Abstract

Following on from two previous JETC (Joint European Thermodynamics Conference) presentations, we present a preliminary report of further advances towards the thermodynamic description of critical behavior and a supercritical gas-liquid coexistence with a supercritical fluid mesophase defined by percolation loci. The experimental data along supercritical constant temperature isotherms (T ≥ Tc) are consistent with the existence of a two-state mesophase, with constant change in pressure with density, rigidity, (dp/dρ) T, and linear thermodynamic state-functions of density. The supercritical mesophase is bounded by 3rd-order phase transitions at percolation thresholds. Here we present the evidence that these percolation transitions of both gaseous and liquid states along any isotherm are preceded by pre-percolation hetero-phase fluctuations that can explain the thermodynamic properties in the mesophase and its vicinity. Hetero-phase fluctuations give rise to one-component colloidal-dispersion states; a single Gibbs phase retaining 2 degrees of freedom in which both gas and liquid states with different densities percolate the phase volume. In order to describe the thermodynamic properties of two-state critical and supercritical coexistence, we introduce the concept of a hypothetical homo-phase of both gas and liquid, defined as extrapolated equilibrium states in the pre-percolation vicinity, with the hetero-phase fractions subtracted. We observe that there can be no difference in chemical potential between homo-phase liquid and gaseous states along the critical isotherm in mid-critical isochoric experiments when the meniscus disappears at T = Tc. For T > Tc, thermodynamic states comprise equal mole fractions of the homo-phase gas and liquid, both percolating the total phase volume, at the same temperature, pressure, and with a uniform chemical potential, stabilised by a positive finite interfacial surface tension.

Highlights

  • We present the evidence that these percolation transitions of both gaseous and liquid states along any isotherm are preceded by pre-percolation hetero-phase fluctuations that can explain the thermodynamic properties in the mesophase and its vicinity

  • We have known for several years, from computer experiments on model square-well molecular fluids [1], that at a critical temperature (Tc ) and pressure, two-phase gas–liquid coexistence becomes one supercritical mesophase with both gas and liquid states percolating the phase volume in a colloidal state of coexistence

  • At the gas bonded-cluster percolation transition PB, we can see that the equilibrium state in the mesophase after percolation is approximately an equimolar mixture of homophase gas and homophase liquid, each with the same chemical potential and each phase with the same mole fraction

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Summary

Introduction

We have known for several years, from computer experiments on model square-well molecular fluids [1], that at a critical temperature (Tc ) and pressure (pc ), two-phase gas–liquid coexistence becomes one supercritical mesophase with both gas and liquid states percolating the phase volume in a colloidal state of coexistence. For temperatures above critical coexistence, the rigidity has a constant value in the mesophase that separates the percolation loci which bound the limits of existence of liquid and gas states in the supercritical region. The motivation for the analysis reported here is to understand the observed experimental thermodynamic state functions at T ≥ Tc in terms of the colloidal properties of a mixture of both gaseous and liquid states arising from hetero-phase fluctuations on either side of the percolation transitions that define the mesophase region. We explain the various experimental observations of critical and supercritical fluids by heterophase fluctuations and consider the role of surface tension in this process of stabilisation of the colloidal two-state fluid phases

Hetero-Phase Fluctuations
Supercritical Percolation of Hetero-Phase Fluctuations
Evidence from Computer Experiments
Conclusions
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