Understanding the role of the co- and counter-diffusive properties of CO2 and CH4 in coal has important implications for enhanced coalbed methane recovery (ECBM) and CO2 sequestration in coals and for related issues of gas outbursts during mining. This study addresses how coal-gas interactions affect CO2 injectivity, in particular the roles of coal deformation, gas flow, CH4-CO2 counter-diffusion and gas absorption/desorption on the evolution of transport and mechanical properties of fractured coals, and therefore on ECBM recovery.
A fully coupled coal deformation, gas flow, CH4-CO2 counter-diffusion and gas absorption/desorption finite element (FE) model was developed to investigate the combined net effects on evolutions of CO2 injection related parameters. The FE model was successfully applied to match the experimental data; and a field scale model was constructed to quantify CO2 injection rate and other transport parameters for ECBM under in-situ conditions. Model results indicated that (1) Coal rank has a converse influence on the CO2 injection performance, lower coal rank reservoir could be more suitable to carry out CO2-ECBM technology; (2) Initial permeability has positive impact on the performance of CO2 replacing methane. This finding also has an important indication for the implementation of this technology in shale and other low permeability media; (3) CO2 injection is very sensitive to changes in the injection gas Langmuir strain constants, so trying to reduce the resultant strain constant, such as using mixed gases like N2 and CO2 or flue gas, is an efficient solution to improve the methane recovery efficiency.
Using carbon dioxide to displace CH4 in unmineable coalbeds has been paid more attention due to the global warming and the resource shortage. This technique has been proposed as one of the geologic strategies to mitigate increasing concentrations of CO2 in the atmosphere and it is particularly attractive in those cases where the coal medium contains large amounts of natural gas (CH4) [1-3].
Carbon dioxide is known to have a greater affinity to coal than methane. Early laboratory isotherm measurements for pure gases have demonstrated that coal can absorb approximately twice as much CO2 by volume as methane. Recent research on CO2 sorption capacity of different ranks of United States coal has shown that this ratio may be as high as 10:1 in some low rank coals [4]. This observation suggests that stronger affinity of CO2 to the coal material could initiate a mechanism of displacement of the originally in-place CH4, when CO2 is introduced to the coalbed environment. This is extremely important not only for sequestration but also for coalbed methane production. Since the concept of coal seam sequestration was first proposed by Macdonald of Alberta Energy during discussions with Gunter in 1997 [1], a number of field CO2-ECBM storage pilot projects have been carried out in North America, Europe (Poland), China, Japan. The Allison Unit pilot, which is located in the Northern New Mexico part of the San Juan Basin, represents the world’s first field trial of CO2-ECBM in 1996 [5-6].