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COAL IS ONE of a variety of energy sources that both developed and developing nations use. It is the fossil fuel that is relied upon most heavily for electricity generation in the United States. Organic matter from the Carboniferous period, which occurred approximately 360–286 million years ago, forms currently accessible coal deposits. There are several different types of coal, each with varying degrees of thermal value. In the process of electricity and heat generation, coal combustion releases many pollutants into the air, water, and land. These pollutants include mercury, sulfur oxides, nitrogen oxides, methane, and carbon oxides. The dispersal of such toxins into the environment has many ecological, human health, and economic effects. More specifically, coal combustion contributes to the climate-changing effect of increased atmospheric carbon. Because of this, alternatives to coal combustion are presently being researched and developed. Coal is presently a necessary and inexpensive way of producing electricity and heat; however, the use of this resource has significant consequences.

Types of Coal

There are four main classifications of coal. Each type of coal is formed as a result of the exposure to assorted combinations of temperature and pressure during formation. For instance, coal that was exposed to low temperatures and pressures is usually moister, softer, and has lower energy content. The four coal classifications include lignite, subbituminous, bituminous, and anthracite.

The first type of coal, lignite, is soft with a high moisture content and low thermal value as compared with other types of coal. Lignite is usually light brown to brown-black in color and resembles deteriorating and compressed wood. In the United States, most lignite deposits are found in the western states; specifically, North Dakota is the state that produces the largest amount of lignite. This type of coal is relatively inexpensive and, thus, highly desirable, from an economic standpoint, to fuel electric power plants.

The next classification of coal is subbituminous. This type of coal is the intermediate between lignite and bituminous coal. It has a moisture content of between 20 and 30 percent. This is higher than bituminous coal and anthracite; however it is lower than lignite. Subbituminous is desirable from a pollution standpoint because it has a low relative sulfur and carbon content, but the thermal value of subbituminous coal is low. However, many power plants prefer to burn subbituminous coal, as it provides cleaner energy generation. Subbituminous coal is found primarily in Alaska, Montana, and Wyoming and is recognized by its unpolished black color.

Pollution Controls

Bituminous coal is the third type of coal. Though it is harder than lignite or subbituminous coal, bituminous coal is often referred to as soft coal. This is due to the high sulfur content. Because bituminous coal has such a high amount of sulfur present, electricity generators that choose to burn this type of coal must equip their plants with sophisticated pollution-control systems. These mechanisms are called scrubbers because they scrub the pollution from the air by binding reactive toxins with inert, calcium-based substances located in the air stacks of power plants. The best available technology allows scrubbers to remove 98 percent of all sulfur emissions and 99 percent of all particulate matter from smoke stacks. Bituminous coal is dark black in color and may have dull-black bands striated throughout. This type of coal is typically found in Appalachian Mountain regions, the Great Lakes, the Mississippi Valley, and north and central Texas.

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