Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling

Hydrate dissociation equilibrium conditions for the mixture of carbon dioxide (CO2), nitrogen (N2), and water (H2O) are measured in the temperature range of 274.15–280.15 K. The relative molar composition of carbon dioxide in the feed gas mixture varies between 0.05 and 0.25 which is the interesting...

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Published in:Fuel
Main Authors: Jarrahian, Azad, Nakhaee, Ali
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2019
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/44926/
https://oceanrep.geomar.de/id/eprint/44926/1/Jarrahian.pdf
https://doi.org/10.1016/j.fuel.2018.10.017
id ftoceanrep:oai:oceanrep.geomar.de:44926
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spelling ftoceanrep:oai:oceanrep.geomar.de:44926 2023-05-15T17:12:02+02:00 Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling Jarrahian, Azad Nakhaee, Ali 2019 text https://oceanrep.geomar.de/id/eprint/44926/ https://oceanrep.geomar.de/id/eprint/44926/1/Jarrahian.pdf https://doi.org/10.1016/j.fuel.2018.10.017 en eng Elsevier https://oceanrep.geomar.de/id/eprint/44926/1/Jarrahian.pdf Jarrahian, A. and Nakhaee, A. (2019) Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling. Fuel, 237 . pp. 769-774. DOI 10.1016/j.fuel.2018.10.017 <https://doi.org/10.1016/j.fuel.2018.10.017>. doi:10.1016/j.fuel.2018.10.017 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2019 ftoceanrep https://doi.org/10.1016/j.fuel.2018.10.017 2023-04-07T15:42:30Z Hydrate dissociation equilibrium conditions for the mixture of carbon dioxide (CO2), nitrogen (N2), and water (H2O) are measured in the temperature range of 274.15–280.15 K. The relative molar composition of carbon dioxide in the feed gas mixture varies between 0.05 and 0.25 which is the interesting range of composition when it comes to production of methane, and sequestration of carbon dioxide, from methane hydrate reservoirs. A thermodynamic model is presented based on the classical van der Waals and Platteeuw (vdW-P) solid solution theory for the hydrate phase combined with the Equation of State (EoS) for combustion gas and combustion gas-like mixtures (CG-EoS). The results of this model are compared to the dissociation data measured here, along with all available data from the experimental literature. The predicted results from two thermodynamic software programs, CSMGem, and Multiflash (which use Peng-Robinson (PR) and Cubic Plus Association (CPA) EoSs respectively), are also statistically evaluated. A Clausius-Clapeyron type equation was used to derive the enthalpy of dissociation at 279.15 K, and the values were found to converge for mixtures containing 0.1–0.25 mol fraction of carbon dioxide. Article in Journal/Newspaper Methane hydrate OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Fuel 237 769 774
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description Hydrate dissociation equilibrium conditions for the mixture of carbon dioxide (CO2), nitrogen (N2), and water (H2O) are measured in the temperature range of 274.15–280.15 K. The relative molar composition of carbon dioxide in the feed gas mixture varies between 0.05 and 0.25 which is the interesting range of composition when it comes to production of methane, and sequestration of carbon dioxide, from methane hydrate reservoirs. A thermodynamic model is presented based on the classical van der Waals and Platteeuw (vdW-P) solid solution theory for the hydrate phase combined with the Equation of State (EoS) for combustion gas and combustion gas-like mixtures (CG-EoS). The results of this model are compared to the dissociation data measured here, along with all available data from the experimental literature. The predicted results from two thermodynamic software programs, CSMGem, and Multiflash (which use Peng-Robinson (PR) and Cubic Plus Association (CPA) EoSs respectively), are also statistically evaluated. A Clausius-Clapeyron type equation was used to derive the enthalpy of dissociation at 279.15 K, and the values were found to converge for mixtures containing 0.1–0.25 mol fraction of carbon dioxide.
format Article in Journal/Newspaper
author Jarrahian, Azad
Nakhaee, Ali
spellingShingle Jarrahian, Azad
Nakhaee, Ali
Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling
author_facet Jarrahian, Azad
Nakhaee, Ali
author_sort Jarrahian, Azad
title Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling
title_short Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling
title_full Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling
title_fullStr Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling
title_full_unstemmed Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling
title_sort hydrate–liquid–vapor equilibrium condition of n2 + co2 + h2o system: measurement and modeling
publisher Elsevier
publishDate 2019
url https://oceanrep.geomar.de/id/eprint/44926/
https://oceanrep.geomar.de/id/eprint/44926/1/Jarrahian.pdf
https://doi.org/10.1016/j.fuel.2018.10.017
genre Methane hydrate
genre_facet Methane hydrate
op_relation https://oceanrep.geomar.de/id/eprint/44926/1/Jarrahian.pdf
Jarrahian, A. and Nakhaee, A. (2019) Hydrate–liquid–vapor equilibrium condition of N2 + CO2 + H2O system: Measurement and modeling. Fuel, 237 . pp. 769-774. DOI 10.1016/j.fuel.2018.10.017 <https://doi.org/10.1016/j.fuel.2018.10.017>.
doi:10.1016/j.fuel.2018.10.017
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1016/j.fuel.2018.10.017
container_title Fuel
container_volume 237
container_start_page 769
op_container_end_page 774
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