CHALMERS UNIVERSITY OF TECHNOLOGY
DEPARTMENT OF NAVAL ARCHITECTURE
AND MARINE ENGINEERING
GOTHENBURG - SWEDEN
VERTICAL EXCITING FORCES ON A
RESTRAINED CYLINDER FROM WAVES
IN SHALLOW WATER
by
CHEUNG H. KIM
DIVISION OF SHIP HYDROMECHANICS REPORT NO. 37
Gothenburg, May 1967
CONTENTS
.t'.
Part I: Vertical Exciting Forces due to Transverse Incident Wave
1. Intröductiön . s s s s
i
s . s s s s si
si
i
2
Potential
and boundarycondition
. ..
. s.
.
13. Exciting forces s s. e s s s s s s s
.
s s e s s e e'.
Numerical calculation, and discussion . . . .Apliication - Heave öf freely floating cylinders 5
Discussion .. . . .. .. . .
.
. .
.
. . . 6Part II: Vertical Exciting Forces due to Longitudinal Ináident
Waves.,
1. Introduction .. s. s s s. 's. s
2. Potential and bôundary condition . . .
s .
. 73.Excitingforces.
.. ... .... .-. ...
8t.Numerical calculation and discussion
.. . . .
95 . App ii. cat-i on . . . - . . . . - . . . s s s s s s iO
Acknowledgement ...
..
.. .
...
. . s e s ss es es
References
.
... .. -. .
s_11N orne nc lature . . . s s s s e s s e e s s s s . .12
Vertical Exciting Forces na.Restràined GXlinder from Waves
ihallow' Water.
Part I.
1., Introduction.
Suppose that a cylinder is fixed on a calm water surface and that laterally oncoming waves then are passing the cylinder in a directio
perpendicular to its axis. As a resul.t of the, wave motion the
pressure distribution yields an oscillating force and montent. Our aim is to calculate the vertical component: of the exciting force
in .shallòw water. Our basic assumptions are:
ideal flUid water,
linearized boundary conditions.
.
Grim [i] has computed the exciting forces in water of infinite
depth. The author exténds his theory to shallow water.
The forces as well as the heaving motions and phase 'lags' of a freely
floating cylinder in beam seas are also calculated ànd represented
in figures and discussed.
The calculations show that the heaving' amplitude and phase lags in Shallow water are generally higher than those of, deep water waves.
The computation has been carried out on the SAAB D21 - computer of
the University in Gothenburg. . .
2. Potential and boundary condition.
The origin of the coordinate system is at the cross point of the waterline in calm water and the centrline'of the profile. The.
x-axis lies horizontally to the eight an4 the y-x-axis vertically
pointing downward. .
Grim
fi]
assumed that the potential of fluid motion dùe to a beam wave passing a fixed cylinder is composed of the potential of the laterally passing wave and the potential, which describes theFor this latèr coTnonent the potential for the forced. heaving
motion in calm water is assumed [1], wheré the amplitude of the hèavé velocity 'TJ=1,
Generally the potential of the incident wave in shallow water is
-
+ i
=.gE
w
.w wamplitude of the wave gravitational constant
2
shallow water wave number; = v0.tanh
vh
circular frequency of the wave
water depth.
complex coordinate x+iy
'For the calculation of vertical forces one needs only the even
potep'tial function about the y-axis. Therefore our potential and
stream function of the wave should be cosh v_(h-y) cosh v0h s Inh ' (h-y) cosh v0h cos(-v0z
+ iv0h -- wt)
cosh v0hCOS \)0XCOS wt
sin
VX.COS
(A)tThê potential for the disturbed motion of the fluid in shallow water [3] is
+
iwt
{A r_!cosh K(hy)'
h ' h e L
'iRh
K2ir.cosh
1.
20h+sinh 21i
coshv0(h-y
(-1 +
ZA
n1
n (2n-. s s s s s s s (l.l) s s s s s s s (1.1'.)eot]+
2rr'sv2.èosh y(ji_y)e0
(2v0h+sinh 2h)scosh v0h
where g = = = w = h z =$ o
3
where is a component stram function for forced heave in calm
water of finite, depth (see []').
3. Exciting forces.
By satisfying the boundary condition.(L3) One obtains the
Intensi-ties of sources A0 and A and. therefore the potential of the fluid
motion which satisfies all the boundary conditions is determined. The exciting force is then obtained by integrating the hydrodynamic
pressures along the surface of the cylinder:
dx =
w[zJ
Re(A4,.)dx].sin wt--
coshv0(h-y)
cas vx.dx].sin wt
-cosh
v0h
-
PwrEfImcA,dx].còs
wt ; '.The secon,d term represents the .hydrodynamic force due to
Froude-Krylov assumption i.e. the force from theundeformed surface wave,
while the rest terms do the c'ornponeùts of hydrodynainic forces Çaused. by the disturbance of the fluid owing to the presence of.
the body.
where A A = unknown intensities of sources
V =
u2/g
= shallow water wave number
h water depth
w
circular fequençy
The boundary çondition on the 'surface of the cylinder is thus written as follows: sinh
v(h-y)
Re z (A = - L_.. sin, y x fl .coshlvh
O (1 3)Im z(A,) = O
The exciting force obtained consists of two components with a
phase difference of 90°. One is in phase with the vertical
dis-placements of the water particles and the other is in phase with their vertical velocities at xo, y=y. Each of them is defined
by the real and imaginary parts of the force and represented by
r ç cosh v0(h-y) = p w E j Re dx + p gj
---.- - cos
VnoS
scoshvh
F..= pwE
jIm(Adx
or in dimensionless form F r r pgBn F. E. = ____ i pgBn i j .Thus Er and E are the dimensionless components of exciting forces
due to the lateral incident wave of unit amplitude on a cylinder
with unit width of beam.
4, Numerical calculation and discussion.
The method of calculation is the same as in [3]. The number of
the terms of the Fourier expansion is five as in ref [3].
Calculations are carried out for several Lewis cylinders and
represented in Figurés l-5.
For the cylinder of H0,8 and=0,8
the forces in infinitely deep water are calculated according to
Grim and plotted in Figure 1. The exciting forces for depth
para-meter h/T10 are almost identical with those of deep water, except
in the very low frequency range. This fact is due to the
hydro-dynamic character of heave in shallow water as discussed in [3].
It is generally stated that the influence of limited water depth on the exciting forces is remarcable, see Figures l5. The effects
of the form of the cylinders are also illustrated. The deep,.
narrow cylinders are less influenced by water depth,. than the shallow draft fuller ones.
As a comparison the Froude-Kryiov fbrces were calculated and drawn
5
5. Application - heave of freely floating cylinders due to beam
waves.
The space and body coordinate systems are taken. as shown in the Figure A.
The equation of the heaving motion of the freely flóátlng cylinder
due t laterally oncoming waves n
sin(v0x+wt)
(m+m") + .N + pgB = F
where n
= mass of the cylinder= hydrodynamic mass
N = damping coefficient.
B = breadth of the cylinde.r
p water density
= ç0e1Wt, is a complex number
F =
F0et,
F0 = (E+iEj)pgB=
circular frequency of encounter
The equation is reduced to
(.R+iR.)
= (E+iE1).1T r+ n)
N where Rr = i pgB W and R =The amplitude ratio of heave and wave is Er + iE1
- R + iR
the magnitude and the argument of which are respectively
o_
Er2+E2
li.
R2+R2
.
E.R- ER.
s =
tn
flhr+
ER)
where s is the phase lag i.e. the lag of maximum heave motion
behind the maximum of the wave.
6. Discussion.
6
The amplitude ratios of heave and wave and the phase lags
in degrees are calculated for several cylinders as funçtions of
frequency and depth parameter , see Figures 6-9.
From the Figures and the results of [] it is seen, that the
heaving motIon and phase lag in shallow water are generally larger
than those in deep water. For depth parameter 10 and they are.
almost identical.
The form effects of the cylinders on the mötions are also illustrated
in the Figures i.e. the deep narrower cylinders are less influenced.
by the change of depths, while the shallöw fuller ones are largely
Part II
1. Introduction.
As an extention of the work by Grim [i] and Abels [s] let a three-dimensional ship be fixed in calm water of limited depth and
suppose that longitudinal waves are passing the ship in a direction
parallel to its longitudinal axis. Our attention is confined to
the plane motion of the fluid around. a section between two
trans-verse control planes of the ship. It is then required to determine
the
hydrodynamic
forceon the section.
.Grim's assumption is also applied to this problem and numerical
calculation are carried out in order
tO
find the inftuence ofwater depth. on the hycirodynamic force. The results are given in
figúres and discussed. Assumed:
ideal fluid,.
linöarized boundary conditions.
2. Potêntial and boundary condition on the cylinder.
The coordinates are the same as in 1. (Part I) except for the.
z-axis, which is taken as the longitudinal axis of a ship, see
Figure B.
The fluid motion of the undeformed longitudinally oncoming waves
is represented by the potential
+
"w = % cosh
v0h
cos iv0(h_y)_(v0z+wt)] . . . . (2.1From the above our rêquired potential is written as equation (1.1'):
. cosh y. (h-y)
=.g . wt
W W
coshy0h
Owhich gives the oscillating vertical velocity of a water particle
at a point around the sectiOn at z: sinh y (h-y)
V=w
..-
CO5Wt
The factor cos is not included, for the problem is confined to
a sectiOn. It must however be used in the appiicati.on of the
re-sults to a three dimensional ship, see 5. Application.
Consequently there exists oscillating flujd flow with the velocity
y through .the section.
On the other hand the boundary condition on the profile requires that no fluid is penetrating the surfäce of the cylinder. To ful-fi.1 this condition one needs therefore to add another stream. The
potential of forced heaving motion in calm water equation (1.2) with unit amplitude o th heaving velocity U is used for this
purpose.. The potential represents the motion of h? djsturbed
water of the longitudinally passing wave (2.1) in the lateral plane. The boundary condition is thus written as follOws
ç sinh y (h-y)
JO
dx+1phO
. . . .. ...
..(2.2)
"s cosh
where is the stream function of the forced heave in shallow
water (see [3]).
3. Exciting fOrce..
By solving the boundary condition (2.2) one obtains the required
potential of the. deformed motion of the longitudinally oncoming
wave (.2.1) in the lateral plane. The hydrodynamic pressure on the
surface of the section thus consists of two components: 1, Pressure due to the deformed fluid motion.
2. Pressure due to the undeformed fluid motion,
The force is therefore obtained by
-8-ç ç cosh y (h-y) I h dx - pgh J ° dx (2 3)j5
s cash v0hThe second integral is the exciting force according to Froude-Krylov
in shallow water. The force is composed of two components with a
phase diff. ir/2 in a manner similar to the equat±ons (1.3). We define the real component as:
Ísn0nr
the imaginary component as
C) E
I
(A nr 9 - A . .)dx + ni nra r cosh \ (h-y)+ pg
J ° dx , s eosh v0h + A .ó. .)dx ni nnjIn dimensiönless form they are given as
F F.
t.
-pgBh i pgBh
where B breadth of the cylinder
E
amplitude of the incident wave,4, Numerical calculation and discussion,
Numerical öalculation are done as in Part I, The dimensionless
exciting fOrces as functionC öf frequency for depth parameter
hIT were computed. and some of them are plotted in the Figures
10-13. .
From the Figure 10 and 12 it is seen that the òurves of Grim at
infinite depth and of hIT 10 are almost identical. As a omparison
the Fraude-Krylov forces were also calculated ad plotted in the
figures.
It is generally stated that the influence of shallow water on the
force are larger for fu1let sections.. than fOr fines ones.
j \
s e (2.4)
5.Applicätion - Exciting forces on a fixed ship in head waves.
Consider.
a ship fixed in a longitudinally oncoming surface wave
n
sin(vz + wt)
to calculate the exciting .force and moment on the hull (see Fig.C).
The exciting force for an arbitrary section at thiökness dz is
i(v z+wt)
pgBsdz(E
+ iE1.)e
Taking the origiorl of the còord.inate system at the midship section,
the mornnt of the àbov
förce about
he pitching axis
Xis
approxi-mately written as
i(v z+wt)
gBiszsdz(E
+ iE1)e
°
Integrating the elementary forces and moments along the total ship
length, one obtains the heaving force and pitching moment aböut the
axis x at the midship section:
lo
-L-
i(v z+wt)
pgh J
Bz(Er+iEi)e
°
.dz
. e e s -. s s e i(2.6)
2iCy z+ot)
pgh J
Bz(Er+iEi)e
°
z.dz,
where
is the beam of cylinders.
I
The author expresses sincerely his gratitude
to Prof..Falkemo, who
has supported this work
He takes this opportunity to acknowledge Dipi.-Ing.
P.Claussen for
L T
L .
Fe1y f1Oating
1 nde
in a bam Waver.
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[i]
Grim,O.:
"Eine Methode für eine genauere Berechnung der
Tauch-und Stampfbewegungen in glattém Wasser Tauch-und in
Wellene"
HSVA - BerichtNr 1217.
Juni 1960.
M.ilne-Thornson,L.M.
"Theoretical Hydrodynamics."
Third Edition.
1955.
Kirn,C.H.:
"Calculation öf Hydrodynamic Forces for CylinderS
Oscillating in Shallow Water,"
Division of Ship Hydromechanics Report No 36,
Cha.lmers UniverSity of Technology.
Feb. 1967.
Grirn,O.:
"Die durdh. eine Oberfläcbenwelle erregte Tauchbewegun
Schifftechnik Bd.!4_1957. Heft 20.
Abels,Fa:
"Die Druckverteilung an einem festgehaltenen
Schiffsmödell
im regelrn.ssigen Seegang."
Jahrbuch der STG, Vol.53,, 1959.
[6]
Grim,O. u Kirsch,i1.:
"TR-4 Prograsrun zur Berechnung, der Thuch- und
Starnpf-schwingungen nach der Strei.fenmethode."
Inst. für Schiffbau, Hamburg, Jan.1966.
[2]
[31
[4].
12
-Nomenclature.
A source intensity
Ann source intensities (real, jmgináry)
B beam of cylinders
E E1 dimensionless exciting force (rea.]-, imaginary)
dimensionless Foude-Krylov exciting force
F exciting force
Fri F1 excititig force (real, imaginary)
depth of water òr sbscript fOr finjte depth
wavè amplitude
half-beam draft ratio
in
imaginary part
L length betieen perpendicular
m mass of a section
in" hydrodynamic mass of a sect-ion
N darnpiñg coeff. of a section
real part
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X,
y body coordinate systemx0,
y0
space coordinate systemz an axis of the coordinate system xyz
section coefficient
E -phase lag
13
-shallow water wave number
density of wäter velocity potential
velocity potential for shallow water
component potential for shallow wate.r (real, imaginary) complex velocity potential for limjted water depth
stream function
stream function for shallow water
component stream function for shallÒw water (real,
imaginary) complex stream. function for shallow water
circular frequency
complex heave, amplitude ;uhr, ''hni