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Thermodynamic fluid equations-of-state

dc.contributor.authorWoodcock, Leslie
dc.date.accessioned2018-12-07T14:53:05Z
dc.date.available2018-12-07T14:53:05Z
dc.date.issued2018-01
dc.description.abstractAs experimental measurements of thermodynamic properties have improved in accuracy, to five or six figures, over the decades, cubic equations that are widely used for modern thermodynamic fluid property data banks require ever-increasing numbers of terms with more fitted parameters. Functional forms with continuity for Gibbs density surface (p,T) which accommodate a critical-point singularity are fundamentally inappropriate in the vicinity of the critical temperature (T-c) and pressure (p(c)) and in the supercritical density mid-range between gas- and liquid-like states. A mesophase, confined within percolation transition loci that bound the gas- and liquid-state by third-order discontinuities in derivatives of the Gibbs energy, has been identified. There is no critical-point singularity at T-c on Gibbs density surface and no continuity of gas and liquid. When appropriate functional forms are used for each state separately, we find that the mesophase pressure functions are linear. The negative and positive deviations, for both gas and liquid states, on either side of the mesophase, are accurately represented by three or four-term virial expansions. All gaseous states require only known virial coefficients, and physical constants belonging to the fluid, i.e., Boyle temperature (T-B), critical temperature (T-c), critical pressure (p(c)) and coexisting densities of gas ((cG)) and liquid ((cL)) along the critical isotherm. A notable finding for simple fluids is that for all gaseous states below T-B, the contribution of the fourth virial term is negligible within experimental uncertainty. Use may be made of a symmetry between gas and liquid states in the state function rigidity (dp/d)(T) to specify lower-order liquid-state coefficients. Preliminary results for selected isotherms and isochores are presented for the exemplary fluids, CO2, argon, water and SF6, with focus on the supercritical mesophase and critical region.
dc.description.versioninfo:eu-repo/semantics/publishedVersion
dc.identifier.doi10.3390/e20010022
dc.identifier.issn1099-4300
dc.identifier.urihttp://hdl.handle.net/10400.1/11342
dc.language.isoeng
dc.peerreviewedyes
dc.publisherMDPI Ag
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.subjectGibbs density surface
dc.subjectCritical-point
dc.subjectTemperature relation
dc.subjectTriple-point
dc.subjectArgon
dc.subjectPressures
dc.subjectLiquid
dc.subjectGas
dc.subjectRegion
dc.subjectMpa
dc.titleThermodynamic fluid equations-of-state
dc.typejournal article
dspace.entity.typePublication
oaire.citation.issue1
oaire.citation.startPage22
oaire.citation.titleEntropy
oaire.citation.volume20
person.familyNameWoodcock
person.givenNameLeslie
person.identifier.orcid0000-0003-2350-559X
rcaap.rightsopenAccess
rcaap.typearticle
relation.isAuthorOfPublicationb550a18f-b4d3-4d68-8b8d-84f3373024aa
relation.isAuthorOfPublication.latestForDiscoveryb550a18f-b4d3-4d68-8b8d-84f3373024aa

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