Abstract
To investigate the impact of moisture in various states on the adsorption of CH(4), N(2), and CO(2) by coal, this study conducted isothermal adsorption experiments on dry coal for moisture and on coal with varying moisture content for CH(4), N(2), and CO(2). The results revealed that coal moisture adsorption progresses through four stages: monolayer adsorption, multilayer adsorption, cluster formation, and condensation into free moisture filling pores. The presence of moisture in coal varies across these stages, with its impact on CH(4), N(2), and CO(2) adsorption decreasing as moisture content increases. As the moisture content rises, the adsorption constants (a and b values) progressively decline and eventually level off. Based on differences in coal moisture states, delineated by a relative humidity of 0.50 (corresponding to a moisture content of 2.39% in experimental samples), adsorption potential theory identified low moisture content stages where the monolayer and multilayer adsorption potentials for moisture (E(1) = 4.99 kJ/mol, E(2) = 39.71 kJ/mol) exceeded those for CH(4), N(2), and CO(2), suggesting competitive adsorption effects. In the high-water content stage, the mesoporous structural fractal dimension D(2) of the coal samples was found to be 2.77, nearly reaching 3, as determined through liquid nitrogen adsorption experiments and fractal dimension theory. This suggests that the intricate pore structure leads to water condensation, free water formation, and pore blockage, making it the primary factor influencing the adsorption of CH(4), N(2), and CO(2) in coals, which is inherently linked to the characteristics of coal.