Dynamic Mechanical Properties and Damage Evolution Behaviors of Ice-Rich Frozen Soil with Various Initial Moisture Contents
Publication: Journal of Cold Regions Engineering
Volume 38, Issue 4
Abstract
To investigate the dynamic mechanical response and damage evolution behavior of ice-rich frozen clay, split Hopkinson pressure bar (SHPB) tests were performed on frozen clay specimens with initial moisture contents of 20%–1,000% under different temperatures, strain rates, and stress states. The stress–strain curves, dynamic strength, peak strain, absorbed energy density, failure mode, and failure progress were studied. The experimental results revealed the following: (1) in the radial-free state, the stress–strain curve of frozen clay with initial moisture contents ranging from 20% to 85% and 1,000% could be divided into three stages: elasticity, plasticity, and failure. In addition, a double peak phenomenon occurs in the stress–strain curves within the initial moisture content range of 120%–480%. (2) In the radial-free state, as the initial moisture content increased, the dynamic strength first increased to a maximum value, then decreased to a minimum value less than the dynamic strength of ice, and eventually increased marginally to the dynamic strength of ice. However, the variation in dynamic peak strain with initial moisture content followed a decrease–increase–decrease three-stage pattern. (3) In the passive confining pressure state, the initial moisture content of frozen soil determined its sensitivity to the confining pressure. (4) The high-speed camera test results indicated that the failure of the ice-rich frozen clay was mainly caused by tensile cracks. The degree of failure of the frozen clay specimens became more evident as the moisture content and strain rate increased. In the passive confining pressure state, the ice-rich frozen clay specimens remained intact except for a small amount of edge peeling.
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Data Availability Statement
The data sets generated and analyzed in the current study are available from the corresponding author upon reasonable request.
Acknowledgments
This research was financially supported by the National Natural Science Foundation of China (Grant No. 42301152), the Opening Foundation of the State Key Laboratory of Frozen Soil Engineering (No. SKLFSE202004), and the Anhui Provincial New Era Education Quality Project Foundation (No. 2022xscx078).
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© 2024 American Society of Civil Engineers.
History
Received: Aug 30, 2023
Accepted: Mar 11, 2024
Published online: Jul 23, 2024
Published in print: Dec 1, 2024
Discussion open until: Dec 23, 2024
ASCE Technical Topics:
- Cold regions engineering
- Continuum mechanics
- Dynamics (solid mechanics)
- Engineering mechanics
- Freeze and thaw
- Frozen soils
- Geomechanics
- Geotechnical engineering
- Hydrologic engineering
- Hydrologic properties
- Hydrology
- Ice
- Material mechanics
- Materials engineering
- Pressure (type)
- Soil dynamics
- Soil mechanics
- Soil pressure
- Soil properties
- Soil stress
- Soil water
- Soils (by type)
- Solid mechanics
- Stress (by type)
- Structural analysis
- Structural engineering
- Water and water resources
- Water content
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