MOLECULAR DYNAMICS EQUATION OF STATE FOR NONPOLAR GEOCHEMICAL FLUIDS

dc.contributor.authorDuan Z.
dc.contributor.authorMoller N.
dc.contributor.authorWeare J.H.
dc.date.accessioned2020-11-26T08:26:23Z
dc.date.available2020-11-26T08:26:23Z
dc.date.issued1995
dc.description.abstractRemarkable agreement between molecular dynamics simulations and experimental measurements has been obtained for methane for a large range of intensive variables, including those corresponding to liquid/vapor coexistence. Using a simple Lennard-Jones potential the simulations not only predict thePVT properties up to 2000°C and 20,000 bar with errors less than 1.5%, but also reproduce phase equilibria well below 0°C with accuracy close to experiment. This two-parameter molecular dynamics equation of state (EOS) is accurate for a much larger range of temperatures and pressures than our previously published EOS with a total fifteen parameters or that of Angus et al. (1978) with thirty-three parameters. By simple scaling, it is possible to predict PVT and phase equilibria of other nonpolar and weakly polar species.
dc.identifierhttps://elibrary.ru/item.asp?id=661722
dc.identifier.citationGeochimica et Cosmochimica Acta, 1995, , 8, 1533-1538
dc.identifier.issn0016-7037
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/19642
dc.titleMOLECULAR DYNAMICS EQUATION OF STATE FOR NONPOLAR GEOCHEMICAL FLUIDS
dc.typeСтатья

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