Coking. Coking coal is an essential raw material for the production of iron and steel. Coke is a solid carbonaceous residue formed from coking coal (a lowash, lowsulphur bituminous coal, also known as metallurgical coal), which is used in make steel and other iron products [].Coke is produced by burning coal at temperatures up to 1000 °C in the absence of oxygen to remove the volatile ...
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coal produced in the United States is subbituminous. Wyoming is the leading source of subbituminous coal. Bituminous coal contains 4586 percent carbon, and has two to three times the heating value of lignite. Bituminous coal was formed under high heat and pressure. Bituminous coal in the United States is between 100 to 300 million years old.
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Manufacturing process. Coal tar is obtained by cooling the gas that is formed during the destructive distillation of coal to approximately ambient temperature. It is a black, viscous liquid composed primarily of a complex mixture of condensedring aromatic hydrocarbons.
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Coal is physically, chemically, and thermally altered peat. Peat is partially decayed plant material, mineral matter, and water, which accumulates in anoxic swamps or mires (peatforming wetlands). Peats generally have organic contents greater than 75%, inorganic mineral contents less than 25%, and water contents of 7590% (Schopf 1966; Jarrett 1983; Clymo 1987; Alpern and deSousa 2002).
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energy through a process known as photosynthesis. When plants die, this energy is usually released as the plants decay. Under conditions favorable to coal formation, however, the decay process is interrupted, preventing the release of the stored solar energy. The energy is locked into the coal.
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Abstract. This chapter describes the process of coalification, which gradually turns plant debris into coal, involving heat, pressure and the effects of time. Chemical changes during peatification and coalification are described, and also structural changes in coal during coalification are covered (cleats and their development).
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Coal formation is a continuing process (some of our newest coal is a mere 1 million years old). Today, in areas such as the Great Dismal Swamp of North Carolina and ia, the Okefenokee Swamp of Georgia, and the Everglades in Florida, plant life decays and subsides, eventually to be covered by silts and sands and other matter. Perhaps millions
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Uses of Coal. It is mainly used to generate heat and electricity. It is used in s and in industries to accomplish various tasks. It is the cheapest source of power fuel. The iron and steel industry depends heavily on fossil fuel for energy. It is also used to produce useful products such as coke, tar, and coal gas.
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Abstract. The transformation of vegetable matter into peat and coal is commonly regarded as proceeding in two steps, called the biochemical and physicochemical stage of coalification (Stach et al. 1982), respectively. Other terms, such as "first and second phase" (Mackowsky 1953), or "diagenetic and metamorphic stage" (Teichmüller 1962 ...
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Coal is a vital component of the world's energy resources, and one that is expected to fill a significant role in meeting our energy needs well into the foreseeable future. Geological science and associated technology are used to find and evaluate the coal resources that will be used to meet these needs, a process referred to as coal exploration,
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Coal is a combustible black or brownishblack sedimentary rock that contains a variable amount of carbon (usually more than 50 wt%) and variable amounts of other elements (mainly hydrogen, sulphur, oxygen and nitrogen) [46]. Unlike mineral rocks, which are composed of inorganic material, coal is formed over millions of years by
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process itself, and also improves heat exchange and the recovery of waste products. Better heat exchange and a better degree of coal mixing in the fluidized bed allow for the lowering of the process temperature in relation to conventional pulverized combustion, which, in turn, allows for the lowering of the emission of nitrogen oxides.
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The main factors that influence the coalification process are temperatures, pressures and time of duration. The coalification can be further divided into the diagenesis and metamorphism of coal. The process that makes peat or sapropelite turned into lignite or saprodite is called the diagenesis of coal.
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Coal devolatilization is a process in which coal is transformed at elevated temperatures to produce gases, tar* and char. Gas formation can be related to the thermal decomposition of specific ...
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Examples of unconventional fossil fuels include oil shale, tight oil and gas, tar sands (oil sands), and coalbed methane. Figure e : Conventional oil and natural gas deposits are trapped beneath impervious rock (gray). Conventional natural gas may be associated with oil or nonassociated. Coalbed methane and tight gas found in shale and ...
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Explain the process of the formation of petroleum. Ans. Petroleum was formed from dead organisms that got buried in the sea millions of years ago. These dead bodies got covered with layers of sand and clay.
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Description: Coalification is a geological process of formation of materials with increasing content of the element carbon from organic materials that occurs in a first, biological stage into peats, followed by a gradual transformation into coal by action of moderate temperature (about 500 K) and high pressure in a geochemical stage. Notes:
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Coal is classified as a sedimentary rock. It is a common nonrenewable fuel used mainly in the production of electricity. It is a fossil fuel because it forms from dead plant matter. The quality of coal depends on how it formed; as the organic matter is subjected to greater heat and pressure, the carbon content increases.
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Coal combustion and gasification are the processes to utilize coal for production of electricity and many other applications. Global energy demand is increasing day by day. Coal is an abundant source of energy but not a reliable source as it results into high CO2 emissions. Energy industries are expected to decrease the CO2 emission to prevent global warming. Coal gasification is a process ...
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This collision formed the Appalachian Mountains which at the time reached elevations of 15,000 to 23,000 feet burying the forming coal to great depths. Subsequent glacial action eroded the Appalachians to the highlands they are today. It is estimated that nearly 95% of the anthracite formed in this region eroded away before man began mining coal.
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Coal may be characterized by considering the evolutional process that takes coal from its origin to its eventual use as a resource. The study of coal geology incorporates an understanding of coal formation, coal extraction and utilization, coal quality and environmental considerations, and coal as a source rock for liquid and gaseous hydrocarbons.
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Coal was formed from the remains of ferns, trees, and grasses that grew in great swamps 345 million years ago. These remains formed layers as they sank under the water of the swamps. The plant material partially decayed as these layers formed beds of peat, a soft brown substance that is up to 30% carbon. Peat is the earliest stage of coal ...
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Coal rank and process of coal formation: The transformation of plant material to peat is a biochemical process, the earlier stage of this being due largely to the activity of bacteria (aerobic and anaerobic) and fungi. The transformation of peat to coal, or coalification, is a geochemical process, being
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