Characteristics of Coal
The characteristics of coals that determine classification and suitability for given applications are the proportions of :
1. volatile matter
2. fixed carbon
3. moisture
4. sulfur
5. ash
Each of these is reported in the proximate analysis. Coal analyses can be reported on several bases: as-received, moisture-free (or dry), and mineral-matter-free (or ash-free). As-received is applicable for combustion calculations; moisture-free and mineral-matter-free, for classification purposes.
Volatile matter is driven off as gas or vapor when the coal is heated according to a standard temperature test. It consists of a variety of organic gases, generally resulting from distillation and decomposition. Volatile products given off by coals when heated differ materially in the ratios (by mass) of the gases to oils and tars. No heavy oils or tars are given off by anthracite, and very small quantities are given off by semianthracite. As volatile matter in the coal increases to as much as 40% of the coal (dry and ash-free basis), increasing amounts of oils and tars are released. However, for coals of higher volatile content, the quantity of oils and tars decreases and is relatively low in the subbituminous coals and in lignite.
Fixed carbon is the combustible residue left after the volatile matter is driven off. It is not all carbon. Its form and hardness are an indication of fuel coking properties and, therefore, guide the choice of combustion equipment. Generally, fixed carbon represents that portion of fuel that must be burned in the solid state.
Moisture is difficult to determine accurately because a sample can lose moisture on exposure to the atmosphere, particularly when reducing the sample size for analysis. To correct for this loss, total moisture content of a sample is customarily determined by adding the moisture loss obtained when air-drying the sample to the measured moisture content of the dried sample. Moisture does not rep-resent all of the water present in coal; water of decomposition (combined water) and of hydration are not given off under standardized test conditions.
Ash is the noncombustible residue remaining after complete coal combustion. Generally, the mass of ash is slightly less than that of mineral matter before burning. Sulfur is an undesirable constituent in coal, because the sulfur oxides formed when it burns contribute to air pollution and cause combustion system corrosion.
N. Berkowitz has written: 'Coal gasification' -- subject(s): Coal gasification 'Coal research and development in Canada, 1968'
R. B. Townshend has written: 'The complete air-gunner'
Miles Tomalin has written: 'Coal mines and miners' -- subject(s): Coal mines and mining
It means eyes, black like coal. Bitumen is the British term for coal.
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Coal in the midlands
The grain size of coal can vary, but it typically ranges from fine particles to larger chunks. Coal can be classified based on its grain size as fine, medium, or coarse coal. The grain size of coal can impact its combustion efficiency and handling characteristics.
Soft coal, also known as bituminous coal, is a type of coal that is relatively soft and contains a higher percentage of carbon and volatile matter compared to harder coal types like anthracite. It is commonly used as a fuel source for power generation and heating due to its higher energy content. Soft coal is also known for its smokey burning characteristics.
The amount of coal needed to produce 1 ton of fly ash varies depending on the characteristics of the coal and the combustion process. On average, it takes about 10-20% of the original coal weight to result in 1 ton of fly ash.
A classified coal group refers to categorizing coal based on its properties and characteristics, such as moisture content, sulfur content, energy content, and caking properties. This classification helps in determining the best use for the coal and its quality for different end uses. Examples of classified coal groups include anthracite, bituminous, and lignite.
Anthracite coal is a type of coal that is hard, shiny, and has a high carbon content (over 87%). It is known for burning cleanly with little smoke or odor, making it a preferred choice for residential heating. Anthracite coal is also the oldest and rarest form of coal, formed over millions of years of intense pressure and heat.
Anthracite coal requires the most intense pressure to form, as it is the highest rank of coal with the greatest degree of metamorphism and carbon content. This process typically involves higher temperatures and pressures compared to other types of coal, resulting in its hard and lustrous characteristics.
J. A. Cavallaro has written: 'Washability characteristics of Arkansas and Texas lignites' -- subject(s): Lignite, Coal, Desulfurization 'A washability and analytical evaluation of potential pollution from trace elements in coal' -- subject(s): Coal, Analysis, Trace elements
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P. L. Lorio has written: 'Relationship of tree survival and yield to coal-spoil characteristics'