1991
DOI: 10.1016/0016-2361(91)90094-q
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Capillary-like condensation of sorbed gases in coals

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1992
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Cited by 9 publications
(3 citation statements)
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“…The shape of the adsorption isotherm changes from more Langmuir-like to more rectilinear as the rank of the coal decreases. Hysteresis is seen often between adsorption and desorption isotherms, and typically the hysteresis becomes larger as the coal rank decreases. Although hysteresis is generally associated with mesoporous adsorbents, at the low CO 2 pressures ( P / P s < 0.95) studied here, this origin of the hysteresis is unlikely . As noted in previous studies, coal swelling may be the origin of the hysteresis as well as the rectilinear shape of the adsorption isotherms.…”
Section: Resultssupporting
confidence: 48%
“…The shape of the adsorption isotherm changes from more Langmuir-like to more rectilinear as the rank of the coal decreases. Hysteresis is seen often between adsorption and desorption isotherms, and typically the hysteresis becomes larger as the coal rank decreases. Although hysteresis is generally associated with mesoporous adsorbents, at the low CO 2 pressures ( P / P s < 0.95) studied here, this origin of the hysteresis is unlikely . As noted in previous studies, coal swelling may be the origin of the hysteresis as well as the rectilinear shape of the adsorption isotherms.…”
Section: Resultssupporting
confidence: 48%
“…The adsorption isotherm analysis revealed a hysteresis loop within the range of 0.5<P/P 0 <0.99, indicating that the evaporation in the pore differs from the condensation within it, reflecting the capillary condensation phenomenon in the presence of mesopores [ 67 ]. The hysteresis type of coal samples, classified according to the ISO 9277:2022 recommendations by IUPAC [ 68 ], was identified as H3 type.…”
Section: Resultsmentioning
confidence: 99%
“…Larson and co-workers suggested that rearrangement will induce substantial increase in the self-diffusivity of CO 2 in the coal matrix, although it also appears that as the structure undergoes volumetric relaxation, the excess free volume associated with the glassy state is reduced, resulting in lower diffusion (Duda et al, 1994). The absorption of CO 2 allows the relaxation of the structure network and results in the weakening or softening of the internal structure of coal (Astakhov and Shirochin, 1991). This may contribute to local lithotype compression and compaction due to the heterogeneous and layered structure of most bituminous coal.…”
Section: Introductionmentioning
confidence: 96%