Handbook of Hydrocarbon and Lipid Microbiology 2010
DOI: 10.1007/978-3-540-77587-4_166
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Coal, Coal Mines and Spoil Heaps

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Cited by 11 publications
(6 citation statements)
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“…Increased pressure and temperature alter the physical and chemical characteristics of the resulting sediment, which is metamorphosed into coal. Due to the heterogeneity of plant tissue and varying geochemical conditions, the structure of coal will differ between coal seams (Kirby et al, 2010). Coal is mainly composed of organic carbonaceous matter, noted as macerals and inorganic minerals in various proportions.…”
Section: Sulphur In Coalmentioning
confidence: 99%
“…Increased pressure and temperature alter the physical and chemical characteristics of the resulting sediment, which is metamorphosed into coal. Due to the heterogeneity of plant tissue and varying geochemical conditions, the structure of coal will differ between coal seams (Kirby et al, 2010). Coal is mainly composed of organic carbonaceous matter, noted as macerals and inorganic minerals in various proportions.…”
Section: Sulphur In Coalmentioning
confidence: 99%
“…Increased pressure and temperature alter the physical and chemical characteristics of the resulting sediment, which is transformed into coal. Due to the heterogeneity of plant tissue and varying geochemical conditions, the structure of coal will differ between coal seams (Kirby et al, 2010). Almost all the elements of the Chemical Periodic Table can be found in coal.…”
Section: General Facts About Coalmentioning
confidence: 99%
“…Subsequent changes in temperature with depth under overlying strata and pressure modify the physical and chemical characteristics of the sedimentary environment, during which the peat transforms into lignite and higher-ranking coals. Variations in geochemical conditions and the heterogeneity of plant tissues contribute to different coal types (Kirby et al, 2010), which comprise varying proportions of macerals (organic components) and inorganic minerals. The primary maceral groups are the huminite to vitrinite, exinite or liptinite, and inertinite groups (Stach et al, 1982;Diessel, 1992;Taylor et al, 1998;Speight, 2013;Flores & Moore, 2024).…”
Section: Introductionmentioning
confidence: 99%