56 research outputs found

    Effects of compressibility and wetting on the liquid-vapor transition in a confined fluid

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    When a fluid is constrained to a fixed, finite volume, the conditions for liquid-vapor equilibrium are different from 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 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 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 and including the case of partial wetting. We introduce the Berthelot-Laplace length λ=2γκ/3\lambda=2\gamma\kappa/3, which combines the liquid isothermal compressibility κ\kappa and its surface tension γ\gamma. The quantitative effects are fully captured by a single, non-dimensional parameter: the ratio of λ\lambda to the container size.Comment: 13 pages, 13 figure

    Minimal microscopic model for liquid polyamorphism and water-like anomalies

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    Liquid polyamorphism is the intriguing possibility for a single component substance to exist in multiple liquid phases. We propose a minimal model for this phenomenon. Starting with a binary lattice model with critical azeotropy and liquid-liquid demixing, we allow interconversion of the two species, turning the system into a single-component fluid with two states differing in energy and entropy. Unveiling the phase diagram of the non-interconverting binary mixture gives unprecedented insight on the phase behaviors accessible to the interconverting fluid, such as a liquid-liquid transition with a critical point, or a singularity-free scenario, exhibiting thermodynamic anomalies without polyamorphism. The model provides a unified theoretical framework to describe supercooled water and a variety of polyamorphic liquids with water-like anomalies.Comment: 15 pages, 11 figure

    Fluid inclusions in minerals: from geosciences to the physics of water and back

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    Compressibility anomalies in stretched water and their interplay with density anomalies

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    Water keeps puzzling scientists because of its numerous properties which behave oppositely to usual liquids: for instance, water expands upon cooling, and liquid water is denser than ice. To explain this anomalous behaviour, several theories have been proposed, with different predictions for the properties of supercooled water (liquid at conditions where ice is more stable). However, discriminating between those theories with experiments has remained elusive because of spontaneous ice nucleation. Here we measure the sound velocity in liquid water stretched to negative pressure, and derive an experimental equation of state, which reveals compressibility anomalies. We show by rigorous thermodynamic relations how these anomalies are intricately linked with the density anomaly. Some features we observe are necessary conditions for the validity of two theories of water.Comment: 17 pages, 3 figures, 24 reference

    Viscosity and Stokes-Einstein relation in deeply supercooled water under pressure

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    We report measurements of the shear viscosity η\eta in water up to 150MPa150\,\mathrm{MPa} and down to 229.5K229.5\,\mathrm{K}. This corresponds to more than 30K30\,\mathrm{K} supercooling below the melting line. The temperature dependence is non-Arrhenius at all pressures, but its functional form at 0.1MPa0.1\,\mathrm{MPa} is qualitatively different from that at all pressures above 20MPa20\,\mathrm{MPa}. The pressure dependence is non-monotonic, with a pressure-induced decrease of viscosity by more than 50 % at low temperature. Combining our data with literature data on the self-diffusion coefficient DsD_\mathrm{s} of water, we check the Stokes-Einstein relation which, based on hydrodynamics, predicts constancy of Dsη/TD_\mathrm{s} \eta/T, where TT is the temperature. The observed temperature and pressure dependence of Dsη/TD_\mathrm{s} \eta/T is analogous to that obtained in simulations of a realistic water model. This analogy suggests that our data are compatible with the existence of a liquid-liquid critical point at positive pressure in water.Comment: 11 pages, 8 figures, 7 tables, 1 supplementary figure. Summary of main changes: the abstract and conclusion were modified, minor edits were made to all figures for clarity, one table and the supplementary figure were adde

    Cavitation in water: a review

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    Interfacial Properties of Fluids Exhibiting Liquid Polyamorphism and Water-Like Anomalies

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    It has been hypothesized that liquid polyamorphism, the existence of multiple amorphous states in a single component substance, may be caused by molecular or supramolecular interconversion. A simple microscopic model [Caupin and Anisimov, Phys. Rev. Lett., 127, 185701, (2021)] introduces interconversion in a compressible binary lattice to generate various thermodynamic scenarios for fluids that exhibit liquid polyamorphism and/or water-like anomalies. Using this model, we demonstrate the dramatic effects of interconversion on the interfacial properties. In particular, we find that the liquid-vapor surface tension exhibits either an inflection point or two extrema in its temperature dependence. Correspondingly, we observe anomalous behavior of the interfacial thickness and a significant shift in the location of the concentration profile with respect to the location of the density profile.Comment: This manuscript has been submitted to the Journal of Physical Chemistry B, as a part of the special issue, "Pablo G. Debenedetti Festschrift.
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