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
To render these general principles more intelligible, let us
suppose that the water in B is raised to the temperature of 213°,
the stopcock C being open; the vessel A will then be filled with
steam of the same temperature, and having a pressure of 15 lbs.
per square inch. This will be common steam. If the stopcock be now
closed, and the whole apparatus be exposed to the temperature of
243°; the steam in A will preserve the same density, but its
pressure will be [Pg171] increased from 15 lbs. to a little more
than 16 lbs. per square inch. Let the stopcock C be then opened
and while the temperature of the steam in A shall continue to be
243°, the pressure will suddenly rise from 16 lbs. to about 26
lbs. per square inch. The weight of the steam in A will be at the
same time increased in the same proportion of 16 to 26 as its
pressure. The steam thus produced in A will then be common steam,
and any abstraction of heat from it would be attended with partial
condensation.
(96.) The law, according to which the pressure of elastic fluids
in general, whether gases or vapours, increases with their
temperature, was simultaneously discovered by Dalton and Gay
Lussac. If the pressure which the gas or vapour would have at the
temperature of melting ice, were expressed by 10,000, then the
increase of pressure which it would receive for every degree of
temperature by which it would be raised, its volume being supposed
to be preserved, would be expressed by 208-1/3. Thus, if the
pressure of gas, or vapour, on a surface of a certain magnitude at
the temperature of 32° were 10,000 ounces, then the same gas or
vapour would acquire an additional pressure of 208-1/3 ounces for
every degree of temperature which would be imparted to it above
32°. This law is common to all gases and vapours.
It may be objected that water cannot exist in the state of vapour
under the usual pressures at so low a temperature as melting ice.
This, however, does not hinder the application of the above law,
for that law will equally hold good by computing the pressure
which the vapour would have if it were a permanent gas, and if it
could therefore exist in the elastic form at that low temperature.
Public-domain text, read in full here on John Shaqi.
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