment
coefficients
5.
Conclusion and Acknowledgement
In order to obtain the flow field around the ob!iauing shiDhull and the hydrodynamic
forces, we proposed a calculation method to use a thick wing model for a ship hull and a kind of Rarikine source method to take into account the
free surface effect. Then we showed that
calculated results seemed to be reasonable and our method might be useful for such problem. As to the quantitative agreement with experi-ments, we must check for another ship formand improve the calculation method, for example, to treat with the trim, sinkage and
healing.
We wish to express our sincere thanks to Mr. Kokichi Oda and Ms. Keiko Matsuki for
their work to complete this manuscript.
This research was partly supported by the Grand-in-Aid for Research of the Ministry of
Education, Science and Culture. Further we are deeply indebted to the staffs of the Large-Sized computer Center of Kvushu University for their work using FACOM M780/20, VP-200, 0S IV/F4.
R efere n ces
i) K.Fuwa; Hydrodynamic Forces. Acting on a Ship in Oblique Towing, Journal of the Society of Naval Architects of Japan,
.Vo.L134Dec. .1973...
... 2)' S.Mizoguchi;Calculation of Flow with
Three-Dimensional Separation Vorticities around Ships, Journal of the Kansai
society of Naval Architects, Japan. No.188, Mar. 1983
K.vÍatsumura; LTanaka, T.Oki, S.Kishi; On the Nonlinear Lift Characteristics of
Slender Bodies at Incidence, Journal of the Society of Naval Architects of Japan,
Vol.154. Dec. 1983
K.Matsumoto, K.Suemitsu; Hydrodynamic Force Acting on a Hull in Maneuvering
Motion. Journal of the Kansai Society of Naval Architects, Japan, No.190, Sep.
1983
T.Nishiyama On the Lateral Resistance of a Prolate Spheroid and Ship, Journal of the
Society of Naval Architects of Japan. Vol.85, 1952
T.Hanaoka; Non-Uniform Theory of Wave
- Making on Low Aspect
Ratio Lifting Surface. Proceedings of the 10th Japan NaionaI Congress for Applied Mechanics, 1960K.Nonaka: Free Surface Effects on the
Side Force and Moment Acting on a Ship Hull with a Drift Angle, Journal of the
Society of Naval Architects of Japan. Vol.138, Dec. 1975
T.Hori, K.Matsumura, I.Tanaka; On the Lateral Force Caused by Wave Generation Acting on the Ship Hull with Steady Drift Angle, Journal of the Society of Naval
Architects of Japan, Vol.159, Jun. 1986
W.Song; Wave.making Hydrodynamic
Forces Acting on a Ship with Drift Angle
and Wave Pattern in Her Neighborhood, Journal of the Society of Naval Architects of Japan, Vol.211, Mar. 1989
F.Xia, L.Larsson: A Calculation Method
for the Lifting Potential Flow
AroundYawed Surface-Piercing 3-D Bodies,
Pro-ceedings of Sixteenth Symposium on Naval
Hydrodynamics. Berkeley,.1986
C.WiDawson; A Practical Computer Method for Solving Ship-Wave Problems, Proceedings of Second International Con-ference on.Naval Hydrodynamics, Berkely, 1977
J.Ando, K.Nakaake; A Method to
Calcu-late
Wave Flow by Rankine
Source.xl 02 F,..
F,..
If.t
20 -
Q'Jj
V ! 4 T JJ3 rn(x',J, 1) X G3(x, y, z; i, j, í)dS where '7k (L12
y,
qvx4r J-U2 (xe)
On the Flow Field and the Hydrodynamic Forces of an Obliquing Ship 111 Transactions of the West-Japan Society of where
Naval Architects, No.75. Mar. 1.988
3) W.Bollay; A Non-linear Wing Theory and O (x, y, z; z', y', z')
its ADplication to Rectangular Wings of
1
Small Asoect Ratio, ZAMM, 1939
-
214) 17th ITTC Resistance Committee Report:
-±
)± (zz)
Cooperative Experiments on Wigley Para-
1
bouc Models in Japan, 1983 / 2 ' 2 ' 2
is) TKashiwagi;
Study on Manuevering Hy-(xx) ()
(zz)
drodynamic Force Acting on a Ship
Moving in Following Sea, Doctor Thesis.
(Expression of q',)
Osaka tjniversity, 1984
We divide the ship center plane into K
divisions in the draftwise direction and giveAppendix
the number k(=1--K to each strip and the
(Expression of q)
numberk'(=lK±l) to each dividing line
The velocity vector q5(q33, qsy. qsz) induced () from the bottom to the still water surface.
by the source distribution m on the hull surface Then w assume the constant strength of bound is expressed as vortex y, on the k-th strip and the free vortex
7 a a a sheet shedding with the angle ( ¡9/2) from
(q5, q5. q)
= ( )(A-1)
the k-th strip as in Fig.2. The velocity vector qa
Sy 3z /(q, q,q) induced by the vortex systems is
is the disturbed velocity potential due to expressed as m and becomes
27
H
(A-2)
z
k'(x)2±y2+ (z_)2
(x)cose±ysine
Slfl O , i d4r
J-L12(z) --- ycosO - (x)sin
-/(x) H-y-e- (z)
('L12
'sine
, x4ir
J-u2 (z-1)-ycose(x)sine)
(x)cos
±ysin C(x)2-i-y2± (z'
7k 1u2
x
Zr
4
Ju2
(x)±y2 V(x_)2±y2+(z_)2
f(x_)2+y2+(z_
I
(x.)cosC±ysinO
-___'cose)
( sin O)7(x) 2±y2± (z)
+1 4Juz (z')2±)ycosO\xç)
q, q-,, =
q(A-3)
z k'-- I
(x)2-f-y2+(z-1
)2112
Kunjhu NAKATAKE, Atsushj KOMURA. Jun ANDo, Katsumj
KATAOKA r112
+
cosE)j J112(ZThk'j
LaF aF
ax' a' az
7
-ycosE) - (x)sinE) 2
-
'
rVzR_J
(x.)2±
ycosO - (x)sinE) 2
u'
r ¿12ycos E) - (x ) sin E)
JJ_U2
(zi)2
ycOsE)(x_)sin
2 t(Expression of qp)
The velocity vector q
(qFx-,
qy,
Fz) induced by the source disributjon ' ori thestill water surface is expressed as (qFx, FY, FZ)
(A-4)
p is the discurbed velocity pocential due
to 0p and becomes