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
=44. Howson's Long Range Barometer.=--Very recently quite a novel design
has been patented by Mr. Howson, for a long range barometer. The
construction requires neither distortion of the tube, nor mechanism for
converting a short scale into a long one; but the mercury itself rises and
falls, through an extended range, naturally, and in simple obedience to
the varying pressure of the atmosphere. The tube is fixed, but its cistern
is sustained by the mere pressure of the atmosphere. Looking at the
instrument, it seems a perfect marvel. It appears as though the cistern
with the mercury in it must fall to the ground. The bore of the tube is
wide, about an inch across. A long glass rod is fixed to the bottom of the
glass cistern, where a piece of cork or some elastic substance is also
placed. The tube is filled with mercury; the glass rod is plunged into the
tube as it is held top downwards, until the cork gets close up to the tube
and fits tightly against it. The pressure against the cork simply prevents
the mercury from coming out while the instrument is being inverted. When
it is inverted, the mercury partly falls, and forms an ordinary barometric
column. When the top is held, the cistern and glass rod, instead of
falling away, remain perfectly suspended. There is no material support to
the cistern; the tube only is fixed, the cistern hangs to it. Glass is
many times lighter than mercury. When the glass rod is introduced, it
displaces an equal volume of mercury. The glass rod, being so much lighter
than mercury, floats and sustains the additional weight of the cistern by
its buoyancy. In the mean time, the atmosphere is acting upon the mercury,
keeping up the ordinary barometric column. Supposing there is a rise in
the ordinary barometer, the atmosphere presses some more mercury up the
tube. This mercury is taken out of the cistern, which of course becomes
lighter, and therefore the rod and cistern float up a little higher, which
thus causes the column of mercury to rise still more. The increased
pressure and buoyancy thus acting together, increase the ascent in the
barometric column, as shown by the fixed scale. One inch in the barometer
might be represented by two or more inches in this instrument, according
to construction. Supposing there was a decrease of pressure, the mercury
would fall, come into the cistern, make it heavier, and increase the fall
somewhat. Friction guides, at the top of the rod, prevent it coming into
contact with the side of the tube when vertically suspended. The
illustration, Fig. 31, shows the appearance of the instrument as framed in
wood by the makers, Messrs. Negretti and Zambra.
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