Dynamics of Phase Transitions in a Snow Mass Containing Water-Soluble Salt Particles
- Авторы: Zelenko V.L.1, Heifets L.I.1, Orlov Y.N.1, Voskresenskiy N.M.1
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Учреждения:
- Department of Chemistry, Moscow State University
- Выпуск: Том 92, № 7 (2018)
- Страницы: 1285-1292
- Раздел: Physical Chemistry of Solutions
- URL: https://bakhtiniada.ru/0036-0244/article/view/170049
- DOI: https://doi.org/10.1134/S0036024418070348
- ID: 170049
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Аннотация
A macrokinetic approach is used to describe the dynamics of phase transitions in a snow mass containing water-soluble salt particles. Equations are derived that describe the rate of salt granule dissolution and the change in the phase composition and temperature of a snow mass under the conditions of heat transfer with an isothermal surface. An experimental setup that models the change in the state of a snow mass placed on an isothermal surface is created to verify theoretical conclusions. Experimental observations of the change in temperature of the snow mass are compared to theoretical calculations. The mathematical model that is developed can be used to predict the state of a snow mass on roads treated with a deicing agent, or to analyze the state of snow masses containing water-soluble salt inclusions and resting on mountain slopes.
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Об авторах
V. Zelenko
Department of Chemistry, Moscow State University
Автор, ответственный за переписку.
Email: zel_07@mail.ru
Россия, Moscow, 119991
L. Heifets
Department of Chemistry, Moscow State University
Автор, ответственный за переписку.
Email: heifets@tech.chem.msu.ru
Россия, Moscow, 119991
Yu. Orlov
Department of Chemistry, Moscow State University
Автор, ответственный за переписку.
Email: orlov-100@yandex.ru
Россия, Moscow, 119991
N. Voskresenskiy
Department of Chemistry, Moscow State University
Автор, ответственный за переписку.
Email: voskr@tech.chem.msu.ru
Россия, Moscow, 119991
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