Online Encyclopedia

ANTHRACITE (Gr. avOpaE, coal)

Online Encyclopedia
Originally appearing in Volume V02, Page 106 of the 1911 Encyclopedia Britannica.
Spread the word: del.icio.us del.icio.us it!

ANTHRACITE (Gr. avOpaE,
See also:
coal)
  , a
See also:
term applied to those varieties of
See also:
coal which do not give off tarry or other
See also:
hydrocarbon vapours when heated below their point of ignition; or, in other words, which burn with a smokeless and nearly non-luminous flame . Other terms having the same meaning are, " stone coal " (not to be confounded with the German Steinkohle) or "blind coal " in Scotland, and "Kilkenny coal " in Ireland . The imperfect anthracite of north Devon, which however is only used as a pigment, is known as
See also:
calm, the same term being used in
See also:
geological classification to distinguish the strata in which it is found, and similar strata in the Rhenish hill countries which are known as the
See also:
Culm
See also:
Measures . In
See also:
America, culm is used as an
See also:
equivalent for waste or slack in anthracite
See also:
mining . Physically, anthracite differs from ordinary bituminous coal by its greater hardness, higher density, 1.3-1.4, and lustre, the latter being often semi-metallic with a somewhat brownish reflection . It is also
See also:
free from included soft or fibrous notches and does not
See also:
soil the fingers when rubbed . Structurally it shows some alteration by the development of secondary divisional planes and fissures so that the
See also:
original stratification lines are not always easily seen . The thermal conductivity is also higher, a lump of anthracite feeling perceptibly colder when held in the warm hand than a similar lump of bituminous coal at the same temperature . The chemical composition of some typical anthracites is given in the article COAL . Anthracite may be considered to be a transition stage between ordinary bituminous coal and
See also:
graphite, produced by the more or less
See also:
complete elimination of the volatile constituents of the former; and it is found most abundantly in areas that have been subjected to considerable earth-movements, such as the flanks of
See also:
great mountain ranges . The largest and most important anthracite region, that of the north-eastern portion of the Pennsylvania coal-field, is a good example of this; the highly
See also:
con torted strata of the Appalachian region produce anthracite exclusively, while in the western portion of the same basin on the
See also:
Ohio and its tributaries, where the strata are undisturbed, free-burning and coking coals, rich in volatile
See also:
matter, prevail . In the same way the anthracite region of South Wales is confined to the contorted portion west of
See also:
Swansea and
See also:
Llanelly, the H CH central and eastern portions producing steam, coking and house coals .

Anthracites of newer,

See also:
tertiary or cretaceous age, are found in the Crow's
See also:
Nest
See also:
part of the Rocky Mountains in
See also:
Canada, and at various points in the
See also:
Andes in Peru . The
See also:
principal use of anthracite is as a smokeless fuel . In the eastern
See also:
United States, it is largely employed as domestic fuel, usually in close stoves or furnaces, as well as for steam purposes, since, unlike that from South Wales., it does not decrepitate when heated, or at least not to the same extent . For proper use, however, it is necessary that the fuel should be supplied in pieces as nearly
See also:
uniform in
See also:
size as possible, a condition that has led to the development of the breaker which is so characteristic a feature in
See also:
American anthracite mining (see COAL) . The large coal as raised from the mine is passed through breakers with toothed rolls to reduce the lumps to smaller pieces, which are separated into different sizes by a
See also:
system of graduated
See also:
sieves, placed in descending order . Each size can be perfectly well burnt alone on an appropriate grate, if kept free from larger or smaller admixtures . The
See also:
common American classification is as follows: Lump, steamboat, egg and
See also:
stove coals, the latter in two or three sizes, all three being above 12 in. size on round-hole screens . Chestnut below 1i inch above i. inch . ,r ++ S;'! rr From the
See also:
pea size downwards the principal use is for steam purposes . In South Wales a less elaborate classification is adopted; but great care is exercised in hand-picking and cleaning the coal from included particles of
See also:
pyrites in the higher qualities known as best malting coals, which are used for kiln-drying malt and hops . Formerly, anthracite was largely used, both in America and South Wales, as blast-
See also:
furnace fuel for iron smelting, but for this purpose it has been largely superseded by coke in the former country and entirely in the latter . An important application has, however, been
See also:
developed in the extended use of
See also:
internal combustion motors driven by the so-called "mixed," "poor," " semi-
See also:
water " or " Dowson
See also:
gas " produced by the gasification of anthracite with air and a small proportion of steam .

This is probably the most economical method of obtaining

power known; with an engine as small as 15 horse-power the
See also:
expenditure of fuel is at the
See also:
rate of only r lb per horse-power
See also:
hour, and with larger engines it is proportionately less . Large quantities of anthracite for power purposes are now exported from South Wales to France,
See also:
Switzerland and parts of Germany . (H .

End of Article: ANTHRACITE (Gr. avOpaE, coal)
[back]
ANTHRACENE (from the Greek avOpa, coal)
[next]
ANTHRACOTHERIUM (” coal-animal,” so called from...

Additional information and Comments

There are no comments yet for this article.
» Add information or comments to this article.
Please link directly to this article:
Highlight the code below, right click and select "copy." Paste it into a website, email, or other HTML document.