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Effects of compressibility and wetting on the liquid-vapor transition in a confined fluid
被引:5
作者:
Caupin, Frederic
[1
]
机构:
[1] Univ Lyon, Univ Claude Bernard Lyon 1, Inst Lumiere Matiere, CNRS, Villeurbanne 69622, France
关键词:
THERMODYNAMIC PROPERTIES;
WATER;
INCLUSIONS;
DENSITY;
PALEOTEMPERATURES;
HOMOGENIZATION;
TEMPERATURES;
EQUILIBRIA;
CAVITATION;
ANOMALIES;
D O I:
10.1063/5.0098969
中图分类号:
O64 [物理化学(理论化学)、化学物理学];
学科分类号:
070304 ;
081704 ;
摘要:
When a fluid is constrained to a fixed, finite volume, the conditions for liquid-vapor equilibrium are different from those for the infinite volume or constant pressure cases. There is even a range of densities for which no bubble can form, and the liquid at a pressure below the bulk saturated vapor pressure remains indefinitely stable. As the fluid density in mineral inclusions is often derived from the temperature of bubble disappearance, a correction for the finite volume effect is required. Previous works have explained these phenomena and proposed a numerical procedure to compute the correction for pure water in a container completely wet by the liquid phase. Here, we revisit these works and provide an analytic formulation valid for any fluid, including the case of partial wetting. We introduce the Berthelot-Laplace length lambda = 2 gamma kappa/3, which combines the liquid isothermal compressibility kappa and its surface tension gamma. The quantitative effects are fully captured by a single, nondimensional parameter: the ratio of lambda to the container size. Published under an exclusive license by AIP Publishing.
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页数:12
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