15 y Sc!ipsbuwimde
ARCH ¡EF
Technche Hogeschoo
water in the
Body Plan seo fig. 1.
aft store abt
1.25 ni
above the floorengine room abt 0h20 ra above the ciliad.er heads
fishhold abt 0.60 ni above the concretion on th bbtoai crows quarter abt 0.75 ni above the floor
no water in the foropoak
all tanks on port full with seawater on starboard nuch fewer soawat r
Length over all , (_f_
- LJ'_)
Length at design drught 19,00
Breadth
5.60
D dp t h
2.85
Moan Draught above keol 2.00
Draught fwd dsigii
1.85
Draught aft
2.15
At the momnt of oepsizing - Driught fwd
1.93
nf t
2.56
Displacement (mol. sholiplating)
in soawtor
98.73
Contro of Gr :vity above keel 1.93 abaft half of the length
0.32
GM
0.94
Again in the upright positions
A RKABLE CAS: 0F CAPSIZING 0F A SMALL TRÁ7LIR
Deift
byJ G. DE 11T
INTR0DUCTI0I'
During a heavy gale a small Dutch -brawler capsized and remained floating upside doam for «bout 20 minutes. Thon the vessel began to heel
again slowly and suddenly returned into its normal position. Being back in the upright position thora wore big quantities of water in the hold, tanks, quarters and angine room. The upper part of the steering bridge-house was torn off. Ono member of the crow of 5 was lost. In this upright
position again the ship was very unstable and the crow was able to improve the behaviour and the stability by paying out 50 fathoms of the warp at the end of which a ballast vioight of 50 kg vías comiectod and by discharging water with buckets and a handpump. The weather improved and the vessel was towed into harbour safely.
In connoction with the investigation by the Navigation Board the stability of this ship was studied by Ir, L.F. Hurfot of the Tochnicl University at Dulf-t. Due -be tuo fact that the vessel and rt of the crow wore rescued it was possible to reconstruct the loading condition at the moments of e .psizing and regaining the upright pocition again rathor accurately.
-2-S e a conditi on
According to meteorological data the aind and se:coidi-tions were
direction of the vzind
330°.
7indforce according ta 10 of the Beaufort Sca1evelooi-ty
85
- 95
lan/hr vii-th guts 0±' -- to 1 minute possibly :bt 120 km/hr
vii-th intervals of some minutes
ave height 4 - 5 m
individ.ual viaves 50% higher probably one
each 30 minutes.
Rîave length 80 - 100 ni.
General picture
confused sea.
P1ace
8 naut. miles east o
ST.3 - buoy
(53°-32.5 NL
-
4°-2'EL)
Dateg 7th Octobre 1954.
Stability Calcul-tian.
Fello;sT method forthe calculation of the cross-curves of the
statical stability was usad and a body plan according to Tschebyscheff
scalo 1
20. The cross-curves viere do±ermiiod for heeling anglos to
180°.
Curve 1 of fig. 2 is the curvo o rightiiig lovers for the condition
in which tho vassoi capsized, At 35
the dynamical stability vins 153 mm
For the calculation of this condition the su2orstructuro was not taken
into account. Duo to th
damage discovered afterwards the superstructure
must have boon flooded very soon.
In the upside down position the vessel has sufficient stability to
prevent the vessel to rcturn to her upright position. Thorofore the
ves-sel will romain floating in this position for a considorablo time. In
the moantinio seawater will ponotrato into the vassal through hatchos,
vontilatorpipos and into the tanks through air vont pipos.
The disp1acmont will incroaso. Curvo 2 of fig. 2 represents a
dis-placement of abt 156 ton. TIne stability is unsuffician-t in this
condi-tion, Duo to froc-surfaces of the viator in the vessel, the stability
doeronsos still furthor and. is rnproducod in curvo 4. For this
condi-tion the quantities of water ponotratod into the vessel v;oro nearly
eccording to tho estimates made by the crow after returning to the
upright position. As mentioned already the port oil-fuel tank 'iias much
moro flooded than the starboard tank. Due to this
unsymmetrical
floo-o
ding the ship vail Ithoolt froni 180
to 130
and will romain rolling at
about this point of cquilibrium. From the curvo 4 it can be soon that
the area betvîeon 76
and l30
is vary small now. It needs only the wor
exercised by a heavy wave to push the vassoi to a position of abt. 10
If the flooding should not have boon unsymmetrical the curvo of
righting lavors should have boon according to curva 3. It can ba
doub-ted whethor the vass1 vîould hava regained the nearly upright position
again.
Conclusions.
The stability of this vassoI cama up to the Rahola at ndrd. fully.
Capsizing must 'D
owed to the aburma1 forcas caused 'ay a very
heavy ground-sea.
Horfs-t
Ir
L.P.
Vorsiag van hot ondorzock naar do
stabili-1955
toit van do viskottor OX. 60
(Report of the investIgation into the
sta-bility of the fishingvossal TJ}C,60)(Unpublishod)
E 4o n
co
Lui 2o
- 4o 2o -- 30 -E q-o -I0/
_S__ -2o°r?
800 7CURVE
I :INTACT STABL1TY - Dt5PLAOEMEt-T
98.73 m3
CL)QVE 2
PARTLY
FLOODED-A& 156
rn 110SURFACES.
C.L)RVE 3
PAR.TL'1 FLOODED - DI5PL. ABT.
56 r
FREE 3uRFACE
EDuCTlor NCLUDE
NO PENETRATION OF
/ATETt'i PoRTSD
OF.Î
CURVE 4: A5 CURVE 3. PORT5 IDE
FLootE.D AS OB5ERVEr'
I 2o'FIG.2
-I oa' 4 o 4 _-.__t 35:
4 O -2-'70
4o
OIL FUEL TAr1i
o