Coal


Coal is a fossil fuel extracted from the ground either by underground mining or strip mining. It is a readily combustible black or brownish-black sedimentary rock. It is composed primarily of carbon and hydrocarbons, along with assorted other elements, including sulfur. Often associated with the Industrial Revolution, coal remains an enormously important fuel and is the most common source of electricity world-wide. In the United States, for example, the burning of coal generates over half the electricity consumed by the nation.

Contents

4.1 Anthracite coal
4.2 Bituminous coal
4.3 Lignite coal
4.4 Sub-bituminous coal
4.5 Coke
4.6 Jet

Etymology and folklore

Coal is thought ultimately to derive its name from the Old English col but this actually meant charcoal at the time; coal was not mined prior to the late Middle Ages; i.e. after ca. 1000 AD. Mineral coal was referred to as sea-coal since it was found washed up on beaches occasionally.

It is associated with the astrological sign Capricorn. It is carried by thieves to protect them from detection and to help them to escape when pursued. It is an element of a popular ritual associated with New Year's Eve. To dream of burning coals is a symbol of disappointment, trouble, affliction and loss, unless they are burning brightly, when the symbol gives promise of uplifting and advancement.

Santa Claus is said to leave a lump of coal instead of Christmas presents in the stockings of naughty children.

Composition and creation

Coal consists of more than 50 percent by weight and more than 70 percent by volume of carbonaceous material (including inherent moisture). Coal is formed from plant remains that have been compacted, hardened, chemically altered, and metamorphosed by heat and pressure over geologic time. It is suspected that coal was formed from ancient plants that grew in swamp ecosystems. When such plants died, their biomass was deposited in anaerobic, aquatic environments where low oxygen levels prevented their decay and oxidation (rotting and release of carbon dioxide). Successive generations of this type of plant growth and death formed thick deposits of unoxidized organic matter that were subsequently covered by sediments and compacted into carbonaceous deposits such as peat or bituminous or anthracite coal. Evidence of the types of plants that contributed to carbonaceous deposits can occasionally be found in the shale and sandstone sediments that overlie coal deposits, and with special techniques, within the coal itself. The greatest coal-forming time in geologic history was during the Carboniferous era (280 to 345 million years ago).

Uses

Coal is primarily used as a solid fuel to produce heat through combustion. Combustion of coal, like any other carbon containing compond, produces carbon dioxide (CO2), along with varying amounts of sulfur dioxide (SO2) depending on where it was mined. Sulfur dioxide reacts with water to form sulfurous acid. If sulfur dioxide is discharged into the atmosphere, it reacts with water vapor and is eventually returned to the Earth as acid rain.

Coal also contains many trace elements, including arsenic and mercury, which are dangerous if released into the environment. Coal also contains low levels of uranium, thorium, and other naturally-occurring radioactive isotopes whose release into the environment may lead to radioactive contamination (see [1](http://www.ornl.gov/info/ornlreview/rev26-34/text/colmain.html) and [2](http://greenwood.cr.usgs.gov/energy/factshts/163-97/FS-163-97.html) for numbers and details). While these substances are trace impurities, if a great deal of coal is burned, significant amounts of these substances are released.

When coal is used in electricity generation, the heat is used to create steam, which then is used to power turbine generators. Approximately 40% of the Earth's current electricity production is powered by coal, and the total known deposits recoverable by current technologies are sufficient for at least 300 years' use. Emissions from coal-fired power plants represent the largest source of artificial carbon dioxide emissions, according to most climate scientists a primary cause of global warming. Many other pollutants are present in coal power station emissions. Some studies claim that coal power plant emissions are responsible for tens of thousands of premature deaths annually in the United States alone. In addition, emissions from coal-fired power plants are a major contributor to acid rain in some countries. Modern power plants utilize a variety of techniques to limit the harmfulness of their waste products and improve the efficiency of burning, though these techniques are not widely implemented in some countries, as they add to the capital cost of the power plant.

In the past, coal was converted to make coal-gas, which was piped to customers to burn for illumination, heating, and cooking. At present, the safer natural gas is used instead. Coal can also be converted into liquid fuels like gasoline or diesel. The Bergius process (direct liquefaction by hydrogenation) was used in Nazi Germany, and for many years in South Africa - in both cases, because those regimes were politically isolated and unable to purchase crude oil on the open market. Estimates of the cost of producing liquid fuels from coal indicate that domestic US production of fuel from coal becomes cost-competitive with oil priced at around 35 USD per barrel [3](http://www.findarticles.com/p/articles/mi_m0CYH/is_15_6/ai_89924477), which is well above historical averages - but is now viable due to the spike in oil prices in 2004 and nanotechnology [4](http://www.coalpeople.com/old_coalpeople/march03/tiny_tomorrow.htm). There is another process to manufacture oil from coal called low temperature carbonization (LTC). The process was perfected by Lewis Karrick, an oil shale technologist at the U.S. Bureau of Mines in the 1920s.[5](http://www.rexresearch.com/karrick/karric~1.htm)

Types of coal

Anthracite coal

Anthracite coal is the highest rank of coal; used primarily for residential and commercial space heating. It is hard, brittle, and black lustrous coal, often referred to as hard coal, containing a high percentage of fixed carbon and a low percentage of volatile matter. The moisture content of fresh-mined anthracite generally is less than 15 percent. The heat content of anthracite ranges from 22 to 28 million Btu/ton (26 to 33 MJ/kg) on a moist, mineral-matter-free basis. The heat content of anthracite coal consumed in the United States averages 25 million Btu/ton (29 MJ/kg), on the as-received basis (i.e., containing both inherent moisture and mineral matter). Note: Since the 1980s, anthracite refuse or mine waste has been used for steam electric power generation. This fuel typically has a heat content of 15 million Btu/ton (17 MJ/kg) or less.

Bituminous coal

Bituminous coal is a dense coal, usually black, sometimes dark brown, often with well-defined bands of bright and dull material, used primarily as fuel in steam-electric power generation, with substantial quantities also used for heat and power applications in manufacturing and to make coke. Bituminous coal is the most abundant coal in active U.S. mining regions. Its moisture content usually is less than 20 percent. The heat content of bituminous coal ranges from 21 to 30 million Btu/ton (24 to 35 MJ/kg) on a moist, mineral-matter-free basis. The heat content of bituminous coal consumed in the United States averages 24 million Btu/ton (28 MJ/kg), on the as-received basis (i.e., containing both inherent moisture and mineral matter).

Lignite coal

Lignite coal is the lowest rank of coal, often referred to as brown coal, used almost exclusively as fuel for steam-electric power generation. It is brownish-black and has a high inherent moisture content, sometimes as high as 45 percent. The heat content of lignite ranges from 9 to 17 million Btu/ton (10 to 20 MJ/kg) on a moist, mineral-matter-free basis. The heat content of lignite consumed in the United States averages 13 million Btu/ton (15 MJ/kg), on the as-received basis (i.e., containing both inherent moisture and mineral matter).,

Sub-bituminous coal

Sub-bituminous coal is a coal whose properties range from those of lignite to those of bituminous coal and are used primarily as fuel for steam-electric power generation. It may be dull, dark brown to black, soft and crumbly at the lower end of the range, to bright, jet-black, hard, and relatively strong at the upper end. Subbituminous coal contains 20 to 30 percent inherent moisture by weight. The heat content of subbituminous coal ranges from 17 to 24 million Btu per ton on a moist, mineral-matter-free basis. The heat content of subbituminous coal consumed in the United States averages 17 to 18 million Btu/ton (20 to 21 MJ/kg), on the as-received basis (i.e., containing both inherent moisture and mineral matter). A major source of subbituminous coal in the United States is the Powder River Basin in Wyoming.

Coke

>Coke is a solid carbonaceous residue derived from low-ash, low-sulfur bituminous coal from which the volatile constituents are driven off by baking in an oven without oxygen at temperatures as high as 2,000 F (1,000 C) so that the fixed carbon and residual ash are fused together. Coke is used as a fuel and as a reducing agent in smelting iron ore in a blast furnace. Coke from coal is grey, hard, and porous and has a heating value of 24.8 million Btu/ton (29 MJ/kg). Byproducts of this conversion of coal to coke include coal-tar, ammonia, light oils, and "coal-gas". (Coke can also be made from petroleum)

Jet

Jet is a compact form of lignite that is sometimes polished and has been used as an ornamental stone since the Iron Age.

World coal reserves

It has been estimated that, as of 1996, there are around one exagram (1 1015 kg) of total coal reserves economically accessible using current mining technology, approximately half of it being hard coal. The energy value of all the world's coal is well over 100,000 quadrillion Btu (100 zettajoules). There probably is enough coal to last for 300 years.

The United States Department of Energy uses estimates of coal reserves in the region of 1,081,279 million short tons, which is about 4,786 BBOE (billion barrels of oil equivalent) ([6](http://www.eia.doe.gov/emeu/iea/res.html)). The amount of coal burned during 2001 was calculated as 2.337 GTOE (gigatonnes of oil equivalent), which is about 46 MBOED (million barrels of oil equivalent per day) ([7](http://www.iea.org/dbtw-wpd/bookshop/add.aspx?id=144)). At that rate those reserves will last 285 years. As a comparison natural gas provided 51 MBOED, and oil 76 MBD (million barrels per day) during 2001.

See also

  • Major coal producing regions.
  • Major coal exporters.
  • Coal mining techniques.
  • Coaldust
  • Coal-tar
  • Coal Measure (stratigraphic unit)
  • List of rocks
  • Fluidized bed combustion
  • Calorific Value of Coal
  • Granular material
  • Future energy development

External links

Other uses

Coal is also a color.




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