Previously undeformed columnar-grained ice exhibits a period of increasing or constant creep rate during the transient creep stage when loaded in simple compression perpendicular to the long axis of the columns. It is shown that this behavior is associated with the formation of small-angle boundaries and internal cracks. Creep strain beyond 0.25% for first load tends to a power-law dependence on time. On reload, specimens exhibit a normal transient creep behavior and have, initially, a lower resistance to deformation than for first load. With deformation, this resistance increases so that the reload creep curves cross the first load curves at about 0.2% creep. For reload, creep strain less than about 0.25% and greater than about 0.2% appear...
A power law relation between stress and strain rate of the form σ ∝ ε̇1/n was used to describe the r...
The stress-strain relationship to fracture for polycrystalline ice in tension has been shown to be g...
The deformation modes of polycrystalline ice are reviewed. Whereas single crystals of ice deform eas...
Previously undeformed columnar-grained ice exhibits a period of increasing or constant creep rate du...
An investigation was undertaken of the creep of columnar- grained ice under constant compressive str...
Observations are reported on the cracking activity during compressive creep of columnar-grained ice ...
Observations were made on the creep behavior of columnar ice beams of different thicknesses subjecte...
Information is presented on the stress, strain, temperature and time dependence of crack formation i...
Observations were made at one temperature on the cracks that form in ice during creep under constant...
The apparent activation energy for creep of columnar-grained ice subjected to a compressive stress o...
Ice loaded in compression deforms elastically and creeps, and if the loading is rapid or of long eno...
During the course of experiments on crack formation in ice subject to a constant compressive load, s...
Using columnar-grained ice specimens, a study was done of the reverse plastic deformation (strain re...
It has been shown that the development of grain-boundary and transgranular crack populations in tran...
During ice-structure interaction, ice will fail in a brittle manner dominated by two processes. The ...
A power law relation between stress and strain rate of the form σ ∝ ε̇1/n was used to describe the r...
The stress-strain relationship to fracture for polycrystalline ice in tension has been shown to be g...
The deformation modes of polycrystalline ice are reviewed. Whereas single crystals of ice deform eas...
Previously undeformed columnar-grained ice exhibits a period of increasing or constant creep rate du...
An investigation was undertaken of the creep of columnar- grained ice under constant compressive str...
Observations are reported on the cracking activity during compressive creep of columnar-grained ice ...
Observations were made on the creep behavior of columnar ice beams of different thicknesses subjecte...
Information is presented on the stress, strain, temperature and time dependence of crack formation i...
Observations were made at one temperature on the cracks that form in ice during creep under constant...
The apparent activation energy for creep of columnar-grained ice subjected to a compressive stress o...
Ice loaded in compression deforms elastically and creeps, and if the loading is rapid or of long eno...
During the course of experiments on crack formation in ice subject to a constant compressive load, s...
Using columnar-grained ice specimens, a study was done of the reverse plastic deformation (strain re...
It has been shown that the development of grain-boundary and transgranular crack populations in tran...
During ice-structure interaction, ice will fail in a brittle manner dominated by two processes. The ...
A power law relation between stress and strain rate of the form σ ∝ ε̇1/n was used to describe the r...
The stress-strain relationship to fracture for polycrystalline ice in tension has been shown to be g...
The deformation modes of polycrystalline ice are reviewed. Whereas single crystals of ice deform eas...