Coal

Coal is a carbonaceous rock which occurs as a result of anaerobic decomposition of plant matter and lithification of the resulting material. Coal occurs in three main forms: anthracite, bituminous coal, and lignite, depending on the degree of lithification. Coal is primarily carbon, with traces of sulfur, oxygen, hydrogen, nitrogen, and other elements. The processes of decomposition and lithification drive off most of the oxygen, hydrogen and nitrogen from the plant material, leaving primarily carbon.

Due to its high carbon content and solid, easily-handled form, coal is used for fuel, and has been for hundreds of years (see history of coal mining). Coal can be burned directly, or it can be converted to coke by anaerobic heating (called coking), which alters the physical properties to provide a more uniform and more combustible product. Coal is used in steelmaking both to provide heat and to add controlled amounts of carbon to the iron.

Economic use

Industrial Revolution

Large-scale exploitation of coal began concurrently with the Industrial Revolution, and coal was one of its primary ingredients. Coal was used to make iron, and later steel, and was used to power steam engines which were used to transport very large quantities of goods (relative to previous animal-driven transport) and to pump out deep mines of coal and iron.

United States

Currently, burning of coal provides about one-quarter of the electric power of the United States, and accounts for about one-quarter of energy use worldwide. About 90% of coal mined in the United States is burned to produce electricity.

China

Coal produces over 80% of China's energy; 2.3 billion metric tons of coal were mined in 2007. Despite the health risks posed by severe air pollution in cities (see Beijing) and international pressure to reduce greenhouse emissions, China’s coal consumption is projected to increase in line with its rapid economic growth. Most of the coal is mined in the western provinces of Shaanxi and Shanxi and the northwestern region of Inner Mongolia. However most coal customers are located in the industrialized southeastern and central coastal provinces, so coal must be hauled long distances on China’s vast but overextended rail network. More than 40% of rail capacity is devoted to moving coal, and the country has been investing heavily in new lines and cargo-handling facilities in an attempt to keep up with demand. Despite these efforts, China has suffered persistent power shortages in industrial centers for more than five years as electricity output failed to meet demand from a booming economy. Demand for electricity increased 14% in 2007. Severe snowstorms in late January 2008 seriously disrupted the rail and electrical systems, at a time when some 200 million city workers were attempting to visit their home villages during the Lunar New Year holiday.

Coal mining

see Coal mining, history of

Coal deposits are found in many places around the world, though the deposits which have had the largest economic impacts are those in the Rhine/Ruhr area of Germany, Wales and the Midlands of England, and numerous parts of the U.S., especially Pennsylvania (in the 19th century) and Wyoming (in ther 21st century). Currently, coal production in China is rapidly increasing to meet soaring demand from China's industrialization.

Coal mining takes two forms: open-pit, or strip, mines, and deep mines. Open-pit mines are used when coal deposits are shallow; overburden deposits are removed from the site, and coal is excavated from the ground in what becomes large pits. These mines can become quite deep, and when open-pit mines are played out, the mining company often abandons the site with no restoration. Deep mines are similar to those for any other mineral deposit found deep enough in the earth that the cost of removing the overburden is prohibitive. Shafts are dug and veins of coal are excavated and transported to the surface.

Coal mining is hazardous work in isolated locations. High degrees of solidarity among miners led to the formation of labor unions.