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All-Atom Molecular Dynamics of Pure Water-Methane Gas Hydrate Systems under Pre-Nucleation Conditions: A Direct Comparison between Experiments and Simulations of Transport Properties for the Tip4p/Ice Water Model
被引:9
|作者:
Guerra, Andre
[1
]
Mathews, Samuel
[1
]
Maric, Milan
[1
]
Servio, Phillip
[1
]
Rey, Alejandro D.
[1
]
机构:
[1] McGill Univ, Dept Chem Engn, Montreal, PQ H3A 0G, Canada
来源:
基金:
加拿大自然科学与工程研究理事会;
芬兰科学院;
关键词:
water;
methane;
hydrates;
viscosity;
diffusivity;
molecular dynamics;
POLYVINYLPYRROLIDONE PVP CONCENTRATION;
HYDROPHILIC GRAPHENE NANOFLAKES;
SELF-DIFFUSION COEFFICIENT;
NATURAL-GAS;
CARBON-DIOXIDE;
IRREVERSIBLE-PROCESSES;
DISSOCIATION PROCESS;
POTENTIAL FUNCTIONS;
CRYSTAL-GROWTH;
FLUE-GAS;
D O I:
10.3390/molecules27155019
中图分类号:
Q5 [生物化学];
Q7 [分子生物学];
学科分类号:
071010 ;
081704 ;
摘要:
(1) Background: New technologies involving gas hydrates under pre-nucleation conditions such as gas separations and storage have become more prominent. This has necessitated the characterization and modeling of the transport properties of such systems. (2) Methodology: This work explored methane hydrate systems under pre-nucleation conditions. All-atom molecular dynamics simulations were used to quantify the performance of the TIP4P/2005 and TIP4P/Ice water models to predict the viscosity, diffusivity, and thermal conductivity using various formulations. (3) Results: Molecular simulation equilibrium was robustly demonstrated using various measures. The Green-Kubo estimation of viscosity outperformed other formulations when combined with TIP4P/Ice, and the same combination outperformed all TIP4P/2005 formulations. The Green-Kubo TIP4P/Ice estimation of viscosity overestimates (by 84% on average) the viscosity of methane hydrate systems under pre-nucleation conditions across all pressures considered (0-5 MPag). The presence of methane was found to increase the average number of hydrogen bonds over time (6.7-7.8%). TIP4P/Ice methane systems were also found to have 16-19% longer hydrogen bond lifetimes over pure water systems. (4) Conclusion: An inherent limitation in the current water force field for its application in the context of transport properties estimations for methane gas hydrate systems. A re-parametrization of the current force field is suggested as a starting point. Until then, this work may serve as a characterization of the deviance in viscosity prediction.
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