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TRAS 15
Tuesday Jan: 26 I have now before me Bergmans Commentated
Chemica e tertio novorum Societalis Reg. Leicul. Ups. actirum
tomo exerpla. Upsalise
Joh. Edman. Reg. Acad. Typograph 1777. 4to It consists of
two papers: one exhibiting a chemical analysis of the contents and
productions of Volcanos: the other a chem. analysis of the
several sorts of pretious stones. In the first, p. 65 is an
account of the Puzzolana, & which is nearly the same thing,
the Dutch Tras. It gives the theory of the mortar and with those
substances most clearly & perfectly. I have therefore extracted what
relates to these subjects, which is as follows.
16
In two specimens 100 parts of Puzzolana
I | II Silicious
(that is chrystalline) earth 55 | 60 Argillaceous 20 |
29 Calcarious 5 | 6
Calx of iron 20 | 15
100| 100
This substance as every body knows
mixt up with quick lime slacked in water presently grows into a
stone: which most useful property is much illustrated by the account
above given of its composition.
17
The firmness of mortar depends in a general view upon the lime water, with
which the whole
. This attracts the aerial acid
from the atmosphere: which
saturation, the particles which were
separated this is rather obscure) [
haurto sparticula soluta
] grow on as it were to the others and glew them
together, whereas before they were connected only by a kind of
accompanied with a very weak degree of cohesion. This combination is
the sooner effected, the quicker the water evaporates.
18
Common mortar is made with sand a pure silicious earth: the
particles of which being like glass, neither take up water nor
contract
contract any adhesion with any other particles; by which means the whole
mass takes a long time to dry and harden.
19
Now then if instead of sand, the puzzolana
be employ'd, the case is very different. The particles of
the clay not only greedily absorb the water, but by their spongy texture
serve admirably well to connect and fasten with the other
ingredients. Ponder this, there is the calx of iron, and which has still
some portion of phlogiston adhering to it. This, as
has been found by experience, contributes greatly to the
strength of the whole: insomuch that if to your puzzolana
you add fresh quicklime (by which the water is not only
most greedily absorbed, but by means of the heat produced by the mixture
presently drawn off in vapour) the whole mass, if your workmen are
lazy, will harden as they are working it, and become unfit for
use.
20
The Dutch says (which signifies mortar) is very
nearly of the same nature as the
puzzolana except that it contains rather more heterogeneous
matters (
seems to mean silicious earth ) at least that
does which is brought from Ardernack like
somewhere in Germany near the
for besides particles of mica and iron ore
particles of schoerl and granate, &
other substances may also be distinguished by the eye and in some
measure separated by . In general too it contains rather more
calcarious
earth, as appears from its' effervescing more violently in acid.
21
With respect to silicious earth, you are to understand that
the
common clay,
which is brought from Cologne ( which I believe is used for
is commonly half or even 3/4 of it and more,
silicious earth ( See Bergmans
Opuscula Vol. 1. p. 289. Holmise Upsalia &
1779.
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