2017
DOI: 10.1016/j.coal.2017.02.001
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Maceral controls on porosity characteristics of lithotypes of Pennsylvanian high volatile bituminous coal: Example from the Illinois Basin

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Cited by 72 publications
(44 citation statements)
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“…At the end of sorption part of the experiment the carbon dioxide capacity of sample V was 22.4% higher and the carbon dioxide capacity of sample D was 21.7% lower than the value obtained for basic coal sample B. The sorption capacity of samples under investigation are similar to the values obtained for comparable coal samples of clarain and durain by Teng et al (2017) and sample TN researched by Zhao et al (2016).…”
Section: Resultssupporting
confidence: 74%
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“…At the end of sorption part of the experiment the carbon dioxide capacity of sample V was 22.4% higher and the carbon dioxide capacity of sample D was 21.7% lower than the value obtained for basic coal sample B. The sorption capacity of samples under investigation are similar to the values obtained for comparable coal samples of clarain and durain by Teng et al (2017) and sample TN researched by Zhao et al (2016).…”
Section: Resultssupporting
confidence: 74%
“…The same situation can be observed for an aromatic carbon region (1550-1650 cm −1 ). Absorption in this band have a prominent aromatic carbon a peak at 1610 cm −1 (Ibarra et al 1996) and is an indication of conjugated C=C structures which occur in significantly higher numbers in the vitrinite rich sample V in comparison with sample D. Bands in the aliphatic bending region (1350-1450 cm −1 ) (Teng et al 2017) are less prominent for the samples with less vitrinite content. In case of sample D the appearance of an absorption peak at 1030 cm −1 is very likely to represent mineral matter (Zhang et al 2015).…”
Section: Resultsmentioning
confidence: 93%
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