The Science of BrickmakingHarris, George Frederick
Science
The Science of Brickmaking
Harris, George Frederick
Brickmaking -- Handbooks, manuals, etc.
We should not forget that remarkable substance of which the well-known
Dinas bricks are made. The proportion of silica present ranges from
about 96 to 99 per cent., the remainder consisting principally of
alumina, though traces of iron, lime, and magnesia frequently occur.
There is not, of course, sufficient natural flux for this “clay,” so a
small proportion (2.5 to 3 per cent.) of lime is added, which produces
the desired effect. In other words, if we can obtain a pure siliceous
sand, with hardly any lime, iron or magnesia in it, we have the
material of which the better kinds of fire-bricks are made. Such sandy
earths are not uncommon in the South of England, but strange to relate,
they are not used for the purpose indicated.
The earths from which the superior Stourbridge bricks are made, are
approximately of the following chemical composition:--Silica, 64.10;
alumina, 23.15; iron oxide, 1.85; magnesia, .95; water and loss, 10.00
per cent. It will be observed that the proportion of iron and magnesia
here is very small, whilst lime is altogether absent. It is a most
excellent earth for the purposes for which it is used, and the chemical
results may be taken as a standard for that class of material. Another
Stourbridge earth yields as much as 4.14 per cent. of iron, however,
whilst its proportion of silica is lower, 51.80, and alumina higher,
30.40, which serves to remind us of the variability of even good earths
used in the manufacture of fire-clay goods.
Let us now turn to the consideration of pottery clays, of which the
following results may be taken as typical:--
_Chemical Composition of Pottery Clays._
------------+-------+-------+--------
| 1 | 2 | 3
+-------+-------+--------
Silica | 46.38 | 49.44 | 58.07
Alumina | 38.04 | 34.26 | 27.38
Iron oxide | 1.04 | 7.74 | 3.30
Lime | 1.20 | 1.48 | .50
Magnesia | trace | 1.94 | trace
Water | 13.57 | 5.14 | 10.30
------------+-------+-------+--------
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