We
obtain the activity coefficients and lower bounds to the solubility
of CaCl2 in aqueous solutions at temperatures between 298.15
and 473.15 K using molecular simulations with three previously developed
nonpolarizable force fields. We find that a scaled-charge force field
gives incorrect activity coefficients at low concentration and has
a different absolute chemical potential than experiments, but still
predicts an accurate solubility for the calcium chloride dihydrate.
The two full-charge models have chemical potentials and activity coefficients
closer to experiments, but there is considerable variation between
them, with the chemical potentials differing by over 100 kJ·mol−1. The slow dynamics of the full-charge models at high
concentrations are unrealistic and require advanced sampling methods
to obtain the activity coefficients. We find that development of polarizable
models is likely necessary to accurately represent both thermodynamic
and transport properties of divalent electrolyte solutions.
Phase equilibria of fluid substances
and their mixtures are important
in numerous scientific as well as industrial applications and are,
therefore, a major focus of thermophysical property research. For
the development and improvement of thermophysical property models,
reliable experimental data are crucial. However, measurements of thermophysical
properties in the vicinity of the dew line can be substantially distorted
by surface phenomena such as adsorption and capillary condensation
on the quasi nonporous metal surfaces of the experimental apparatuses.
To support the qualitative understanding of these phenomena on an
atomistic level and to estimate their impact on experiments, we performed
classical molecular dynamics (MD) simulations. As a first proof-of-concept
investigation, we focused on pure CO2 on an idealized face-centered
cubic (fcc) {111} gold surface. The results, in the form of an adsorption
isotherm at T = 283.15 K, are compared to sorption
measurements using a specially designed gold sinker incorporated in
an optimized gravimetric sorption analyzer. This first comparison
between atomistic MD simulations and gravimetric experiments helps
in assessing the applicability of our simulation technique and paves
the way for a deeper understanding of the relevant surface phenomena
occurring in our apparatus.
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