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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Format: | Article |
Language: | Russian |
Published: |
Nauka
2020-05-01
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Series: | Лëд и снег |
Subjects: | |
Online Access: | https://ice-snow.igras.ru/jour/article/view/806 |