Report 1055
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NAVY DEPARTMENT Bad
THE DAVID W. TAYLOR MODEL
WASHINGTON 7, D.C.
_BEHAVIOR OF A PROPOSED OCEANOGRAPHIC RESEARCH
VESSEL IN WAVES
by
F.V. Reed
RESEARCH AND DEVELOPMENT REPORT
August 1956
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Report 1055
Na)
Gy
no. 1055
BEHAVIOR OF A PROPOSED OCEANOGRAPHIC RESEARCH
VESSEL IN WAVES
by
F.V. Reed
August 1956
Report 1055
TABLE OF CONTENTS
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LIST OF ILLUSTRATIONS
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Figure 2 - Model of Oceanographic Research Vessel ..............:ce:cessceceresecenecenes
Figure 3 - Reduction of Speed with Constant Tow Force and
Wavelength/Waveheight | ROBY FIICG) coacosopnoscoDacbadnno0adaonocOcHNDEOSaboCOHONdOCEDCEOCONCEC
Figure 4 - Plots of Pitch and Heave versus Speed for Constant Wavelength
Figure 5 - Total Resistance of Model in Still Water .............:c:ccesssssssesseeseseeeeee
LIST OF TABLES
Table 1 - Design Characteristics of the Oceanographic Research Vessel ...
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NOTATION
Maximum beam
Block coefficient
Longitudinal prismatic coefficient
Coefficient of maximum sectional area
Draft
Waveheight
Length of ship
Amplitude of wave
Ship speed producing resonant period of encounter
Amplitude of heave
Maximum slope of wave
Wavelength
Amplitude of pitch
lV
ABSTRACT
A 5-foot model of a proposed oceanographic research vessel was
tested for seaworthiness. Measurements of speed, pitch, and heave were
made in a variety of wave conditions with the model heading into the waves,
and qualitative observations were made in several wave conditions with the
model in following seas.
INTRODUCTION
BACKGROUND
The broad definition of oceanography as ‘‘the science which is done at sea’’! may be
taken to epitomize the notion that it is the science which results when the naval architect,
the hydrodynamicist, the meteorologist, the seismologist, the biologist, and the chemist turn
their attention to the study of the sea.
The diversified character of the studies means that a ship designed to conduct such
research must meet, specifically or by compromise, needs which may be common to or con-
flicting among the various branches. To list but a few of the items of equipment and facilities
which must be available at one time or another, there are echo-sounding gear, explosives for
seismological work, trawls of various kinds, snappers, dredges and corers for bottom-sampling,
means of taking water samples and temperature, and laboratories and stowage facilities for
samples and specimens.
THE PROBLEM
The problem of designing a ship specifically for oceanographic research is far from
simple. Should she be large like the Russian hydrographic ship WITJAS, purportedly of
5500 tons displacement,” or small like the 380-ton ATLANTIS, should she be a 12 or a 16
knot ship, and should it be attemped to provide for all types of acoustical work — these are
only a few of the difficult questions that must be answered.
The per-diem cost of an oceanographic expedition is quite high and is one of the more
important factors which put an upper limit on the size of the research ship. The ship must be
large enough to carry sufficient personnel and equipment to make an expedition scientifically
profitable, and yet her requirements as to crew, rations, and fuel—not to mention maintenance
cost between cruises—must be modest.
Seaworthiness is of course a basic requirement of any vessel intended for long periods
of blue-water sailing, but more is desired of the research ship than mere ability to survive
heavy weather. It is desirable to reduce the sea-excited motion of the ship as muchas possible.
Excessive motion not only means misery and consequent inefficiency for personnel but adds
References are listed on page 9,
to the difficulty of handling gear and, most important of all, hampers the conduct of even the
most routine scientific work. In addition it might be mentioned that for certain types of work
it would be a great advantage to be able to control the heading of the ship at speeds below
steerageway and even while lying to.
Precise criteria for satisfactory performance do not exist, but there is obvious benefit
in a vessel which will permit operations which have previously been prevented by a state 5 sea.
PROPOSED HULL DESIGN
A hull which has been proposed to meet the many and diverse requirements of ocean-
ographic research was designed by CDR R.T. Miller, USN. The lines and outboard profile are
shown in Figure 1 and several views of a 5-foot model of this vessel are shown on Figure 2.
Pertinent design particulars are listed in Table 1.
TABLE 1
Design Characteristics of the Oceanographic Research Vessel
Length, overall, feet 181
Length, waterline, feet 170
Length between perpendiculars, feet 163
Draft (design waterline), feet 14.75
Displacement (design waterline), tons 1000 (salt water)
Design speed’(still water), knots 12
Longitudinal prismatic coefficient Cp 0.53
Coefficient of maximum sectional area Cy 0.80
Block coefficient Cp 0.423
Ratio of ship length to maximum beam L/B 5.2
Ratio of maximum beam to draft B/H 2.2
The values of Cy, Cp, L/B, and B/H are typical of tugs and trawlers of the same
approximate size as the proposed ship; the same is true of the deadrise.
The level of the forecastle deck terminates farther forward on the starboard side than
on the port side; see Figures 2a and 2b. This affords 100 feet of clear working space on the
starboard side for streaming equipment. The rubrail on the starboard side is faired into the
hull down to the waterline, starting at the after end of the deck house and extending fotward
some 14 feet. This arrangement preserves the function of the rubrail without offering an
obstruction to gear being worked overside.
The model was ballasted to the design waterline to give a radius of gyration of 0.22L,
resulting in a pitching period (determined experimentally) of 0.738 seconds or 4.3 seconds
full scale. The figure 0.22 L for the radius of gyration is somewhat smaller than that usually
————
Dk. Camber
Figure 1a - Preliminary Lines
DWL - Stbd. Only
Figure 1b - Outboard Profile (Rev. 2)
Figure 1 - Oceanographic Research Vessel
DWL
NP21-63892
Figure 2a - Starboard Side
antennae
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4603
NP21-63891
Figure 2b - Port Side
Figure 2c
Bow View Figure 2d - Quarter View Figure 2e - Stern View
Figure 2 - Model of Oceanographic Research Vessel
assumed in the absence of specific data for such tests at the Taylor Model Basin. The smaller
value was chosen in view of the intended location of most of the massive items of equipment—
the winch and stowage reel for deep-sea cable and the main propulsion plant. These, with
most of the fuel, will be located in the middle half-length of the ship.
MODEL TESTS
The tests were conducted in the 140-foot basin, using a pneumatic wavemaker and a
gravity-type dynamometer.
Wavelengths corresponding to 127.5, 170, 204, and 340 feet QWik = Oss LO, 12, 20)
were used, each with A/h/ values of 20, 30, and 40. The model was tested in head seas using
tow forces corresponding to still-water speeds of 6 and 12 knots. Pitch, heave, and speed
were measured for these conditions.
The model was also run in several sea conditions with her stern to the sea, viz.,
h =0.75L, 1.0L, 1.2L, and 2.0L, all at A/h =20. These tests were for qualitative results,
no measurements of pitch and heave being taken.
The measurements of total resistance in still water were obtained incidentally in order
to determine the data necessary to carry out the tests. It is considered that scaling of resis-
tance data from a 5-foot model to full scale is of doubtful validity. The resistance curve is
given , Figure 5, page 9, merely to indicate the reproducibility of the data.
RESULTS AND DISCUSSION
The results of the tests are presented in Figures 3 and 4 and Table 2. Figure 3 shows
the reduction of speed in waves; the tow force and the \/A/ ratio are constant for each curve;
speed is plotted against wavelength. The magnitude of pitch and heave are shown in Figures
4a through 4d; each figure involves a single wavelength and each curve represents amplitude
of motion plotted against speed for a constant ratio of A/h. The speed Vp which would pro-
duce resonance in pitch—the most violent motion for a given wavelength should be expected
at this speed—is shown for each wavelength.
As the curves show, reduction of speed in waves is in some cases quite drastic. How-
ever, in heavy weather, ship speed is more likely to be determined by the master, in the interest
of safety and comfort, rather than by lack of power. digh speed is useful mainly in traveling
to and from station, so that a ship which can make 7 or 8 knots in a state 4 sea would probably
be quite satisfactory from the standpoint of speed.
As to the observed pitching and heaving, they, too, are quite drastic on occasion, and
are considerable throughout most of the conditions investigated. Unfortunately this behavior
is characteristic of small ships in large waves. Table 2 shows that the pitch amplitude re-
ferred to the maximum slope of the exciting wave (column w,,/W_,) is never larger than 1.12,
and the nondimensional heave Z,,/?,, does not exceed 1.3. In view of the fact that values of
Tow Force corresponding to
12 knots in still water
8 Tow Force corresponding to
r 6 knots in still water ------
ge =|
c
= =
=
36 Sa ae |
a ‘|
n N
= ‘
a 4 {—\
een ise ate fh
40 80 120 160 200 240 280 320 360
Wavelength in feet
ia [Tow Force corresponding to a
IL 12 knots in still water
*
Tow Force corresponding to
Ig ail 6 knots in still water -----~
a
cs
= .
Sel
Sie
a=]
2 6§———--==
eS aa
S =.
= i \ A/h=30
n4 —. — Lee
\
\ ee an ae Hoey
2 ee = =
ner a
Ltt —— ee eee
oO 40. 80 120 160 200 240 280 320 360
Wavelength in feet
le Tow Force corresponding to
L 12 knots in still water
Tow Force corresponding-to
10 F 6 knots in still water ----——
n ee er =|)
2 8 Se
Sb /b=40
6S
og N
Qa \
Oa \
2 ‘
nt ra
\ =
eb lk dae: —_—
Ir Venn 7
2 -
L at a —t it 4 4 1 tt
(0) 40 80 120 160 200 240 280 320 360
Wavelength in feet
Figure 3a - \/h = 20
Figure 3b -A/h = 30
Figure 3c -A/h = 40
Figure 3 - Reduction of Speed with Constant Tow Force and Wavelength/Waveheight Ratio
Length of ship equal to 170 feet.
Ym in degrees
Zm in feet
vm in degrees
Zm in feet
HE d=170' A/L=1
: al ee aa = oA/h= 20
é [real | L +/h = 30
| 6 x/h = 40
[ala 5 =>
] TF
ae eh jauszeseeezca
’ : pebece
asi L 33 H+
X=1275 X/_= 0.75 c
Se elateeale own20 | im HOU
+ d/n=30 me
Po soe Se 18 ce
j
Ship Speed in knots
Figure 4a - Wavelength 127.5 Feet
»=204 Ys 12
o Wh =20
9
+ d/h =30
8 x Wh =40
‘ Bee:
6 +
5
4
3
t—]
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Ht
5
4
‘ +44
: HEE
| = at!
Vp 212.17 knots
Sa
fo) 6 8
Ship Speed in knots
Figure 4c - Wavelength 204 Feet
¥,, in degrees
2
2
<
i=
N
Ship Speed in knots
Figure 4b - Wavelength 170 Feet
eee
—r i
£ tt SS se ae
sa Le LL
= es 1 1 iE all
| i
h=340' d/L=2
It
im © \/h=20
+ X/h=30
X d/h=40
4 6 8
Ship Speed in knots
Figure 4d - Wavelength 340 Feet
Figure 4 - Plots of Pitch and Heave versus Speed for Constant Wavelength
in VR=22.l knots a
iKe)
1.6 and 2 for v/o, and z,,/r,, are not unusual for other vessels, it appears that the values
recorded here are by no means excessive.
Throughout the tests in head seas, the bow was dry except for an occasional bit of
splashing; the stern shipped water only in the steepest waves—i.e., X/h = 20—of lengths
dh =0.75L, 1.0L and 1.2L.
The model rode easily and was dry in following seas at speeds of 6 and 12 knots. When
lying to, she took water at the stern in seas of } = 0.75L, A/A = 20, and also A = 1.0L, \/A = 25
and steeper, and was dry otherwise.
TABLE 2
Tabulation of Test Results
ft
127.5 6.30 | 20.24 | 2.85 : 0.284 0.321
127.5 4.31 | 29.22 | 2.07 : 0.339 0.336 Zero
127.6 3.25 | 39.20 6 0.316 0.337
127.5 | 4.30 | 29.60 0.598 6 knots
127.5 | 3.17 | 40.20 j 0.915 Stillwater
127.5 | 6.52 | 19.60 | 1.33 | 0.67 | 9.52 | 0.310 Diay
127.5 | 4.36 | 29.20 | 0.73 | 0.37 | 10.70 | 0.417 Stillwater
127.5 | 3.19 | 40.00 | 1.55 | 0.78 | 11.25 | 0.420
170 8.36 | 20.6 4.80 2.01 0.482 0.549
170 5.46 | 30.1 3.55 1.78 0.574 0.594 Zero
170 4.02 | 42.2 2.50 1.14 0.568 0.586
170 3.67 0.826 6 knots
Stillwater
170 8.66 | 19.6 4.45 | 4.34 2.97 1.000 0.485 12 knots
170 5.7/8 | 29.4 4.90 5.94 1.183 0.800 Stillwater
3.21
170 | 4.26 | 39.9 | 3.02 | 2.07 | 8.74 | 0.972 | 0.670
204 | 10.20 | 20.00 | 5.40 | 3.95 0.772 | 0.600
204 6.97 | 29.30 | 4.15 | 2.87 0.824 | 0.676 | Zero
204 5.36 | 38.90 | 2.80 | 1.59 0.595 | 0.605
204 6.86 | 29.75 | 5.35 | 2.85 | 2.075 | 0.833 | 0.884 | 6 knots
204 5.13 | 39.80 | 3.67 | 2.69 | 2.860 | 1.050 | 0.812 | Stillwater
204 | 10.30 | 19.78 | 9.30 | 4.99 | 3.830 | 0.969 | 1.020
204 6.77 | 30.10 | 6.55 | 4.54 | 6.120} 1.195 | 1.095 | 22 knots
3.00
204 5.10 | 40.20 | 5.00 7.580 | 1.177 | 1.117 | Stillwater
340 16.90 | 20.05 | 9.35 | 8.78 1.040 1.065
340 11.24 | 30.20 | 5.70 | 5.25 0.934 0.956 Zero
340 8.50 | 40.00 | 4.42 | 3.70 0.871 0.982
1.063 6 knots
Stillwater
340 | 17.30 | 19.67 | 8.50 | 8. 7.49 | 0.925 | 0.928
340 | 11.33 | 30.00 | 6.49 | 5. 8.96 | 0.982 | 1.083 | 12 ie
340 | 8.75 | 38.90 | 4.55 | 5. 9:78 |) 1-290) | 01983, Stillwater
0.6
fe}
a
9
3B
9
w
fo)
nN
Total Resistance in pounds
fo)
(0) 0.5 1.0 LS 2.0 2.5 3.0
Speed in knots
Figure 5 - Total Resistance of Model in Still Water
CONCLUSION
Within the limitations of the tests conducted, the model of the proposed oceanographic
research vessel rode easily, was reasonably dry and showed motions which were on the average
somewhat less than those observed on models of other types of vessels.
REFERENCES
1. ‘‘Oceanographic Instrumentation,’? Edited by John D. Isaacs and Columbus O.D. Iselin,
Division of Physical Sciences, National Academy of Sciences, National Research Council,
Publication No. 309 (Jun 1952).
2. Castle, .C., ‘‘USSR/iydrographic Research Ship ‘WITJAS,’’’ Intelligence steport 57-56,
U.S. Navy Forces Germany (9 Feb 1956).
3. Minot, F., ‘‘Report on a Pre-Design Engineering Study of the Development of Superior
Ships for Oceanographic Research,’’ Woods Hole Oceanographic Institution Reference No.
53-26 (May 1958).
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