Hydroquinone
(HQ) is known to form organic clathrates with some
gaseous species such as CO2 and CH4. This work
presents spectroscopic data, surface and internal morphologies, gas
storage capacities, guest release temperatures, and structural transition
temperatures for HQ clathrates obtained from pure CO2,
pure CH4, and an equimolar CO2/CH4 mixture. All analyses are performed on clathrates formed by direct
gas–solid reaction after 1 month’s reaction at ambient
temperature conditions and under a pressure of 3.0 MPa. A collection
of spectroscopic data (Raman, FT-IR, and 13C NMR) is presented,
and the results confirm total conversion of the native HQ (α-HQ)
into HQ clathrates (β-HQ) at the end of the reaction. Optical
microscopy and SEM analyses reveal morphology changes after the enclathration
reaction, such as the presence of surface asperities. Gas porosimetry
measurements show that HQ clathrates and native HQ are neither micro-
nor mesoporous materials. However, as highlighted by TEM analyses
and X-ray tomography, α- and β-HQ contain unsuspected
macroscopic voids and channels, which create a macroporosity inside
the crystals that decreases due to the enclathration reaction. TGA
and in situ Raman spectroscopy give the guest release temperatures
as well as the structural transition temperatures from β-HQ
to α-HQ. The gas storage capacity of the clathrates is also
quantified by means of different types of gravimetric analyses (mass
balance and TGA). After having been formed under pressure, the characterized
clathrates exhibit exceptional metastability: the gases remain in
the clathrate structure at ambient conditions over time scales of
more than 1 month. Consequently, HQ gas clathrates display very interesting
properties for gas storage and sequestration applications.