Modeling oceanic sedimentary methane hydrate growth through molecular dynamics simulation

The crystallization process of methane hydrates in a confined geometry resembling seabed porous silica sedimentary conditions has been studied using molecular dynamics simulations. With this objective in mind, a fully atomistic quartz silica slit pore has been designed, and the temperature stability...

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Bibliographic Details
Published in:The Journal of Chemical Physics
Main Authors: Fernández-Fernández, Ángel M., Bárcena, Álvaro, Conde, María M., Pérez-Sánchez, Germán, Pérez-Rodríguez, Martín, Piñeiro, Manuel M.
Other Authors: Ministerio de Ciencia e Innovación, Ministerio de Universidades, Fundação para a Ciência e a Tecnologia
Format: Article in Journal/Newspaper
Language:English
Published: AIP Publishing 2024
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Online Access:http://dx.doi.org/10.1063/5.0203116
https://pubs.aip.org/aip/jcp/article-pdf/doi/10.1063/5.0203116/19873692/144107_1_5.0203116.pdf
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Summary:The crystallization process of methane hydrates in a confined geometry resembling seabed porous silica sedimentary conditions has been studied using molecular dynamics simulations. With this objective in mind, a fully atomistic quartz silica slit pore has been designed, and the temperature stability of a methane hydrate crystalline seed in the presence of water and guest molecule methane has been analyzed. NaCl ion pairs have been added in different concentrations, simulating salinity conditions up to values higher than average oceanic conditions. The structure obtained when the hydrate crystallizes inside the pore is discussed, paying special attention to the presence of ionic doping inside the hydrate and the subsequent induced structural distortion. The shift in the hydrate stability conditions due to the increasing water salinity is discussed and compared with the case of unconfined hydrate, concluding that the influence of the confinement geometry and pore hydrophilicity produces a larger deviation in the confined hydrate phase equilibria.