2018
DOI: 10.1016/j.jngse.2018.02.025
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On the fundamental difference of adsorption-pores systems between vitrinite- and inertinite-rich anthracite derived from the southern Sichuan basin, China

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Cited by 23 publications
(16 citation statements)
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“…However, many studies have indicated that a mismatching relationship exists between the methane adsorption capacity and SSA of coal and shale; that is, shale has a larger SSA but lower adsorption capacity (Figure ). This illogical mismatching relationship is due to the SSA in those references only tested by LP‐N 2 GA experiments, which cannot represent the true SSAs of the coal and shale samples. Figure illustrates this illogical mismatching relationship, which indicates that shales have a relatively large BET SSA but a much smaller adsorption capacity.…”
Section: Discussionmentioning
confidence: 99%
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“…However, many studies have indicated that a mismatching relationship exists between the methane adsorption capacity and SSA of coal and shale; that is, shale has a larger SSA but lower adsorption capacity (Figure ). This illogical mismatching relationship is due to the SSA in those references only tested by LP‐N 2 GA experiments, which cannot represent the true SSAs of the coal and shale samples. Figure illustrates this illogical mismatching relationship, which indicates that shales have a relatively large BET SSA but a much smaller adsorption capacity.…”
Section: Discussionmentioning
confidence: 99%
“…A mismatching relationship between the BET SSAs and methane adsorption capacities of coal and shale. Some data are cited from published articles…”
Section: Discussionmentioning
confidence: 99%
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“…Such isotherm indicates the nonporous or macroporous nature of the studied TGSH [73]. This isotherm also indicated that mono-layer/multi-layer adsorption for nitrogen molecules occurred; the point of inflection from mono-(0 < P/P o < 0.6) to multi-layer (P/P o > 0.6) adsorption appeared at P/P o about 0.6 [63]. Also the overlapping of the two isotherm branches (adsorption/desorption) at P/P o < 0.6 reflects the poor connectivity between the semiclosed pores of the TGSH, while the separation between those branches at relatively higher pressure (P/P o > 0.6) indicates the presence of opened large pores in association with the semi-closed ones [50].…”
Section: Characterization Of Talc-graphite Schistmentioning
confidence: 62%