GAS APPARATUS.
315
with the water in the cistern ; and for this reason, the che
mist must refrain as much as possible from keeping the
hands upon either ; or, if it is suspected that they have been
heated, he must cool them again by means of the water in
the cistern. The height of the barometer and thermometer
during the experiment is of no consequence. When the
marks have been thus ascertained upon the jar, for every
ten cubical inches, a scale is made upon one of its sides, by
means of a diamond pencil.
Glass canes are graduated in the same manner for using
in the quicksilver trough, only they must be divided into
cubic inches. The bottle for gauging these should hold
one cubic inch, and, consequently, the gauge-bottle must
hold precisely 252 grains 58, or ten pennyweights, a half
pennyweight, and half a grain of distilled water ; or the
specific gravity of the quicksilver at hand is to be taken, the
weight of a cubic inch calculated, and used to fill the gauge.
Another mode of determining the volume of elastic aeri
form fluids, consists in transferring the unknown volume of
air into a narrow cylindrical vessel, standing on the shelf of
the pneumatic trough, and then marking, by means of a slip
of paper pasted on the jar, the exact height of the elastic
fluid. This being done, the jar is turned up and filled with
water, exactly up to the mark ; and by weighing the water,
the volume of the gas may be found, either in ounce and
grain measures, or by reduction, into cubic inches. This
method, like that of graduating jars by pouring in succes
sive portions of water, or quicksilver, requires a correction
for the difference of level between the liquid in the jar and
that in the trough.
In measuring gases with these graduated jars, two cor
rections are necessary, the one for variation in their bulk, by
the increase or diminution of the pressure of the atmosphere,
as marked by the barometer, and the difference of level be
tween the surfaces of the liquid that is used to confine them;
the other for the temperature at which they are measured.
It might certainly be beneficial to science, that one uni
form pressure and temperature should be adopted, at least,
in each country, but this cannot be hoped for.
The barometer is to be observed, and if the jar was not
graduated in the first of the methods here mentioned, the
difference of the levels in the quicksilver trough is to be
deducted from the bárometric height, or the difference of
the levels in the water-trough being taken, 3/ioths of an inch
of baromctric pressure is to be deducted for every four inches