Formation of inhomogeneous spatial structures in the boundary near-surface layer of ice
DOI (Low Temperature Physics):
https://doi.org/10.1063/10.0042360Ключові слова:
ice friction, phase transition, friction force, shear strain and stress, meltingАнотація
Запропоновано нелінійну модель граничного ковзання льоду для опису двох атомно-гладких поверхонь, розділених ультратонким попередньо розтопленим шаром льоду. Модель базується на системі рівнянь типу Лоренца, параметризованій зсувною деформацією, напруженням і температурою приповерхневого шару льоду. Враховано просторову неоднорідність цих параметрів і показано, що під час ковзання вздовж площини контакту формується доменна структура з двома типами доменів. Обчислено часову еволюцію фрактальних розмірностей цих розподілів доменів на площині контакту та продемонстровано існування характерного часу, коли фрактальні розмірності досягають мінімальних значень. Встановлено, що в процесі еволюції система наближається до однорідного стану, в якому на всій площі контакту реалізується фіксоване значення зсувної деформації, що визначає відносну швидкість ковзання тертьових блоків.
Посилання
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