The Romance of Modern Chemistry
Forfatter: James C. Phillip
År: 1912
Forlag: Seeley, Service & Co. Limited
Sted: London
Sider: 347
UDK: 540 Phi
A Description in non-technical Language of the diverse and wonderful ways in which chemical forces are at work and of their manifold application in modern life.
With 29 illustrations & 15 diagrams.
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PRODUCTION OF LIGHT AND HEAT
one or two points which have been mentioned already.
In the first place, it shows what fundamental changes those
substances undergo which take part in a chemical action;
we start with a piece of metallic ribbon and the invisible
air, and there is left behind a soft, white, powdery mass
of magnesia. In the second place, the intense light
observed when magnesium burns is due to the presence
of little particles of infusible magnesia, which are
rendered incandescent by the great heat of the chemical
action.
Again, it is easy to show that just as the carbon dioxide
and water produced by the combustion of a candle are
heavier than the candle, so the white powder produced
by burning a piece of magnesium ribbon weighs more
than the ribbon. The discovery that the products of
combustion are heavier than the combustible substance
was really a very important one in the history of chemistry ;
for up to about 120 years ago it was generally supposed
that a combustible substance contained something called
phlogiston, which came out of the substance when it was
burned. It was the famous French chemist Lavoisier who
finally overthrew this theory, and emphasised the fact
that instead of losing anything when it was burned, a
combustible substance actually became heavier.
The meaning of the term “ combustion ” has been ex-
tended in the foregoing paragraphs so that the burning
of coal and the burning of magnesium are brought under
the same category. We may now extend the term still
further to cover many chemical processes, which, although
they do not very obviously produce light and heat, yet
depend essentially on the same chemical phenomenon,
namely, the combination of some substance with the
oxygen of the atmosphere. These are cases of slow com-
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