Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meaningsLoomis, Frederic Brewster
Science
Field book of common rocks and minerals : $b for identifying the rocks and minerals of the United States and interpreting their origins and meanings
Loomis, Frederic Brewster
Minerals -- United States; Rocks -- United States
Fire clays may or may not have iron oxides in them, but they must be
free or nearly free from fluxing materials, such as lime, magnesia and
the alkalies (sodium and potassium compounds). They may be more or less
plastic, the essential quality being their ability to withstand high
temperatures without fusing. Silica (as sand) tends to diminish the
refractory quality; so that a clay otherwise suitable, if it has sand in
it, becomes at best a second grade fire clay. In coal mining sections it
is customary to term those beds of clay either above or below the coal,
“fire clay”; but this is an unfortunate designation, for though some of
them are true fire clays, the most of them are not.
Stone-ware clays are those with considerable sand and up to five per
cent of fluxing materials. They must be plastic enough to be readily
worked, and then burn to a dense body at comparatively low temperatures.
Sewer-pipe clays must be plastic, and carry a considerable amount of
fluxing material, as the surface of the pipe is expected to vitrify in
the burning.
Brick clays are low grade clays and vary greatly in composition. The
main requisites are that they mould easily and bake hard at relatively
low temperatures with as little warping and cracking as possible. As
most clays shrink both in the air drying and in the baking, sand is
added when the clay is being mixed. The color is mostly due to the
presence of iron impurities. If there are iron oxides and little or no
lime, the brick bakes to a red color, but if there is an excess of lime
over the iron oxides, it bakes to a cream or buff color, which on
vitrifying turns green.
Paving-brick clays range from surface clays, to semirefractory clays,
shale being often used. The essential component is enough fluxing
material, so that the bricks shall begin to vitrify, or fuse, at not too
high temperatures.
Slip clays are those with a high percentage of fluxing material; so
that, when baked at moderate temperatures, the surface fuses into a
glassy brown or green glaze.
Adobe is an impure calcareous clay, widely used in the western United
States for making sun-dried bricks.
Gumbo is a term applied to fine-grained plastic clays which shrink too
much in the burning to be useful in manufactures. They can be burned to
make an excellent ballast for railroads and highways. They are
especially abundant in the Middle Western States.
Loess
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