期刊
JOURNAL OF STRUCTURAL GEOLOGY
卷 115, 期 -, 页码 152-166出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.jsg.2018.07.014
关键词
Ice deformation; Glaciology; Ice microstructure; Grain boundary sliding; Crystallographic preferred orientations
资金
- Todd Foundation
- New Zealand Antarctic Research Institute
- Trans-Antarctic Association
- KOPRI project [PM18030 (20140409)]
- Marsden Fund of the Royal Society of New Zealand [UOO052]
- University of Otago Research Grant 2018
We deformed coarse-grained (similar to 10 mm) natural ice in axial compression at - 30 degrees C, to an axial strain of 0.2, at three different angles to the existing strong crystallographic preferred orientation (CPO). We used three strain rates for each sample orientation. Cryo-electron backscatter diffraction (EBSD) maps show that after deformation there is a mixture of large (similar to 1-2 mm) relict grains, and finer (100-200 mu m) recrystallised grains. The fine grains form a connected network in all samples. The large grains define a very strong CPO with equivalent but weaker CPOs in the recrystallised grains. The final CPO changed completely from its original orientation. Lattice distortion and subgrains equivalent in size to recrystallised grains suggest a subgrain rotation recrystallisation process has generated the recrystallised fraction. We suggest that strain rates were higher in the connected network of recrystallised grains because of a significant component of grain boundary sliding (GBS) that enables large grains to rotate by a combination of glide on the basal plane and rigid rotation, to define a very strong CPO. GBS weakens the CPO in the finer grained regions. The patterns of mechanical behaviour and the resultant microstructures do not bear an obvious relationship to original CPO.
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