Coal: Formation
Formation of Coal |
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To arrive at its present form, coal encountered enormous changes. It began long ago in the formation of plants and other organic material. Those plants died and were covered by layers of sediment. As time passed, heat, weight, and pressure built up on top of the plants, forcing them to change from plants to peat, to coal. Over time, this coal "matured" into higher rank coal. Higher rank coals have less moisture and higher carbon content. Source: Illinois Department of Commerce. American coal mining began in Virginia in 1748. Initially coal was used for home heating and cooking, and coal's use quickly expanded to power steam engines, steam boats, and the railroads. In 1882, the first coal-fueled electrical power station began operations in New York City. Since then, coal use has continued to grow. Today, coal provides approximately half of the electricity in the United States. Coal mining in Alaska can be traced back to the early 1900s during the gold rush years. Visible coal in the Healy area was an obvious source of fuel for steam boats and the railroad operations between Anchorage and Fairbanks. |
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Ranks of Coal |
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There are four main ranks of coal: |
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"Coking coal" describes a specific type of bituminous coal that "cokes" when exposed to high heat in the absence of air. The coking process involves heating coal to draw off volatile substances such as tars and aromatic hydrocarbons. This heating fuses the carbon and residual ash into a hard, grey, porous substance called "coke." Coke is used in the steel-making process as a fuel and reducing agent. Usibelli coal is approximately 8 to 20 million years old. The age of the coal is one factor which determines its contained energy value. At 7,800 BTU Usibelli coal is well suited for use in power plants for steam production which is utilized to spin the electrical turbines and the steam can be utilized for space heat for commercial buildings and structures. This dual use of energy for electricity and heat is called “cogeneration.” |
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