Articles | Volume 13, issue 1
https://doi.org/10.5194/tc-13-351-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-351-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
01 Feb 2019
Research article |
| 01 Feb 2019
| 01 Feb 2019
Crystallographic preferred orientations of ice deformed in direct-shear experiments at low temperatures
Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA, USA
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
David J. Prior
Department of Geology, University of Otago, Dunedin, New Zealand
Lisa Craw
Department of Geology, University of Otago, Dunedin, New Zealand
Sheng Fan
Department of Geology, University of Otago, Dunedin, New Zealand
Maria-Gema Llorens
Departament de Geologia, Universitat Autónoma de Barcelona,
Barcelona, Spain
Albert Griera
Departament de Geologia, Universitat Autónoma de Barcelona,
Barcelona, Spain
Marianne Negrini
Department of Geology, University of Otago, Dunedin, New Zealand
Paul D. Bons
Department of Geosciences, Eberhard Karls University of Tübingen, Tübingen, Germany
David L. Goldsby
Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA, USA
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43 citations as recorded by crossref.
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- Mechanical Properties of Freshwater Ice I. Baker & A. Ogunmolasuyi 10.1021/acs.jpcc.4c05171
- Linear-viscous flow of temperate ice C. Schohn et al. 10.1126/science.adp7708
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- The temperature change shortcut: effects of mid-experiment temperature changes on the deformation of polycrystalline ice L. Craw et al. 10.5194/tc-15-2235-2021
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- Microstructures and Fabric Transitions of Natural Ice from the Styx Glacier, Northern Victoria Land, Antarctica D. Kim et al. 10.3390/min10100892
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- Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations S. Kufner et al. 10.1029/2022JF006853
- Cool ice with hot properties S. Fan & D. Prior 10.1038/s41561-023-01330-z
- Inferring Ice Fabric From Birefringence Loss in Airborne Radargrams: Application to the Eastern Shear Margin of Thwaites Glacier, West Antarctica T. Young et al. 10.1029/2020JF006023
- Stress sensitivity of high-temperature microstructures in ice, with potential applications to quartz J. Platt et al. 10.1016/j.jsg.2021.104487
- Modeling the Deformation Regime of Thwaites Glacier, West Antarctica, Using a Simple Flow Relation for Ice Anisotropy (ESTAR) F. McCormack et al. 10.1029/2021JF006332
- Crystallographic preferred orientations of ice deformed in direct-shear experiments at low temperatures C. Qi et al. 10.5194/tc-13-351-2019
- Evolution of crystallographic preferred orientations of ice sheared to high strains by equal-channel angular pressing Q. Wang et al. 10.5194/tc-19-827-2025
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- Static Ice Pressure Measuring System Based on Fiber Loop Ring-Down Spectroscopy and FPGA X. Deng et al. 10.3390/s20205927
43 citations as recorded by crossref.
- Ultrasonic and seismic constraints on crystallographic preferred orientations of the Priestley Glacier shear margin, Antarctica F. Lutz et al. 10.5194/tc-16-3313-2022
- Full crystallographic orientation (c and a axes) of warm, coarse-grained ice in a shear-dominated setting: a case study, Storglaciären, Sweden M. Monz et al. 10.5194/tc-15-303-2021
- Microstructures in a shear margin: Jarvis Glacier, Alaska C. Gerbi et al. 10.1017/jog.2021.62
- On the Limitations of Using Polarimetric Radar Sounding to Infer the Crystal Orientation Fabric of Ice Masses N. Rathmann et al. 10.1029/2021GL096244
- Microstructure and Crystallographic Preferred Orientations of an Azimuthally Oriented Ice Core from a Lateral Shear Margin: Priestley Glacier, Antarctica R. Thomas et al. 10.3389/feart.2021.702213
- Simulating higher-order fabric structure in a coupled, anisotropic ice-flow model: application to Dome C D. Lilien et al. 10.1017/jog.2023.78
- Temperature and strain controls on ice deformation mechanisms: insights from the microstructures of samples deformed to progressively higher strains at −10, −20 and −30 °C S. Fan et al. 10.5194/tc-14-3875-2020
- Using grain boundary irregularity to quantify dynamic recrystallization in ice S. Fan et al. 10.1016/j.actamat.2021.116810
- Mechanical Properties of Freshwater Ice I. Baker & A. Ogunmolasuyi 10.1021/acs.jpcc.4c05171
- Linear-viscous flow of temperate ice C. Schohn et al. 10.1126/science.adp7708
- Macroscopic response and microstructure evolution in viscoplastic polycrystals with pressurized pores S. Das et al. 10.1007/s10704-020-00500-z
- A physically-based formulation for texture evolution during dynamic recrystallization. A case study of ice T. Chauve et al. 10.5802/crmeca.243
- Ice fabrics in two-dimensional flows: beyond pure and simple shear D. Richards et al. 10.5194/tc-16-4571-2022
- Microstructure-sensitive crystal plasticity and phase-field modeling of deformation and fracture in polycrystalline ice S. Motahari et al. 10.1016/j.actamat.2024.120512
- Multimaxima crystallographic fabrics (CPO) in warm, coarse-grained ice: New insights M. Disbrow-Monz et al. 10.1016/j.jsg.2024.105107
- Origin of englacial stratigraphy at three deep ice core sites of the Greenland Ice Sheet by synthetic radar modelling S. Mojtabavi et al. 10.1017/jog.2021.137
- Plastic Faulting in Ice N. Golding et al. 10.1029/2019JB018749
- Constraining Ice Shelf Anisotropy Using Shear Wave Splitting Measurements from Active‐Source Borehole Seismics F. Lutz et al. 10.1029/2020JF005707
- Radar Characterization of Ice Crystal Orientation Fabric and Anisotropic Viscosity Within an Antarctic Ice Stream T. Jordan et al. 10.1029/2022JF006673
- Recrystallization processes, microstructure and crystallographic preferred orientation evolution in polycrystalline ice during high-temperature simple shear B. Journaux et al. 10.5194/tc-13-1495-2019
- A stratigraphy-based method for reconstructing ice core orientation J. Westhoff et al. 10.1017/aog.2020.76
- Shear localisation in anisotropic, non-linear viscous materials that develop a CPO: A numerical study T. de Riese et al. 10.1016/j.jsg.2019.03.006
- Flow laws for ice constrained by 70 years of laboratory experiments S. Fan et al. 10.1038/s41561-025-01661-z
- The evolution of ice fabrics: A continuum modelling approach validated against laboratory experiments D. Richards et al. 10.1016/j.epsl.2020.116718
- The temperature change shortcut: effects of mid-experiment temperature changes on the deformation of polycrystalline ice L. Craw et al. 10.5194/tc-15-2235-2021
- Can changes in deformation regimes be inferred from crystallographic preferred orientations in polar ice? M. Llorens et al. 10.5194/tc-16-2009-2022
- Crystallographic preferred orientation (CPO) patterns in uniaxially compressed deuterated ice: quantitative analysis of historical data N. Hunter et al. 10.1017/jog.2022.95
- Microstructures and Fabric Transitions of Natural Ice from the Styx Glacier, Northern Victoria Land, Antarctica D. Kim et al. 10.3390/min10100892
- Tidal Modulation of a Lateral Shear Margin: Priestley Glacier, Antarctica H. Still et al. 10.3389/feart.2022.828313
- Does second phase content control the evolution of olivine CPO type and deformation mechanisms? A case study of paired harzburgite and dunite bands in the Red Hills Massif, Dun Mountain Ophiolite Y. Shao et al. 10.1016/j.lithos.2021.106532
- Bridging the Gap Between Experimental and Natural Fabrics: Modeling Ice Stream Fabric Evolution and its Comparison With Ice‐Core Data D. Richards et al. 10.1029/2023JB027245
- Spatial Variations of Fabric and Microstructure of Blue Ice Cores at the Shear Margin of Dalk Glacier, Antarctica S. Lu et al. 10.3390/w15040728
- Progresses in studies on crystallographic preferred orientations in experimentally deformed ice Q. WANG & C. QI 10.3724/j.issn.1007-2802.20240103
- Elastic wave propagation in anisotropic polycrystals: inferring physical properties of glacier ice N. Rathmann et al. 10.1098/rspa.2022.0574
- Strongly Depth‐Dependent Ice Fabric in a Fast‐Flowing Antarctic Ice Stream Revealed With Icequake Observations S. Kufner et al. 10.1029/2022JF006853
- Cool ice with hot properties S. Fan & D. Prior 10.1038/s41561-023-01330-z
- Inferring Ice Fabric From Birefringence Loss in Airborne Radargrams: Application to the Eastern Shear Margin of Thwaites Glacier, West Antarctica T. Young et al. 10.1029/2020JF006023
- Stress sensitivity of high-temperature microstructures in ice, with potential applications to quartz J. Platt et al. 10.1016/j.jsg.2021.104487
- Modeling the Deformation Regime of Thwaites Glacier, West Antarctica, Using a Simple Flow Relation for Ice Anisotropy (ESTAR) F. McCormack et al. 10.1029/2021JF006332
- Crystallographic preferred orientations of ice deformed in direct-shear experiments at low temperatures C. Qi et al. 10.5194/tc-13-351-2019
- Evolution of crystallographic preferred orientations of ice sheared to high strains by equal-channel angular pressing Q. Wang et al. 10.5194/tc-19-827-2025
- Thrust faulting in glaciers? Re‐examination of debris bands near the margin of Storglaciären, Sweden M. Monz et al. 10.1111/bor.12549
- Static Ice Pressure Measuring System Based on Fiber Loop Ring-Down Spectroscopy and FPGA X. Deng et al. 10.3390/s20205927
Latest update: 02 Apr 2025
Short summary
Ice deformed in nature develops crystallographic preferred orientations, CPOs, which induce an anisotropy in ice viscosity. Shear experiments of ice revealed a transition in CPO with changing temperature/strain, which is due to the change of dominant CPO-formation mechanism: strain-induced grain boundary migration dominates at higher temperatures and lower strains, while lattice rotation dominates at other conditions. Understanding these mechanisms aids the interpretation of CPOs in natural ice.
Ice deformed in nature develops crystallographic preferred orientations, CPOs, which induce an...
