The Gases of the Atmosphere: The History of Their DiscoveryRamsay, William
History
The Gases of the Atmosphere: The History of Their Discovery
Ramsay, William
Air; Argon; Chemistry -- History
After an account of some experiments showing that magnesia is not
identical with lime or with alumina, he proceeds:--“It is sufficiently
clear that the calcareous earths in their native state, and that the
alkalis and _magnesia_ in their ordinary condition, contain a large
quantity of fixed air; and this air certainly adheres to them with
considerable force, since a strong fire is necessary to separate it
from _magnesia_, and the strongest is not sufficient to expel it
entirely from fixed alkalis, or take away their power of effervescing
with acid salts.
“These considerations led me to conclude that the relation between
fixed air and alkaline substances was somewhat similar to the relation
between these and acids: that as the calcareous earths and alkalis
attract acids strongly, and can be saturated with them, so they also
attract fixed air, and are, in their ordinary state, saturated with it;
and when we mix an acid with an alkali, or with an absorbent earth,
that the air is then set at liberty, and breaks out with violence;
because the alkaline body attracts it more weakly than it does the
acid, and because the acid and air cannot both be joined to the same
body at the same time.... Crude lime was therefore considered as a
peculiar acrid earth, rendered mild by its union with fixed air; and
quicklime as the same earth, in which, by having separated the air, we
discover that acrimony or attraction for water, for animal, vegetable,
and for inflammable substances.”
The solubility of slaked lime in water is next discussed. If a solution
of lime “be exposed to the open air, the particles of quicklime which
are nearest the surface gradually attract the particles of fixed air
which float in the atmosphere.”
Black next points out that, on mixing _magnesia alba_ with lime-water,
the air leaves the magnesia and joins itself to the lime; and as both
magnesia and calcium carbonate are insoluble in water, the water is
left pure. Similarly quicklime deprives alkalies of their air and
renders them caustic. And it follows that if caustic alkali be added
to a salt of magnesia or of lime, it will separate the magnesia or the
calcareous earth from the acid, in a condition free from “air” but
combined with water.
Public-domain text, read in full here on John Shaqi.
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