“…However, compared with other adsorbents, such as Maxsorb III, ACF, and MOFs [3], the diversity of the macerals, variations in mineral species, and an uneven distribution of pores and fractures in coal create inhomogeneous methane adsorption characteristics [4][5][6], rendering an evaluation of the storage characteristics difficult, and hindering the industrial exploitation of CBM reserves. Past studies have shown that the micro pores (<10 nm) in coal are the main sites of methane storage owing to their large surface area, and that the intercrystalline pores and intragranular corrosion pores of clay minerals also have a fair methane adsorption capacity [1,2,7]. Based on methane adsorption capacity tests of different microlithotypes, Chalmers [8] hypothesized that methane is held as a solution gas in liptinite-rich coals, and in micropores in liptinite-poor coals through physical sorption.…”