On the Disappearance of the Crystal—Liquid Phase Transition as the Number of Atoms in the System Decreases
- Authors: Magomedov M.N.1
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Affiliations:
- Institute of Geothermal Problems, Dagestan Scientific Center, Russian Academy of Sciences
- Issue: Vol 13, No 5 (2019)
- Pages: 880-888
- Section: Article
- URL: https://journals.rcsi.science/1027-4510/article/view/196459
- DOI: https://doi.org/10.1134/S1027451019050070
- ID: 196459
Cite item
Abstract
An expression for the Helmholtz free energy of a nanocrystal that contains vacancies in lattice and the delocalized (diffusional) atoms is obtained on the basis of the previously proposed three-phase model of a simple matter and the RP(vac)-model of a nanocrystal. A model of the Gibbs surface, on which a portion of cells are vacant and a part of atoms are in the delocalized state, is proposed. The fact that a proportion of delocalized atoms are delocalized in a “bulk” way and a proportion of them are delocalized in a “surface way” is taken into account. The equation of state is calculated for argon, whose atoms interact via the Mie–Lennard-Jones pairwise potential. Calculations for the macrosystem were show that, at average temperatures, the equation of state has two S loops on isotherms corresponding to the crystal—liquid (C—L) and liquid—gas (L—G) phase transitions (PTs). At high temperatures, the S loop of the L—G PT contracts to the critical point. At low temperatures, two S loops of the C—L and L—G PTs merge into one large S loop corresponding to the C—G PT. As the number of atoms (N) in the nanosystem decreases, the S loops of both phase transitions in the isotherm decrease, and the C—L S loop disappears at a certain value of the number of atoms (N0). It is shown that N0 increases as the temperature of the isotherm increases and the nanosystem shape deviates from the most energetically optimal one (it is cubic for the RP(vac)-model). The C—L PT disappears in a cluster consisting of N < N0 atoms. Such a cluster gradually transforms into the liquid phase in the case of an isothermal increase in the specific volume.
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About the authors
M. N. Magomedov
Institute of Geothermal Problems, Dagestan Scientific Center, Russian Academy of Sciences
Author for correspondence.
Email: mahmag4@mail.ru
Russian Federation, Makhachkala, 367030
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