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Relative density and isobaric expansivity of cold and supercooled heavy water from 254 to 298 K and up to 100 MPa

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    SYSNO ASEP0509586
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleRelative density and isobaric expansivity of cold and supercooled heavy water from 254 to 298 K and up to 100 MPa
    Author(s) Blahut, Aleš (UT-L) RID, ORCID
    Hykl, Jiří (UT-L) RID, ORCID
    Peukert, Pavel (UT-L) RID
    Vinš, Václav (UT-L) RID, ORCID
    Hrubý, Jan (UT-L) RID, ORCID
    Number of authors7
    Article number034505
    Source TitleJournal of Chemical Physics. - : AIP Publishing - ISSN 0021-9606
    Roč. 151, č. 3 (2019)
    Number of pages18 s.
    Publication formPrint - P
    Languageeng - English
    CountryUS - United States
    Keywordsheavy water ; supercooling ; density measurement ; equation of state
    Subject RIVBJ - Thermodynamics
    OECD categoryThermodynamics
    R&D ProjectsGA16-02647S GA ČR - Czech Science Foundation (CSF)
    GA19-05696S GA ČR - Czech Science Foundation (CSF)
    Method of publishingLimited access
    Institutional supportUT-L - RVO:61388998
    UT WOS000476588700016
    EID SCOPUS85069463336
    DOI10.1063/1.5100604
    AnnotationA dual-capillary apparatus was developed for highly accurate measurements of density of liquids, including the supercooled liquid region. The device was used to determine the density of supercooled heavy water in the temperature range from 254 K to 298 K at pressures ranging from atmospheric to 100 MPa, relative to density at reference isotherm 298.15 K. The measurements of relative density were reproducible within 10 ppm, and their expanded (k = 2) uncertainty was within 50 ppm. To obtain absolute values of density, thermodynamic integration was performed using recent accurate speed of sound measurements in the stable liquid region. An empirical equation of state (EoS) was developed, giving specific volume as a rational function of pressure and temperature. The new experimental data are represented by EoS within their experimental uncertainty. Gibbs energy was obtained by EoS integration allowing computation of all thermodynamic properties of heavy
    water using Gibbs energy derivatives. Although based on data in relatively narrow temperature and pressure ranges, the developed EoS shows an excellent agreement with literature data for densities, isothermal compressibilities, and isobaric expansivities of deeply supercooled heavy water. The curvature of the thermodynamic surface steeply increases toward low temperatures and low pressures, thus supporting the existence of the hypothesized liquid-liquid coexistence boundary in a close vicinity of existing experimental data.
    WorkplaceInstitute of Thermomechanics
    ContactMarie Kajprová, kajprova@it.cas.cz, Tel.: 266 053 154 ; Jana Lahovská, jaja@it.cas.cz, Tel.: 266 053 823
    Year of Publishing2020
    Electronic addresshttps://aip.scitation.org/doi/10.1063/1.5100604
Number of the records: 1  

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