Chemists -- England -- Biography; Priestley, Joseph, 1733-1804
It would be interesting to know the sentiments of Lord Shelburne, then
in the cold shade of retirement, as he perused these passages, and
whether he realised the truth of the little homily from his “tame
philosopher.”
The preface is followed by an introduction, in which Priestley gives a
rapid and confessedly imperfect survey of the state of knowledge
concerning “air” prior to 1774. He gives to Boyle the credit of first
clearly recognising that elastic fluids exist differing essentially from
the air of the atmosphere, but agreeing with it in the properties of
weight, elasticity and transparency. But he also points out that two
remarkable kinds of factitious air had long been known to miners, viz.,
_choke damp_, which is heavier than air, which lies at the bottom of
pits, extinguishes flame and kills animals; and the other, called _fire
damp_, which is lighter than common air, is found, therefore, near the
roofs of subterraneous places and is liable to take fire and explode
like gunpowder. “The word _damp_ signifies _vapour_ or _exhalation_ in
the German and Saxon languages.”
“Air of the former kind, besides having been discovered in various
caverns, particularly the Grotta del Cane in Italy, had also been
observed on the surface of fermenting liquors, and had been called
_gas_ (which is the same with _geist_, or _spirit_) by Van Helmont and
other German chemists; but afterwards it obtained the name of _fixed
air_, especially after it had been discovered by Dr Black of Edinburgh
to exist, in a fixed state, in alkaline salts, chalk, and other
calcareous substances.”
Black’s work is dealt with in half a dozen lines, and a passing
reference is made to Macbride and Brownrigg. A very imperfect account is
given of the work of Hales, although it is stated that “his experiments
are so numerous and various that they are justly esteemed to be the
solid foundation of all our knowledge of this subject.” This section
concludes with the mention of Cavendish’s determinations of the relative
weights of fixed air (carbon dioxide), and inflammable air from metals
(hydrogen), and of Lane’s observations that water charged with carbonic
acid will dissolve iron, “and thereby become a strong chalybeate.”
Priestley was the last man in the world to seek to disparage the work of
his predecessors or to minimise what was due to them. In reality he had
the intention, as he distinctly states, to write at his leisure the
history and present state of discoveries relating to air, in a manner
similar to his _History of Electricity_, and of the _Discoveries
Relating to Vision, Light and Colours_, when no doubt he would have done
full justice to all concerned. In the meantime he gives only such
particulars as are necessary, in his judgment, to the understanding of
his own work.
Public-domain text, read in full here on John Shaqi.
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