Abstract

Due to differences in geological origin and pore and fissure structure, the effects of carbon dioxide (CO 2 ) displacement of methane (CH 4 ) in coal with different metamorphic degrees differ. The CO 2 -enhanced coalbed methane (ECBM) process involves the transformation of adsorbed CH 4 into free state CH 4 under CO 2 /CH 4 competitive adsorption. However, traditional experiments cannot be used to simultaneously analyse the content of the free and adsorbed states of CH 4 . Therefore, a low-field nuclear magnetic resonance (LF-NMR) technique was used to conduct CO 2 replacement of CH 4 in Anthracite (WYM), non-caking coals (BNM) and coking coals (JM) and to establish a quantitative model of CO 2 replacement of adsorbed CH 4 . Additionally, the adsorption efficiency and desorption capacity were calculated while discussing the mechanism of displacement desorption affected by pore and fissure structures. The results showed that WYM were mainly slit holes, BNM were mainly ink-bottle holes and JM were mainly cylindrical holes and slit holes. The micropore specific surface area and pore volume of WYM are the largest. After CO 2 injection, the P1 peak of T2 spectrum decreased significantly, while the P2 and P3 peaks increased, indicating that CO 2 injection effectively promoted the desorption of CH 4 .The NMR conversion coefficients of adsorbed CH 4 for the three coal samples were determined. WYM had the largest initial adsorption capacity of CH 4 (0.0156 mol) and total desorption capacity of CO 2 replacement of CH 4 (0.046 mol), and JM had the largest displacement desorption efficiency (78.885%), indicating that JM favours gas injection to increase CBM production and that WYM and BNM benefit the long-term storage of CO 2 .

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