Дискретнi властивостi квазiрiдких плiвок води в областi передплавлення льоду. 1. Температурнi залежностi товщини наноплiвок води та в’язкопружних властивостей полiкристалiчного льоду

Peculiarities in the temperature dependences of the properties of quasiliquid water films on the surface of ice crystallites have been studied experimentally under ice premelting conditions. Viscoelastic properties of polycrystalline ice in the temperature interval from 60 to 20 oC have been analyze...

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Збережено в:
Бібліографічні деталі
Дата:2018
Автори: Kornienko, M. E., Sheiko, N. L., Kornienko, O. M., Nikolaienko, T. Yu.
Формат: Стаття
Мова:English
Ukrainian
Опубліковано: Publishing house "Academperiodika" 2018
Теми:
Онлайн доступ:https://ujp.bitp.kiev.ua/index.php/ujp/article/view/2018279
Теги: Додати тег
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Назва журналу:Ukrainian Journal of Physics

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Ukrainian Journal of Physics
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Резюме:Peculiarities in the temperature dependences of the properties of quasiliquid water films on the surface of ice crystallites have been studied experimentally under ice premelting conditions. Viscoelastic properties of polycrystalline ice in the temperature interval from 60 to 20 oC have been analyzed. Peculiarities in the temperature dependences of the water nanolayer thickness, L(T), and the imaginary part of the shear modulus (modulus of viscous losses), G2(T), are found. Quasiequidistant temperature variations of the viscous loss modulus are revealed for the first time. A comparison of the results obtained with literature data on the temperature dependences L(T), the density of water in nanolayers, and the ice surface roughness allowed us to associate the observed features with a discrete cluster structure of quasiliquid water nanofilms. Temperature intervals of the enhanced stability for a cluster structure of water nanofilms are revealed, which manifest themselves in the form of extrema in viscoelastic ice parameters in the premelting interval. The interrelation between the phenomena of ice premelting and temperature discretization at the melting in ice nanolayers is considered for the first time.