through, given above, do not measure the inclination of the ship
to the surface of the water, but only her inclination to the true
vertical. Pitching and lifting are produced by the vessel endeavouring
to follow the slope of the waves, or, roughly speaking, to keep her
displacement the same as in still water, both as to volume and to
longitudinal distribution.
“As to the depressing effect of the water on the bow, a layer of
water one foot deep over the entire forecastle exerts a pressure of
65 tons; this will produce a change of trim of 11 inches, together
with an increase in the mean draught of 1¾ inches; i.e. the draught
of water forward will be increased by 7¼ inches, while that aft will
be diminished by 3¾ inches. A layer 2 feet deep will have double this
effect; one 3 feet thick will have treble this effect; and so on up
to a considerable angle. This follows from the fact that the front
slope of the longitudinal curve of stability, up to a considerable
angle, is very nearly straight. Hence the effect, even of a large
body of water passing over the forecastle, tending to make the vessel
dive down head foremost, is small, and of no importance. It modifies,
however, the transverse stability. When proceeding head to sea there
was no appreciable rolling motion. With the wind and sea on the bow
she pitched considerably less than when going head to sea, but rolled
through 5 degrees or 6 degrees. With the wind and sea abeam, lying
passively in the trough of the waves, the maximum angle rolled through
was 14 degrees from port to starboard, 6½ degrees to windward, and
7½ degrees to leeward, and this without perceptible pitching. When,
however, proceeding at about seven and a half knots, with the wind
and sea on her quarter, she rolled through 27½ degrees from port to
starboard, 13 degrees off the perpendicular to windward, and 14½
degrees off the perpendicular to leeward, besides also pitching
through some 4 or 5 degrees. This is by far the greatest angle she
has ever rolled through. It is the apparent period of the waves,
i.e. their period relatively to the ship, which operates in making a
vessel roll. The motions of the vessel, both as to pitching and
lifting and to rolling, were extremely easy. She, indeed, claims to
have behaved better than her companion, the _Agincourt_. Certainly,
her rolling motion was somewhat slower, and she rolled less deeply;
when the _Agincourt_ was rolling 17 degrees from port to starboard,
the _Devastation_ was only rolling 14 degrees. As to pitching, the
_Devastation_ may fairly claim to have had the advantage, for, as we
have seen, although the _Agincourt_ pitched rather less, her bow moved
vertically through a greater distance, so much so that while going
head to sea at seven knots she shipped a sea over her high forecastle,
showing that she could not be driven under the circumstances at a much
higher speed with at least anything like comfort.”[43]
Public-domain text, read in full here on John Shaqi.
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