Coal Geology & Exploration
Abstract
Objective and Method Adsorbed phase density represents a key parameter for determining gas adsorption capacity in coals. Using bituminous coal samples from the Huainan and Huaibei mining areas in Anhui Province, this study carried out high-pressure isothermal adsorption experiments of CO2 and CH4 at temperatures of 24 ℃, 36 ℃, and 48 ℃. In combination with the quantitative characterization of pore structures in coals using low-temperature liquid nitrogen adsorption (LNA) experiments and mercury intrusion porosimetry (MIP), this study analyzed the high-pressure trans-critical CH4 and CO2 adsorption processes in coals. Meanwhile, based on the Gibbs excess adsorption, the adsorbed phase volumes and maximum adsorbed phase densities of CO2 and CH4 in coals were calculated using the intercept method. Furthermore, by integrating the Langmuir model based on the monolayer adsorption theory and the modified Dubinin-Astakhov (D-A) model based on the adsorption potential theory, this study established a model of high-pressure trans-critical CH4 and CO2 adsorption in coals. Results and Conclusions Under the experimental conditions of 24 ℃‒48 ℃ and 0‒32 MPa, the excess adsorption capacities of CH4 and CO2 showed gradually declining trends after peaking due to an increase in the product of their free phase density (ρf) and adsorbed phase volumes (Va) in the high-pressure range. Specifically, the free phase density of CH4 increased linearly with adsorption pressure, resulting in a linear decrease in the excess adsorption capacity in the high-pressure range. In contrast, the free phase density for CO2 increased linearly in the low-pressure range (0‒7 MPa) but exhibited an S-shaped trend in the high-pressure range (> 7 MPa), leading to more complex variations in the excess adsorption capacity. Given the linearly decreasing trend in the excess adsorption capacity of CH4 in the high-pressure range, the adsorbed phase volume and maximum adsorbed phase density of CH4 were calculated using the intercept method. Then, an expression of the adsorbed phase density was derived using the modified D-A model. As a result, a model of the absolute adsorption capacity of CH4 under high pressures was established. By substituting the maximum adsorbed phase density of CO2, used as a substitute for the hypothetical saturated vapor pressure, into the above model, an improved model was developed to fit the adsorbed phase density and absolute adsorption capacity of CO2 in the high-pressure trans-critical adsorption processes. The improved model yielded coefficients of determination (R2) greater than 0.98 for the fitting of the absolute adsorption capacities of CH4 and CO2. However, large deviations were observed during the fitting of CO2 adsorption in the low-pressure range. To address this, the Langmuir model was introduced to describe the adsorption process in the low-pressure range. The resulting combined model further enhanced the fitting accuracy of the absolute adsorption capacities of CH4 and CO2 across the entire pressure range (R2 > 0.99). The results of this study provide a theoretical basis and optimized method for exploring the high-pressure trans-critical adsorption processes of gases in coals and for assessing the CO2 sequestration capacity in deep coal seams.
Keywords
high-pressure isothermal adsorption, adsorbed phase density, absolute adsorption capacity, adsorption model
DOI
10.12363/issn.1001-1986.25.03.0204
Recommended Citation
SONG Xuemei, ZHANG Kun, SANG Shuxun,
et al.
(2026)
"An improved model of trans-critical CH4 and CO2 adsorption in coals based on monolayer adsorption and adsorption potential theories,"
Coal Geology & Exploration: Vol. 54:
Iss.
1, Article 9.
DOI: 10.12363/issn.1001-1986.25.03.0204
Available at:
https://cge.researchcommons.org/journal/vol54/iss1/9
Reference
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