Oxygen-enriched
coal-combustion flue gas geologic sequestration
in unmineable coal seams is a promising option to mitigate gaseous
pollutant emissions and recover coalbed methane (CH4).
Water (H2O) always exists in practical coal seams and shows
significant impact on fluid adsorption, desorption, diffusion, and
flow behaviors. Thus, this study mainly addressed the influence of
H2O on nitrous oxide (N2O) adsorption and desorption,
a typical component that existed in oxygen-enriched coal-combustion
flue gas, on different rank coals. Results indicate that the N2O adsorption equilibrium and kinetic behaviors within moist
coals can be well-predicted using the Sips model and the simplified
bidisperse kinetic model, respectively. The H2O dramatically
hinders the adsorption and diffusion capability of N2O
within coals, which is attributed to the fact that H2O
molecules occupy pore channels, induce coal matrix swelling, and compete
with N2O molecules for the same adsorption sites, particularly
the oxygen-containing functional groups. The H2O impairs
the physisorption and chemisorption of N2O on coals. Furthermore,
the H2O enhances the chemical transformation among the
four main nitrogen-containing species within coals, that is, pyridine-N,
pyrrole/pyridone-N, quaternary-N, and oxide-N. Particularly, the abundant
−H groups of H2O molecules inhibit the decomposition
of pyrrole/pyridone-N and accelerate the transformation of pyridine-N,
while −OH groups of H2O molecules promote the formation
of oxide-N. To sum up, the practical N2O geologic sequestration
should focus on the effects of in-situ H2O within coal
reservoirs.