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
_Directions for Using._--When the apparatus is required for practical use,
sufficient water must be poured into the boiler to fill it about one
third, through an opening, _F_, which must be afterwards closed by the
screw plug. Then apply the lighted lamp. In a short time steam will issue
from _G_; and the mercury in the thermometer, kept carefully immersed,
will rise rapidly until it attains a stationary point, which is the
boiling temperature. The observation should now be taken and recorded with
as much accuracy as possible, and the temperature of the external air must
be noted at the same time by an ordinary thermometer.
The water employed should be pure. Distilled water would therefore be the
best. If a substance is held mechanically suspended in water, it will not
affect the boiling-point. Thus, muddy water would serve equally as well as
distilled water. However, as it cannot be readily ascertained that nothing
is dissolved chemically when water is dirty, we are only correct when we
employ pure water.
=94. Precautions to ensure correct Graduation.=--Those who possess a
boiling-point thermometer should satisfy themselves that it has been
correctly graduated. To do this, it is advisable to verify it with the
reading of a standard barometer reduced to 32 deg. F. The table of "Vapour
Tension" (given at p. 62) will furnish the means of comparison. Thus, if
the reduced reading of the barometer, corrected also for latitude, be
29.922, the thermometer should show 212 deg. as the boiling-point of water at
the same time and place; if 29.745, the thermometer should read 211.7; and
so on as per table. In this way the error of the chief point of the scale
can be obtained. Other parts of the scale may be checked with a standard
thermometer, by subjecting both to the same temperature, and comparing
their indications. The graduations as fixed by some makers are not always
to be trusted; and this essential test should be conducted with the utmost
nicety and care.
Admiral FitzRoy writes, in his _Notes on Meteorology_:--"Each degree of
the boiling-point thermometer is equivalent to about 550 _feet of ascent_,
or one-tenth to 55 feet; therefore, the smallest error in the graduation
of the thermometer itself will affect the height deduced materially.
Public-domain text, read in full here on John Shaqi.
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