Contact fracture behavior of ice

The formation of an intermediate layer under hydrostatic compression at a shear appearing due to the action of converging and diverging fronts of stress momentums (pulses) is considered. Continuous monitoring of deformational changes in the structure of ice was carried out using acoustic methods. Th...

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Bibliographic Details
Main Author: V. P. Epifanov
Format: Article
Language:Russian
Published: Nauka 2020-05-01
Series:Лëд и снег
Subjects:
Online Access:https://ice-snow.igras.ru/jour/article/view/806
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