The Gases of the Atmosphere: The History of Their Discovery — John Shaqi
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
Subsequent experiments with nitric oxide showed that air from red
precipitate or from “_mercurius calcinatus_” (red oxide of mercury
in each case, although prepared in different ways) was “between four
and five times as good as common air.” He proceeds:[6]--“Being now
satisfied with respect to the _nature_ of this new species of air,
viz. that being capable of taking more phlogiston from nitrous air,
it therefore originally contains less of this principle, my next
inquiry was, by what means it comes to be so pure, or, philosophically
speaking, to be so much _dephlogisticated_.” He therefore went on to
heat the various oxides of lead, but without any special results worth
chronicling. On moistening red-lead with nitric acid, however, and
distilling the mixture, he obtained, in successive operations, air
which was “five times as good” as common air. This process formed lead
nitrate, which on distillation yielded nitric peroxide and oxygen; the
gas was, of course, collected over water, which absorbed the peroxide,
allowing pure oxygen to pass. He found that red-lead was not the only
“earth” which produced this effect; but that “flowers of zinc” (zinc
oxide), chalk, slaked lime, and other substances also gave a gas,
when distilled with nitric acid, which was “better” than common air.
In some cases he broke up nitric acid by heat into water, nitric
peroxide, and oxygen; in others he heated nitrates. His conclusion
is: “_Atmospherical air_, or the thing we breathe, _consists of the
nitrous acid and earth_, with so much phlogiston as is necessary to
its elasticity; and likewise so much more as is required to bring it
from its state of perfect purity to the mean condition in which we find
it.”[7]
When such experiments were made by heating nitrates in a gun-barrel,
“phlogisticated air” was obtained. This was nitrogen, for the iron had
reduced the oxides of the latter, and combining with their oxygen, had
formed nitrogen; moreover, it had absorbed to a greater or less extent
the oxygen simultaneously produced.
Having concluded that respirable air was a compound of nitrous acid,
phlogiston, and earth, Priestley endeavoured to ascertain what was the
nature of this earth. He concludes “that the _metallic earths_, if free
from phlogiston, are the most proper, and next to them the _calcareous
earths_.”
“Dephlogisticated air may be procured from any kind of earth with which
the spirit of nitre will unite.” A few quantitative experiments would
surely have refuted this erroneous conclusion. Those which he attempted
to make were very crude. A bladder (of which he does not give the
capacity) was filled with
Phlogisticated air, and weighed 7 dwts. 15 grs.
Nitrous air " " 7 " 16 "
Common air " " 7 " 17 "
Dephlogisticated air " " 7 " 19 "
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