CO2 Hydrate Nucleation Kinetics Enhanced by an Organo-Mineral Complex Formed at the Montmorillonite Water Interface

• Published in: Environmental Science & Technology
• Main Authors: Kyung, DS Kyung, Daeseung, Lim, HK Lim, Hyung Kyu, Kim, HJ Kim, Hyung-Jun, Lee, WJ Lee, Woo-Jin
• Format: Article in Journal/Newspaper
• Language: English
• Published: AMER CHEMICAL SOC 2015
• Subjects: MOLECULAR-DYNAMICS SIMULATIONS; CARBON-DIOXIDE HYDRATE; METHANE HYDRATE; SEDIMENT SUSPENSIONS; NA-MONTMORILLONITE; DISSOLUTION RATES; PHASE-EQUILIBRIUM; AMINO-ACIDS; FORCE-FIELD; ADSORPTION; Methane hydrate
• Online Access: http://hdl.handle.net/10203/195531; https://doi.org/10.1021/es504450x

In this study, we investigated experimentally and computationally the effect of organo-mineral complexes on the nucleation kinetics of CO2 hydrate. These complexes formed via adsorption of zwitter-ionic glycine (Gly-zw) onto the surface of sodium montmorillonite (Na-MMT). The electrostatic attraction between the -NH3+ group of Gly-zw, and the negatively charged Na-MMT surface, provides the thermodynamic driving force for the organo-mineral complexation. We suggest that the complexation of Gly-zw on the Na-MMT surface accelerates CO2 hydrate nucleation kinetics by increasing the mineral-water interfacial area (thus increasing the number of effective hydrate-nucleation sites), and also by suppressing the thermal fluctuation of solvated Na+ (a well-known hydrate formation inhibitor) in the vicinity of the mineral surface by coordinating with the -COO- groups of Gly-zw. We further confirmed that the local density of hydrate-forming molecules (i.e., reactants of CO2 and water) at the mineral surface (regardless of the presence of Gly-zw) becomes greater than that of bulk phase. This is expected to promote the hydrate nucleation kinetics at the surface. Our study sheds new light on CO2 hydrate nucleation kinetics in heterogeneous marine environments, and could provide knowledge fundamental to successful CO2 sequestration under seabed sediments.