New Trends in Coal Science 1988
DOI: 10.1007/978-94-009-3045-2_9
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The Infrared Spectra of Coals, 1980–1986

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Cited by 4 publications
(2 citation statements)
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“…The FTIR spectrum revealed that Himmetoǧlu oil shale was a highly humic material. Major (2926 and 2850 cm -1 ) and additional aliphatic bands (1452 and 1372 cm -1 ) of CH 3 and CH 2 in the form of distinct peaks with comparatively higher intensities than coals, a relatively broad aromatic band at 1625 cm -1 , and succesive aromatic bands between 850 and 675 cm -1 were the particular evidence of the organic matter in the sample. The presence of a significant number of strong and broad functional bands corresponding to hydroxyl, carboxyl, and carbonyl groups also indicate the humic nature of the sample.…”
Section: Resultsmentioning
confidence: 89%
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“…The FTIR spectrum revealed that Himmetoǧlu oil shale was a highly humic material. Major (2926 and 2850 cm -1 ) and additional aliphatic bands (1452 and 1372 cm -1 ) of CH 3 and CH 2 in the form of distinct peaks with comparatively higher intensities than coals, a relatively broad aromatic band at 1625 cm -1 , and succesive aromatic bands between 850 and 675 cm -1 were the particular evidence of the organic matter in the sample. The presence of a significant number of strong and broad functional bands corresponding to hydroxyl, carboxyl, and carbonyl groups also indicate the humic nature of the sample.…”
Section: Resultsmentioning
confidence: 89%
“…The presence of a significant number of strong and broad functional bands corresponding to hydroxyl, carboxyl, and carbonyl groups also indicate the humic nature of the sample. An extremely broad and intense OH band (3422 cm -1 ) and the relatively broad and strong form of the typical carboxyl and carbonyl bands (1710 and 1625 cm -1 ) indicate that the humic content of the oil-shale sample was higher than that in immature coals. , …”
Section: Resultsmentioning
confidence: 96%