Tuning Behaviors of Methane Inclusion in Isoxazole Clathrate Hydrates

Abstract

In this study, the inclusion of methane (CH<sub>4</sub>) gas in isoxazole (C<sub>3</sub>H<sub>3</sub>NO) clathrate hydrates was investigated through spectroscopic observations, such as powder X-ray diffraction (PXRD) and Raman spectroscopy. PXRD patterns of isoxazole clathrate hydrates having two different mole fractions of water were analyzed, and Raman spectroscopy was used to understand the CH<sub>4</sub> inclusion behaviors in the hydrate cavities. Raman spectra indicated that CH<sub>4</sub> can be captured in both small and large cavities of structure II hydrate in the C<sub>3</sub>H<sub>3</sub>NO with 34H<sub>2</sub>O system, while CH<sub>4</sub> can be entrapped in only small cavities of structure II hydrate in the C<sub>3</sub>H<sub>3</sub>NO with 17H<sub>2</sub>O system. The PXRD result showed both clathrate hydrate samples exhibit the same cubic <i>Fd3m</i> structure II hydrate as expected. However, the structure II hydrate in the C<sub>3</sub>H<sub>3</sub>NO with 34H<sub>2</sub>O system includes a small amount of hexagonal ice and structure I CH<sub>4</sub> hydrate. The phase equilibrium conditions of the binary (isoxazole + CH<sub>4</sub>) clathrate hydrate were also identified through high-pressure micro differential scanning calorimetry (MicroDSC), and the equilibrium temperatures of the binary (isoxazole + CH<sub>4</sub>) clathrate hydrate at given pressures are higher than those of the structure I CH<sub>4</sub> hydrate

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