A Treatise on Meteorological Instruments: Explanatory of Their Scientific Principles, Method of Construction, and Practical UtilityNegretti, Enrico Angelo Lodovico
Science
A Treatise on Meteorological Instruments: Explanatory of Their Scientific Principles, Method of Construction, and Practical Utility
Negretti, Enrico Angelo Lodovico
Meteorological instruments; Meteorology; Scientific apparatus and instruments
attached to a stout plate, having holes for screws, or fitted to slip into
a staple or bracket, by which it may be fixed to any part of the cabin of
a ship; the arm is hinged to the plate, for the purpose of turning the arm
and barometer up whenever it is desirable.
[Illustration: Fig. 13.]
[Illustration: Fig. 14.]
Other forms of barometer (to be immediately described) have superseded
this in the British Marine, but the French still give the preference to
the wooden frames. They think the barometer can be more securely mounted
in wood, is more portable, and less liable to be broken by a sudden
concussion than if fitted in a metal frame. The English deem the ordinary
wooden barometers not sufficiently accurate, owing to the irregular
expansion of wood, arising from its hygrometric properties. Some of the
English opticians have shown that very portable, and really accurate
barometers can be made in brass frames, and therefore the preference is
now given to this latter material.
=20. The Kew Marine Barometer.=--The form of barometer so-called, is that
recommended by the Congress of Brussels, held in 1853, for the purpose of
devising a systematic plan of promoting meteorological observations at
sea.
The materials employed in its construction are mercury, glass, iron, and
brass. The upper part of the tube is carefully calibrated to ensure
uniformity of bore, as this is a point upon which the accuracy of the
instrument to some extent depends. At sea, the barometer has never been
known to stand above 31 inches, nor below 27. These extremes have been
attained with instruments of undoubted accuracy, but they are quite
exceptional. It is not necessary, therefore, to carry the scales of marine
barometers beyond these limits, but they should not be made shorter. If
the vernier is adjusted to read upward, the scale should extend to 32
inches, to allow room for the vernier to be set to 31 inches at least.
Cases have occurred in which this could not be done, and rare, but
valuable observations have been lost in consequence. If the scale part of
the tube be not uniform in bore, the index error will be irregular
throughout the scale. Whether the bore of the rest of the tube varies in
diameter, is of no moment. From two to three inches below the measured
part, the bore is contracted very much, to prevent the pulsations in the
mercurial column--called "pumping"--which, otherwise, would occur at sea
from the motion of the ship. In ordinary marine barometers, this
contraction extends to the end of the tube. Below the contracted part is
inserted a pipette--or Gay Lussac air-trap--which is a little elongated
funnel with the point downwards. Its object is to arrest any air that may
work in between the glass and the mercury. The bubble of air lodges at the
shoulder, and can go up no farther. It is one of those simple contrivances
which turn out remarkably useful. If any air gets into the tube, it does
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