The Steam Engine Explained and Illustrated (Seventh Edition): With an Account of Its Invention and Progressive Improvement, and Its Application to Navigation and Railways; Including Also a Memoir of WattLardner, Dionysius
History
The Steam Engine Explained and Illustrated (Seventh Edition): With an Account of Its Invention and Progressive Improvement, and Its Application to Navigation and Railways; Including Also a Memoir of Watt
Lardner, Dionysius
Steam-engines; Watt, James, 1736-1819
The reason the degrees were commenced at 32° below the freezing
point was, because, when the thermometer was invented, that
temperature was supposed to be the lowest degree of cold possible,
being that of a certain mixture of [Pg100] snow and salt. This,
however, has since been found to be an error, very much lower
temperatures being obtained by various physical expedients.
The temperature of a body is, then, that elevation to which the
thermometer would rise when immersed in that body. Thus, if in
plunging the thermometer in water we found the mercury to rise or
fall to the division marked 100, we should then say, the
temperature of the water was 100°.
Let us suppose a spirit lamp, or other regular source of heat,
applied to a bath of mercury, so as to maintain the mercury at a
fixed temperature of 200°, and let another vessel, containing a
quantity of ice at a temperature of 20° be immersed in the
mercury. Let a thermometer be placed in the mercury, and another
in the ice. The following effects will then ensue. The thermometer
immersed in the ice will be observed gradually to rise from 20°
upwards, until it indicates the temperature of 32°. It will then
become stationary, and the ice which had hitherto remained in a
solid state will begin to melt and be converted into water. This
process of liquefaction will continue for a considerable time,
during which the thermometer immersed in the ice will constantly
be maintained at 32°. At the moment, however, when the last
portion of ice is liquefied, the thermometer will begin again to
rise. The coincidence of this ascent of the thermometer with the
completion of the liquefaction of the ice, may be very easily
observed, because the ice being lighter, bulk for bulk, than
water, will float on the surface, and so long as a particle of it
remains unmelted it will be distinctly seen.
Now it cannot be doubted that, during the whole of this process,
the mercury, supposed to be maintained at 200°, constantly imparts
heat to the ice; yet, from the moment the liquefaction begins,
until it is completed, no increased temperature is exhibited by
the thermometer immersed in the melting ice. If during this part
of the process no heat were received by the ice from the mercury,
the consequence would be, that the application of the lamp would
cause the temperature of the mercury to rise above 200°, which may
be easily demonstrated by withdrawing the vessel of ice from the
mercurial bath during the process of liquefaction. The moment
[Pg101] it is withdrawn, the thermometer immersed in the mercury,
instead of remaining fixed at 200°, will begin to rise, although
the action of the lamp remains the same as before; from which it
is evident that the heat which now causes the mercury to rise
above 200° was before received by the melting ice.
Public-domain text, read in full here on John Shaqi.
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