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Liquid pre-freezing percolation transition to equilibrium crystal-in-liquid mesophase

dc.contributor.authorWoodcock, Leslie
dc.date.accessioned2021-02-04T14:43:36Z
dc.date.available2021-02-04T14:43:36Z
dc.date.issued2018
dc.description.abstractPre-freezing anomalies are explained by a percolation transition that delineates the existence of a pure equilibrium liquid state above the temperature of 1st-order freezing to the stable crystal phase. The precursor to percolation transitions are hetero-phase fluctuations that give rise to molecular clusters of an otherwise unstable state in the stable host phase. In-keeping with the Ostwald’s step rule, clusters of a crystalline state, closest in stability to the liquid, are the predominant structures in pre-freezing hetero-phase fluctuations. Evidence from changes in properties that depend upon density and energy fluctuations suggests embryonic nano-crystallites diverge in size and space at a percolation threshold, whence a colloidal-like equilibrium is stabilized by negative surface tension. Below this transition temperature, both crystal and liquid states percolate the phase volume in an equilibrium state of dispersed coexistence. We obtain a preliminary estimate of the prefreezing percolation line for water determined from higher-order discontinuities in Gibbs energy that derivatives the isothermal rigidity [(dp/dρ)T] and isochoric heat capacity [(dU/dT)v] respectively. The percolation temperature varies only slightly with pressure from 51.5°C at 0.1 MPa to around 60°C at 100 MPa. We conjecture that the predominant dispersed crystal structure is a tetrahedral ice, which is the closest of the higher-density ices (II to XV) to liquid water in configurational energy. Inspection of thermodynamic and transport properties of liquid argon also indicate the existence of a similar prefreezing percolation transition at ambient pressures (0.1 MPa) around 90 K, ~6% above the triple point (84 K). These findings account for many anomalous properties of equilibrium and supercooled liquids generally, and also explain Kauzmann’s “paradox” at a “glass” transition.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.4236/ns.2018.107026pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.1/15037
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/pt_PT
dc.subjectLiquid statept_PT
dc.subjectPercolationpt_PT
dc.subjectPhase transitionpt_PT
dc.subjectPre-freezing mesophasept_PT
dc.titleLiquid pre-freezing percolation transition to equilibrium crystal-in-liquid mesophasept_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage262pt_PT
oaire.citation.issue07pt_PT
oaire.citation.startPage247pt_PT
oaire.citation.titleNatural Sciencept_PT
oaire.citation.volume10pt_PT
person.familyNameWoodcock
person.givenNameLeslie
person.identifier.orcid0000-0003-2350-559X
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationb550a18f-b4d3-4d68-8b8d-84f3373024aa
relation.isAuthorOfPublication.latestForDiscoveryb550a18f-b4d3-4d68-8b8d-84f3373024aa

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