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...
Published in: | Ice and Snow |
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Main Authors: | , |
Other Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | Russian |
Published: |
IGRAS
2020
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Subjects: | |
Online Access: | https://ice-snow.igras.ru/jour/article/view/806 https://doi.org/10.31857/S2076673420020040 |