This study focuses on improving fundamental understanding
of low,
subcritical CO2 adsorption–desorption behavior of
bituminous coals with the aim to evaluate the utility of shallow-depth
coal seams for safe and effective CO2 storage. Comprehensive
data and a detailed description of coal–CO2 interactions,
e.g., adsorption, desorption, and hysteresis behavior of intact bituminous
coals at CO2 pressures <0.5 MPa, are limited. Manometric
sorption experiments were performed on coal cores (50 mm dia. and
30- or 60-mm length) obtained from a 30 m deep coal seam located at
the Upper Silesian Basin in Poland. Experimental results revealed
that the adsorption capacities were correlated to void volume and
equilibrium time under low-pressure injection (0.5 MPa). The positive
deviation, observed in the hysteresis of adsorption–desorption
isotherm patterns, and the increased sample mass at the end of the
tests suggested CO2 pore diffusion and condensation. This
behavior is vital for assessing low-pressure CO2 injection
and storage capabilities of shallow coal seams where confining pressure
is much lower than that of the deeper seams. Overall, CO2 adsorption depicts a type II adsorption isotherm and a type H3 hysteresis
pattern of the IUPAC classification. Experimental results fitted better
to the Brunauer–Emmett–Teller model than the Langmuir
isotherm model. CO2 adsorption behavior of intact cores
was also evaluated by characteristic curves. It was found that Curve
I favored physical forces, i.e., the presence of van der Waals/London
dispersion forces to describe the coal–CO2 interactions.
However, analysis of Curve II indicated that the changing pressure-volume
behavior of CO2 in the adsorbed phase, under low equilibrium
pressures, cannot be ignored.