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On the heaving motion of two circular cylinders on the surface of a fluid - On the motion of multihull ships in waves

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(1)

16 J4N. 1973

RCHIF

lab. y. Scheepsb

Technische Ho

Deift

."On the Heaving Motion of Two Circular Cylinders on the

Surface of a FluId.T'

"On the Motion of Multihull Ships in Waves (1)."

By Makoto OHKUSU ...-,

These papers are mainly

concerned with the most fundamentalEt

problems for the theoretical treatment of the motions in waves

of multihull ships such as catamaran ships or marine

struc-tures for the exploitation of ocean resources. That is to

cal-culate the hydrodynamic forces, the amplitude and the phase of the waves diverging at infinity, when two or more cylInders,

submerged or floating in afluid, are given a swaying, heaving

and rolling oscillation about their mean position.

In the first paper a theoretical procedure to calculate

exactly the hydrodynamic pressure and the wave amplitude caused

by the oscillation of two circular cylinders with their axes

on the surface of a fluid is developed and it is shown that

the theoretical wave amplitudes are in good agreement with the measured ones obtained on the forced heaving experiments.

This procedure for solving exactly the radiation problem of two circular cylinders, however, is not necessarily convenient

to

solve the more general problems for obtaining the

hydro-dynamic forces and the waves generated due to the oscillation

of two or more cylinders with arbitrary cross sections. Then

in the second paper is proposed an approximate method which

is very effective to solve the radiation problems of such

multi-cylinders. When the hydrodynamic coefficients

(added mass and

damping coefficients etc.) for a cylinder are known, the

(2)

num-ber of the cylinders by this approximate method. And their

accuracy are thought to be satisfactory because the solutions

for two circular cylinders by the approximate method almost

completely agree with the solutions calculated exactly by the

method described in the first paper.

According to Haskind relation extended by Bessho the phase

as well as the amplitude of wave forces and moments which act

upon a body when it is held fixed on incoming plane waves can

be derived from the solutions of the radiation problem of the

body. Using this relation and the solutions of the radiation

problem obtained with our approximate methOd, the equations of

the motions of a catamaran ( Fig.B-1 ) in beam seas are

formu-lated and their solutions are in good agreement with

experi-mental results ( Fig.B-2, 3 and ), where this ship has the

same Lewis form cross section over the length and the motions

in Fig.B-2 and 3 are not of the center of gravity G but of the

point M where the motions of the ship are measured as shown

in Fig.B-1 and the viscosity of a fluid is neglected.

It may be concluded from this result that we can treat easily

and accurately as well the motion of a catamaran in waves as those of an ordinary ship by solving the radiation problem of

each section with our method and applying the strip method.

Along this approach the author is now carrying out some

calcu-lations and experiments on the seakeeping qualities of catamaran

in head seas and beam seas. In addition our approximate method

can be powerful means for the theoretical investigations of the

motion of marine structures with more complicated forms because

the method gives the hydrodynarnic coefficients for submerged

(3)

or floating multi-cylinder composed of an arbitrary number of

cylinders with comparatively simple calculations. The author is now trying to apply the method for the researches of marine

structures? motion in the sea.

(4)

's-y

Fig.B-1 Madu Ship

T

T

u

Wave

P= 720

T=180

2o=

413

-QG

34

Unit mm

(5)

J)

2.0

1.0

o

o

THEORE TI CAL

o

MEASURED

KT

(seT)

Fi.-2

Vi

aìn1itude,çf

catanïn in

g

O

0.1

0.2

0.3

0.6

0.7

0.8

0.9

1.0

0.4

0.5

(6)

4f

N

2.0

¡.0

o

MEASURED

THEORETICAL

0.1

0.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1.0

KT(-T)

Fig.B-3

(7)

4f

2.0

1.0

o

o

o

o

0

0.!

o

o

o

0.2

0.3

0.4

0.5

O

MEASURED

o

o

THEORE TI CA L

0.6

0.7

0.8

0.9

¡.0

-KT=weT)

Fig.B-4 Rolling amplitude

of a catamaran in beam

sea:

Cytaty

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