Pore is the main adsorption and desorption space of coalbed methane (CBM). Pore size configuration and connectivity affect the adsorption/desorption hysteresis effect. Using tectonically deformed coal (TDC) and original structure coal of medium- and high-rank coal as the research objects, through the N2/CO2 adsorption experiment to analyze the pore size distribution and connectivity of different scales. We investigate the control mechanism of heterogeneous evolution in the key pore scales against adsorption/desorption hysteresis characteristics during coal metamorphism and deformation by combining the CH4 isothermal adsorption/desorption experiment under 30°C equilibrium moisture. The findings indicate that the super micropores (<2 nm) are mainly combination ink bottle-shaped pores and have worse connectivity as the degree of metamorphism and deformation increases. The super micropores occupy the vast majority of pore volume and specific surface area; its pore size distribution curve change presents an “M” bimodal type and is mainly concentrated in two pore segments of 0.45–0.70 nm and 0.70–0.90 nm. The effect of ductile deformation exerts a significantly greater effect on super micropores than brittle deformation. The exhibited adsorption–desorption characteristics are the result of the combined effect of the unique pore structure of the TDCs and different moisture contents. The presence of a large number of super micropores is the most important factor influencing the degree of gas desorption hysteresis. The “ink-bottle effect” is the primary cause of gas desorption hysteresis. For CBM development, some novel methods to increase desorption and diffusion rate at the super micropores scale should be considered.
To
understand and evaluate the CO2 injectivity in different
coal seams, low-, middle-, and high-rank coals from Shanxi Province
of China were collected to conduct CO2 adsorption/desorption,
induced swelling/shrinkage, and permeability experiments. Results
show that the adsorption/desorption amount, swelling/shrinkage deformation,
and permeability depend on the coal rank. The CO2 adsorption/desorption
amount of high-rank coal is the largest, followed by middle-rank coal,
and that of low-rank coal is the smallest. The swelling/shrinkage
strain and initial permeability of coals follow the sequence middle-rank
coal > low-rank coal > high-rank coal. The percentage reductions
of
permeability of low-rank coal, middle-rank coal, and high-rank coal
are 57.46, 48.50, and 71.17% when CO2 adsorption reaches
the equilibrium state, indicating that the permeability of high-rank
coal is more sensitive for the CO2 adsorption swelling.
The swelling and shrinkage deformation presents obvious three-dimensional
anisotropic characteristics; the deformation in the vertical bedding
plane direction (VBD) is the maximum, the second is that in the parallel
face cleat direction (PFD), and the deformation in the parallel butt
cleat direction (PBD) is the maximum. The developmental characteristics
of cleats and the distribution of macerals in coal contribute largely
to the anisotropic deformation of coal induced by CO2 adsorption–desorption.
The permeability of coal shows a U-shaped change trend of first decreasing
and then increasing after CO2 adsorption because the permeability
of coal is first dominated by the CO2 adsorption swelling
and then is dominated by the reduction of effective stress. The swelling
behavior and permeability attenuation of coal seams after CO2 injection are unavoidable; adopting the reservoir stimulation methods
to produce more complex fracture networks is the key to improving
CO2 injectivity. Combining the reservoir stimulation methods
with CO2-ECBM technology may be an important development
direction of the CCUS in coal seams.
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