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Enamels and enamelling; an introduction to the preparation and ...

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BAW MATERIALS FOR THE MANUFACTURE OF ENAMELS. 15<br />

Consequently, <strong>the</strong> materials used for making glass must<br />

contain one or o<strong>the</strong>r of <strong>the</strong> above-mentioned compounds.<br />

The matrix of enamel must also contain a very finely<br />

divided infusible white subst<strong>an</strong>ce, generally tin oxide or bone<br />

ash, <strong>to</strong> render <strong>the</strong> glass opaque :<br />

<strong><strong>an</strong>d</strong>, as one or o<strong>the</strong>r of <strong>the</strong>se<br />

is <strong>an</strong> essential constituent of all enamels, <strong>the</strong>y<br />

must also be<br />

reckoned among <strong>the</strong> fundamental materials. As <strong>the</strong> success<br />

of <strong>the</strong> resulting product depends on <strong>the</strong> suitability of <strong>the</strong>se<br />

materials, a more precise account of <strong>the</strong>ir properties <strong><strong>an</strong>d</strong><br />

method of <strong>preparation</strong> will now be given.<br />

Silica.<br />

This subst<strong>an</strong>ce is one of <strong>the</strong> most extensively distributed<br />

bodies met with in our pl<strong>an</strong>et, being not only a main con-<br />

stituent of <strong>the</strong> rocks (e.g., gr<strong>an</strong>ite <strong><strong>an</strong>d</strong> gneiss) forming <strong>the</strong><br />

highest <strong><strong>an</strong>d</strong> largest mountains in <strong>the</strong> world, but also occur-<br />

ring in a pure state in numerous deposits.<br />

The minerals, rock crystal, quartz <strong><strong>an</strong>d</strong> quartz s<strong><strong>an</strong>d</strong>,<br />

as well as flint, consist of almost perfectly pure silica ; as<br />

do also <strong>the</strong> minerals known under <strong>the</strong> names of amethyst<br />

(violet), citrin (yellow), smoky <strong>to</strong>paz <strong><strong>an</strong>d</strong> morion (smoke brown<br />

<strong>to</strong> black), <strong>the</strong> only admixture being <strong>the</strong> minute proportion of<br />

extr<strong>an</strong>eous matter producing <strong>the</strong> particular colour in each<br />

case.<br />

From <strong>the</strong> chemical point of view, silica is composed of silicon<br />

{Si) <strong><strong>an</strong>d</strong> oxygen (O 2 ) = SiO 2 . There are two allotropic modifica-<br />

tions of this body : <strong>the</strong> crystalline (found almost pure, as rock<br />

-crystal <strong><strong>an</strong>d</strong> quartz), <strong><strong>an</strong>d</strong> <strong>the</strong> amorphous form -e.g., flint, hyalite<br />

<strong><strong>an</strong>d</strong> opal.<br />

Silica belongs <strong>to</strong> <strong>the</strong> class of bodies that are infusible when<br />

heated alone. It is inert <strong>to</strong>wards o<strong>the</strong>r subst<strong>an</strong>ces, <strong><strong>an</strong>d</strong> is<br />

unattacked by <strong>the</strong> strongest acids ;<br />

in fact <strong>the</strong>re are only two<br />

bodies capable of acting upon it at all, viz., hydrofluoric acid<br />

<strong><strong>an</strong>d</strong> <strong>the</strong> alkalies. On boiling quartz in a solution of caustic

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