Molecular Dynamics Simulation of the Three-Phase Equilibrium Line of CO 2 Hydrate with OPC Water Model

The three-phase coexistence line of the CO2 hydrate was determined using molecular dynamics (MD) simulations. By using the classical and modified Lorentz-Berthelot (LB) parameters, the simulations were carried out at 10 different pressures from 3 to 500 MPa. For the OPC water model, simulations with...

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Published in:ACS Omega
Main Authors: Hao, Xiluo, Li, Chengfeng, Meng, Qingguo, Sun, Jianye, Huang, Li, Bu, Qingtao, Li, Congying
Format: Report
Language:English
Published: AMER CHEMICAL SOC 2023
Subjects:
Online Access:http://ir.qdio.ac.cn/handle/337002/181546
http://ir.qdio.ac.cn/handle/337002/181547
https://doi.org/10.1021/acsomega.3c05673
id ftchinacasciocas:oai:ir.qdio.ac.cn:337002/181547
record_format openpolar
spelling ftchinacasciocas:oai:ir.qdio.ac.cn:337002/181547 2024-05-12T08:07:01+00:00 Molecular Dynamics Simulation of the Three-Phase Equilibrium Line of CO 2 Hydrate with OPC Water Model Hao, Xiluo Li, Chengfeng Meng, Qingguo Sun, Jianye Huang, Li Bu, Qingtao Li, Congying 2023-10-10 http://ir.qdio.ac.cn/handle/337002/181546 http://ir.qdio.ac.cn/handle/337002/181547 https://doi.org/10.1021/acsomega.3c05673 英语 eng AMER CHEMICAL SOC ACS OMEGA http://ir.qdio.ac.cn/handle/337002/181546 http://ir.qdio.ac.cn/handle/337002/181547 doi:10.1021/acsomega.3c05673 Chemistry Multidisciplinary METHANE HYDRATE CARBON-DIOXIDE PHASE-EQUILIBRIUM GAS HYDRATE NUCLEATION GROWTH ETHYLENE 期刊论文 2023 ftchinacasciocas https://doi.org/10.1021/acsomega.3c05673 2024-04-14T23:52:16Z The three-phase coexistence line of the CO2 hydrate was determined using molecular dynamics (MD) simulations. By using the classical and modified Lorentz-Berthelot (LB) parameters, the simulations were carried out at 10 different pressures from 3 to 500 MPa. For the OPC water model, simulations with the classic and the modified LB parameters both showed negative deviations from the experimental values. For the TIP4P/Ice water model, good agreement with experimental equilibrium data can be achieved when the LB parameter is adjusted based on the solubility of CO2 in water. Our results also show that the influence of the water model on the equilibrium prediction is much larger than the CO2 model. Current simulations indicated that the H2O-H2O and H2O-CO2 cross-interactions' parameters might contribute equally to the accurate prediction of T-3. According to our simulations, the prediction of T-3 values showed relatively higher accuracy while using the combination of TIP4P/Ice water and EPM2 CO2 with modified LB parameter. Furthermore, varied chi values are recommended for accurate T-3 estimation over a wide pressure range. The knowledge obtained in this study will be helpful for further accurate MD simulation of the process of CO2/CH4 replacement. Report Methane hydrate Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Berthelot ENVELOPE(-64.146,-64.146,-65.333,-65.333) ACS Omega 8 42 39847 39854
institution Open Polar
collection Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR
op_collection_id ftchinacasciocas
language English
topic Chemistry
Multidisciplinary
METHANE HYDRATE
CARBON-DIOXIDE
PHASE-EQUILIBRIUM
GAS HYDRATE
NUCLEATION
GROWTH
ETHYLENE
spellingShingle Chemistry
Multidisciplinary
METHANE HYDRATE
CARBON-DIOXIDE
PHASE-EQUILIBRIUM
GAS HYDRATE
NUCLEATION
GROWTH
ETHYLENE
Hao, Xiluo
Li, Chengfeng
Meng, Qingguo
Sun, Jianye
Huang, Li
Bu, Qingtao
Li, Congying
Molecular Dynamics Simulation of the Three-Phase Equilibrium Line of CO 2 Hydrate with OPC Water Model
topic_facet Chemistry
Multidisciplinary
METHANE HYDRATE
CARBON-DIOXIDE
PHASE-EQUILIBRIUM
GAS HYDRATE
NUCLEATION
GROWTH
ETHYLENE
description The three-phase coexistence line of the CO2 hydrate was determined using molecular dynamics (MD) simulations. By using the classical and modified Lorentz-Berthelot (LB) parameters, the simulations were carried out at 10 different pressures from 3 to 500 MPa. For the OPC water model, simulations with the classic and the modified LB parameters both showed negative deviations from the experimental values. For the TIP4P/Ice water model, good agreement with experimental equilibrium data can be achieved when the LB parameter is adjusted based on the solubility of CO2 in water. Our results also show that the influence of the water model on the equilibrium prediction is much larger than the CO2 model. Current simulations indicated that the H2O-H2O and H2O-CO2 cross-interactions' parameters might contribute equally to the accurate prediction of T-3. According to our simulations, the prediction of T-3 values showed relatively higher accuracy while using the combination of TIP4P/Ice water and EPM2 CO2 with modified LB parameter. Furthermore, varied chi values are recommended for accurate T-3 estimation over a wide pressure range. The knowledge obtained in this study will be helpful for further accurate MD simulation of the process of CO2/CH4 replacement.
format Report
author Hao, Xiluo
Li, Chengfeng
Meng, Qingguo
Sun, Jianye
Huang, Li
Bu, Qingtao
Li, Congying
author_facet Hao, Xiluo
Li, Chengfeng
Meng, Qingguo
Sun, Jianye
Huang, Li
Bu, Qingtao
Li, Congying
author_sort Hao, Xiluo
title Molecular Dynamics Simulation of the Three-Phase Equilibrium Line of CO 2 Hydrate with OPC Water Model
title_short Molecular Dynamics Simulation of the Three-Phase Equilibrium Line of CO 2 Hydrate with OPC Water Model
title_full Molecular Dynamics Simulation of the Three-Phase Equilibrium Line of CO 2 Hydrate with OPC Water Model
title_fullStr Molecular Dynamics Simulation of the Three-Phase Equilibrium Line of CO 2 Hydrate with OPC Water Model
title_full_unstemmed Molecular Dynamics Simulation of the Three-Phase Equilibrium Line of CO 2 Hydrate with OPC Water Model
title_sort molecular dynamics simulation of the three-phase equilibrium line of co 2 hydrate with opc water model
publisher AMER CHEMICAL SOC
publishDate 2023
url http://ir.qdio.ac.cn/handle/337002/181546
http://ir.qdio.ac.cn/handle/337002/181547
https://doi.org/10.1021/acsomega.3c05673
long_lat ENVELOPE(-64.146,-64.146,-65.333,-65.333)
geographic Berthelot
geographic_facet Berthelot
genre Methane hydrate
genre_facet Methane hydrate
op_relation ACS OMEGA
http://ir.qdio.ac.cn/handle/337002/181546
http://ir.qdio.ac.cn/handle/337002/181547
doi:10.1021/acsomega.3c05673
op_doi https://doi.org/10.1021/acsomega.3c05673
container_title ACS Omega
container_volume 8
container_issue 42
container_start_page 39847
op_container_end_page 39854
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