Regarding
CO2 geologic sequestration in the coal seam,
injected CO2 in the coal reservoir at an optimum depth
often presents as supercritical fluid (scCO2), which is
capable of changing the physicochemical properties of coal and further
affecting its CO2 storage capacity. Aiming to better explore
the aforementioned influences, we conducted a long-term scCO2–H2O–coal static interaction in the laboratory.
The influences of scCO2 exposure on the pore structure
characteristics, the main oxygenic functional groups, and the high-pressure
CO2 adsorption and desorption capabilities of four rank
coals were explored. The results show that long-term scCO2–H2O exposure has minor effects on the coal micropore
surface area and volume. On the contrary, it remarkably decreases
the mesopore of all of the coals. The alterations in the coal pore
structure parameters are mainly relevant to coal matrix swelling and
mineral dissolution due to long-term scCO2–H2O exposure. In general, long-term scCO2–H2O exposure increases the Neimark fractal dimension of coals,
further implying an elevated pore surface roughness and a more complex
pore structure. Moreover, the main oxygenic functional groups, including
C–O, CO, and −COOH, of coals after long-term
scCO2 exposure are reduced. The aforementioned changes
in the physicochemical properties of coals further affect their CO2 adsorption and desorption capabilities. In particular, the
maximum CO2 adsorption capacity of high-rank coals decreases
after exposure, whereas that of low-rank coals increases. Furthermore,
the CO2 adsorption and desorption hystereses of coals become
pronounced after long-term scCO2–H2O
exposure, implying more stable CO2 sequestration in the
coal seam. In conclusion, the implementation of CO2 sequestration
in the coal seam should focus on the long-term scCO2–H2O–coal interaction.