A new system of chemical philosophy, Volume 2, Part 1Dalton, John
Science
A new system of chemical philosophy, Volume 2, Part 1
Dalton, John
Atomic theory; Chemistry, Inorganic
I take 24 grains of alum and dissolve them in water; of these 8 grains
may be allowed for sulphuric acid, ⅕ of which = 1.6 grain = 1.1 grain
of lime = 880 grains of lime water, such as I commonly use. To the
solution of alum I put 880 grains of lime water; a slight precipitate
appears which soon becomes redissolved almost completely. The liquid is
then acid by the colour test.
To this liquid I put 880 more of lime water, and agitate; a copious
precipitate appears and continues; after subsidence the clear liquid is
still acid by the colour test.
Another 880 grains are added, and the whole is then well agitated; the
agitation is repeated two or three times after the precipitate has
partly subsided, so as to diffuse it equally again through the liquid;
finally, the clear liquid is found to be neutral by the colour test,
and to contain no alumine; for, lime water produces no precipitate when
poured into it.
Another 880 grains being added, and the whole stirred well, the clear
liquid after the subsidence of the precipitate is still neutral by the
colour test.
The fifth portion of 880 grains being then added, and the mixture well
agitated, a considerable portion of the precipitate will evidently
disappear, and the mixture become semitransparent; after a time the
clear supernatant liquid is found strongly alkaline; a little of it
touched with an acid becomes milky, and adding more acid clears it
again. The liquid is now 1.0025 sp. gr., or a little heavier than lime
water.
The sixth portion of 880 grains being now added to the whole mixture,
and agitated, the precipitate rather diminishes, and an increase of
specific gravity takes place in the liquid; it is now 1.003.
The seventh and last portion of 880 grains being added to the mixture,
and agitation being continued for some time, a dense bulky precipitate
is formed, which falls with great celerity, carrying with it the
greatest part of the acid, the alumine and the lime, and leaving the
liquid of the sp. gr. 1.0012. It is a subsulphate into which acid,
potash, lime and alumine enter, as will be shewn.
These phenomena appear to me to be best explained by adopting a
constitution of alum, such as to make it consist of 1 atom bisulphate
of potash and 3 atoms of sulphate of alumine; after which the following
explanation will apply.
The first portion of lime water saturates the excess of acid.
The second portion throws down a correspondent portion of alumine. The
clear liquid is acid, because it contains sulphate of alumine, which is
essentially acid by the colour test, because alumine is not an alkaline
element.
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