Page:The New International Encyclopædia 1st ed. v. 05.djvu/89

COAL. the heating power of coal is its most important property, this is often tested by means of an apparatus known as a ‘calorimeter.’ (See .) The principle of the test depends on the determination of the weight of water which can be converted into steam at 212° F. under atmospheric pressure with one pound of coal. (See also .) In addition to the varieties of coal given above, there may be mentioned semi-bituminous coal and cannel coal. The properties of the different varieties are as follows:

Anthracite contains 84 per cent. or more of fixed carbon, and also little ash, sulphur, and moisture. It has great heating power, and burns with a smokeless flame. Owing to its comparative scarcity, it commands a higher price than the bituminous. Anthracite is dense, has a shining lustre, and usually breaks with a smooth conchoidal fracture. It is estimated by some geologists that about ten inches of peat is required to make one inch of anthracite coal. In the United States anthracite coal is confined chiefly to the eastern edge of the Appalachians in Pennsylvania, where the folding of the rocks has been very intense, and where the coal-seams have been subjected to great pressure. It is also known in Colorado, near Crested Butte, where the bituminous coals have been locally changed to anthracite by the heat of basalt intrusions. It is mined extensively in England, and large quantities are known in China.

Bituminous Coal contains 50 to 75 per cent. of fixed carbon, and 25 to 30 per cent. volatile hydrocarbons. It burns with a rather long and smoky flame, and is also much used for steaming purposes. Many bituminous coals have the property of coking or caking (see ) when heated to redness. Most of the Carboniferous and many of the Mesozoic coals of the United States are bituminous.

Semi-Bituminous Coal resembles bituminous coal in appearance, but is intermediate between it and anthracite. It contains from 70 to 84 per cent. of fixed carbon, and is considered of superior value for steaming purposes. This variety is obtained from Pennsylvania, Maryland, and West Virginia.

Cannel Coal is a variety of coal very rich in volatile hydrocarbons, and found sparingly in parts of Kentucky, Ohio, and Indiana. Its chief use is as a gas-enricher, since it yields 8000 to 15,000 cubic feet of gas per ton. Cannel coal is so called because it burns with a bright flame like a candle, and the name parrot coal was given to it in Scotland, from the crackling or chattering noise it makes while burning. It is very compact in texture and may even have an oily look; certain forms found in England admit of being polished, and ornamental articles have been made from them and sold under the name of jet.

Lignite, or Brown Coal, is a partially formed coal, containing much moisture and volatile matter. It often shows the woody structure of peat and burns very easily, but gives off little heat.

. The value of coal does not seem to have been known to the ancients, nor is it well known at what time it began to be used for fuel. Some say that it was used by the ancient Britons; at all events, it was an article of household consumption to some extent during the Anglo-Saxon period as early as 852. There seems to be reason for thinking that England was the first European country in which coal was used in any considerable quantities. In America the deposits near Richmond, Va., were discovered in 1701, and mining was begun in 1750, while anthracite was first produced in 1793. Extended coal-mining in the United States did not really begin, however, until about 1820. Since that time up to the present, the increase has been about 3500 per cent. In 1822 the amount of coal mined in Virginia was about 48,000 long tons. Now the production for the United States is about 270,000,000 short tons, or greater than that of any other country of the world.

Coal is used largely for domestic purposes, either as fuel or, in the form of gas, for illumination. Its use for the latter purpose is, however, not so widespread as formerly, water-gas having superseded it to a considerable extent. In the production of steam for motive power it also finds important applications. It is furthermore widely employed in the metallurgical industry in the form of either coal or coke, and in this connection may serve both as a fuel and as a reducing agent. (q.v.) is made only from bituminous coal. Lignite seldom has much value as a fuel, owing to the large percentage of moisture that it contains. Because of this moisture it tends to crack in drying, and must therefore be used soon after mining, and in localities where it does not require long transportation from mine to market. This is true, for instance, of some of the lignite deposits in Colorado which are near the Denver market, and therefore possess commercial value. Lignite has sometimes been successfully used in the manufacture of producer gas, and indeed even peat has been found adaptable for this purpose.

. The leading coal-producing countries of the present day are the United States, Great Britain, Germany, France, Belgium, Austria-Hungary, and Russia. The Russian coal-fields are probably the most extensive in Europe. In the Far East coal is known in India, the Malay Archipelago, Japan, and China. The coal-fields of the last-named country are probably the greatest in the world, and may become a source of European supply. Up to the present time they have not been developed in a systematic manner. Italy, Spain, Sweden, Australia, New Zealand, Borneo, the Philippine Islands, and many countries in Africa also produce coal; while in America deposits are worked in Canada, Mexico, Chile, and Argentina, and are known to occur in Colombia and Peru. . The coal-fields of the United States are especially extensive; indeed, in some instances the deposits of a single State exceed those of Germany or France in area. They are separable into several regions, the divisions being geographical and not geological. The geological ages of the coals in 1, 2, 3, 4, and 6 (table on next page on next page  below ) are all Carboniferous, except small Triassic areas in Virginia and North Carolina. Those of 5 are Cretaceous and Tertiary.

By far the most important of these regions is the Appalachian, which takes in portions of Pennsylvania, Ohio, West Virginia, Virginia, Maryland, Eastern Kentucky, Eastern Tennessee, Georgia, North Carolina, and Alabama. It is about 750 miles long, and 70 to 80 miles wide. The coals are all bituminous or semi-bituminous with the exception of those at the northeastern end, in Pennsylvania, where close folding of the rocks