In
this study, we investigated guest behaviors of CO2 and
CH4 molecules during the initial formation of hydroquinone
(HQ) clathrates and then the swapping reactions of guest-loaded HQ.
Two experimental pressures of 3.0 and 5.0 MPa were selected for both
formation and swapping reactions at room temperature, both of which
are known to be in the stability region of HQ clathrates. Prepared
samples were analyzed by a series of spectroscopic measurements to
obtain qualitative and quantitative information on guest molecules
in clathrate cages. After the initial formation, CO2 molecules
showed higher cage occupancies of 90.1 ± 3.9 and 99.4 ±
2.7%, with full conversion into the clathrate form, compared to the
values of 61.9 ± 4.2 and 64.6 ± 4.5% with incomplete conversion
for CH4 molecules at 3.0 and 5.0 MPa, respectively. In
the subsequent swapping reactions, 72–77% of CH4 molecules in guest-loaded HQ clathrate are replaced with CO2, while only 6–9% of CO2 molecules are replaced
with CH4 molecules. The experimental results demonstrated
that kinetic behaviors of CO2 molecules are better favored
than CH4 molecules in HQ clathrates, even though their
thermodynamic equilibria are almost identical.