The influence of temperature, pressure, salinity and capillary force on the formation of methane hydrate

We present here a thermodynamic model for predicting multi-phase equilibrium of methane hydrate liquid and vapor phases under conditions of different temperature, pressure, salinity and pore sizes. The model is based on the 1959 van der Waals–Platteeuw model, angle-dependent ab initio intermolecular...

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Main Authors: Zhenhao Duan, Ding Li, Yali Chen, Rui Sun
Format: Article
Language:English
Published: Elsevier 2011-04-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987111000272
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spelling doaj-4a8a134545b1449a9620a543688c73492020-11-24T20:47:56ZengElsevierGeoscience Frontiers1674-98712011-04-012212513510.1016/j.gsf.2011.03.009The influence of temperature, pressure, salinity and capillary force on the formation of methane hydrateZhenhao Duan0Ding Li1Yali Chen2Rui Sun3Key Laboratory of the Earth’s Deep Interior, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaKey Laboratory of the Earth’s Deep Interior, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, ChinaSchool of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaNorthwest University, Xi’an 710069, ChinaWe present here a thermodynamic model for predicting multi-phase equilibrium of methane hydrate liquid and vapor phases under conditions of different temperature, pressure, salinity and pore sizes. The model is based on the 1959 van der Waals–Platteeuw model, angle-dependent ab initio intermolecular potentials, the DMW-92 equation of state and Pitzer theory. Comparison with all available experimental data shows that this model can accurately predict the effects of temperature, pressure, salinity and capillary radius on the formation and dissociation of methane hydrate. Online calculations of the p–T conditions for the formation of methane hydrate at given salinities and pore sizes of sediments are available on: www.geochem-model.org/models.htm.http://www.sciencedirect.com/science/article/pii/S1674987111000272Methane hydrateab initio potentialSalinityPorous sedimentForming conditionsPhase equilibria
collection DOAJ
language English
format Article
sources DOAJ
author Zhenhao Duan
Ding Li
Yali Chen
Rui Sun
spellingShingle Zhenhao Duan
Ding Li
Yali Chen
Rui Sun
The influence of temperature, pressure, salinity and capillary force on the formation of methane hydrate
Geoscience Frontiers
Methane hydrate
ab initio potential
Salinity
Porous sediment
Forming conditions
Phase equilibria
author_facet Zhenhao Duan
Ding Li
Yali Chen
Rui Sun
author_sort Zhenhao Duan
title The influence of temperature, pressure, salinity and capillary force on the formation of methane hydrate
title_short The influence of temperature, pressure, salinity and capillary force on the formation of methane hydrate
title_full The influence of temperature, pressure, salinity and capillary force on the formation of methane hydrate
title_fullStr The influence of temperature, pressure, salinity and capillary force on the formation of methane hydrate
title_full_unstemmed The influence of temperature, pressure, salinity and capillary force on the formation of methane hydrate
title_sort influence of temperature, pressure, salinity and capillary force on the formation of methane hydrate
publisher Elsevier
series Geoscience Frontiers
issn 1674-9871
publishDate 2011-04-01
description We present here a thermodynamic model for predicting multi-phase equilibrium of methane hydrate liquid and vapor phases under conditions of different temperature, pressure, salinity and pore sizes. The model is based on the 1959 van der Waals–Platteeuw model, angle-dependent ab initio intermolecular potentials, the DMW-92 equation of state and Pitzer theory. Comparison with all available experimental data shows that this model can accurately predict the effects of temperature, pressure, salinity and capillary radius on the formation and dissociation of methane hydrate. Online calculations of the p–T conditions for the formation of methane hydrate at given salinities and pore sizes of sediments are available on: www.geochem-model.org/models.htm.
topic Methane hydrate
ab initio potential
Salinity
Porous sediment
Forming conditions
Phase equilibria
url http://www.sciencedirect.com/science/article/pii/S1674987111000272
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