Comparison of the compressibility coefficient versus temperature, pressure, chemical potential dependencies for water and argon based on the principle of corresponding states

The application of the entropy-driven and density-driven phase transitions for analysis of phase diagram of water and argon is discussed. The reduced coefficient of isothermal compressibility is evaluated as βr = –(dV/dP)T(Pc/Vc) (Pc and Vc are the values in the critical point). The data are present...

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Veröffentlicht in:Low temperature physics (Woodbury, N.Y.) N.Y.), 2024-12, Vol.50 (12), p.1189-1192
Hauptverfasser: Bulavin, L. A., Rudnikov, Ye. G., Lebovka, N. I.
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creator Bulavin, L. A.
Rudnikov, Ye. G.
Lebovka, N. I.
description The application of the entropy-driven and density-driven phase transitions for analysis of phase diagram of water and argon is discussed. The reduced coefficient of isothermal compressibility is evaluated as βr = –(dV/dP)T(Pc/Vc) (Pc and Vc are the values in the critical point). The data are presented as dependencies of βr on the reduced temperature T/Tc, pressure P/Pc, and chemical potential μ/μc. Consideration is based on the principle of corresponding states. For water, the regions with anomalous behavior associated with the entropy-driven liquid–hexagonal ice phase transition and minima observed at T = (315.3 ± 0.2) K, P = (8.30 ± 0.04) kPa, and μ = (1122 ± 5) kJ/kg. For water, the baric dependence βr(P/Pc) along the liquid–vapor equilibrium line forms a closed loop with line of the liquid–hexagonal ice equilibrium. The thermodynamic similarity of water and argon is observed at relatively large temperatures T/Tc > 0.56, pressures P/Pc > 0.00358, and chemical potentials μ/μc > 0.505.
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For water, the baric dependence βr(P/Pc) along the liquid–vapor equilibrium line forms a closed loop with line of the liquid–hexagonal ice equilibrium. 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Consideration is based on the principle of corresponding states. For water, the regions with anomalous behavior associated with the entropy-driven liquid–hexagonal ice phase transition and minima observed at T = (315.3 ± 0.2) K, P = (8.30 ± 0.04) kPa, and μ = (1122 ± 5) kJ/kg. For water, the baric dependence βr(P/Pc) along the liquid–vapor equilibrium line forms a closed loop with line of the liquid–hexagonal ice equilibrium. The thermodynamic similarity of water and argon is observed at relatively large temperatures T/Tc &gt; 0.56, pressures P/Pc &gt; 0.00358, and chemical potentials μ/μc &gt; 0.505.</abstract><cop>Melville</cop><pub>American Institute of Physics</pub><doi>10.1063/10.0034414</doi><tpages>4</tpages><orcidid>https://orcid.org/0000-0002-8314-0601</orcidid><orcidid>https://orcid.org/0000-0002-8063-6441</orcidid><orcidid>https://orcid.org/0000-0002-6328-1650</orcidid></addata></record>
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subjects Argon
Chemical potential
Closed loops
Corresponding states
Critical point
Entropy
Liquid-vapor equilibrium
Phase diagrams
Phase transitions
Water compressibility
title Comparison of the compressibility coefficient versus temperature, pressure, chemical potential dependencies for water and argon based on the principle of corresponding states
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