- Project Runeberg -  Den Norske Nordhavs-expedition 1876-1878 / The Norwegian North-Atlantic Expedition 1876-1878 / 2. Bind /
15

(1880-1901) [MARC]
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15

Krængning 20". Angle of Hed 20°.

Observeret Fart. Virkelig Fart. V Kvartmil i Timen.
(Observed Speed.) (Actual Speed.) (Miles a. » Hour.)
Kvartmil i Timen. X = 0. x — + 1-. X — —1".
(Jfif es an Hour.) V Corr. Diff. f. 1 Kvartmil.
v’ (Corr.) (Dijf. for 1 ilüe.) V Corr. V Corr.

12.0 1 11.6 —0.4 11.4 —0.6 11.8 —0.2
0.03

9.0 8.7 -0.3 8.5 —0.5 9.0 0.0

6.0 5.8 —0.2 ’ 5.4 —0.6 6.2 -(-0.2

4.0 i 3.9 —0.1 3.3 —0.7 4.4 +0.4

3.0 I 2.9 —0.1 ’ 2.0 —1.0 3.6 -fo.6

2.5 2.4 —O.I 1.2 —1.3 3.2 +0.7

2.2 2.1 —O.I ’ O.4 -1.8 3.0 +0.8

O.O3

2.I77 I 2.1 -O.I i O.O —2.2 3.0 4-0.8

I O.O3

i.o j 1.0 0.0 I 2.3 +1-3

Man ser, at Krængningsfejlen, selv med en saa stor
Krængning som 20°, for de større Farter kun udgjør
Brøkdele af en Knobs Fart. Svinger Fartøjet om et Punkt i
eller nær Vandliniens Flade, er Krængningsfejlene i ethvert
Tilfælde meget smaa.

Anderledes stiller Forholdet sig, dersom Stigerøret ikke
staai- midtskibs. Der kommer da under Krængning en ny
Korrektion til. som bliver positiv for Krængning til den ene
Side_ og negativ for Krængning til den anden, og hvis
Størrelse voxer med Stigerørets Afstand fra Diametralplanet.

Efter vor Erfaring viste Vandloggen sig særdeles
hensigtsmæssig og holdtes med største Lethed i Orden. Et
Blik ned i Maskinskylightet var nok til at observere Skibets
Fart i Øjeblikket. Maskinisten kunde under Skrabning og
Trawling holde Skibet gaaende med den befalede Fart.
Til Reduction af de observerede Vindretninger og
Vindhastigheder til sande kræves Skibets Hastighed i
Observa-tionsøjeblikket. Denne observeredes paa Vandloggen, der
saaledes er et udmærket nautisk-meteorologisk Apparat.’"

It is evident that, with greater speed, the error
involved in heeling, even at an angle of 20", will amount to
only a fraction of a mile. And if the point about which
the vessel turns lie in or near the plane of the water-line,
the error will be generally very small.

The case, however, is different in the event of the
upper tube not being amidships. Another correction,
positive with a heel to the one side, negative with a heel to
the other, will then be needed for computing the speed, and
the effect of the heeling will increase with the distance of
the upper tube from amidships.

So far as our experience went, we had every reason
to be satisfied with the water-log; it answered excellently,
and was easy to keep in order. A glance down the
engine-room skylight sufficed to tell the ship’s speed. Hence, -in
dredging or trawling the engineer could keep the vessel at
the exact rate required. For reducing observations of the
wind’s direction and velocity to their true value, the speed
of the vessel at the moment of observation has to be found.
Now, this we took from the water-log, which accordingly
proved an excellent instrument for meteorological work
at sea."

af det Stykke, Vandets Overflade har Hyttet sig fra det oprindelige
Niveau i Røret. Ligger Niveauet under Krængningen højere, det er
over Nulpunktet (Loddet paa Tal paa Skalaen), er x positiv, ligger
det lavere (Loddet ovenfor Nulpunktet paa Skalaen), er x negativ.
Formelen er:

distance o, through which the water in the tube has moved from its
original level. If the level in heeling be higher, i. e. above zero (the
weight within the divisions of the scale), the value of x will be
positive; if lower (the weight above zero), x will be negative. The
formula is as follows: —

Ex. i = -20°, o = 0.m05, x = O ’» 770.
Den negative Værdi af x lig en hel Meter er medtaget som
Regne-exempel for at vise Virkningen af en saadan, omendskjønt den ikke
vil forekomme i Praxis.

Example: i = 20°, o = 0.m0.r>, x = 0.-779.
The negative value of x put equal to a wholo metre, is introduced
merely by way of example, to show its possible effect, the case never
occurring in practice.

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