Articles | Volume 18, issue 3
https://doi.org/10.5194/tc-18-1053-2024
© Author(s) 2024. 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-18-1053-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 Mar 2024
Research article |
| 05 Mar 2024
| 05 Mar 2024
Grain growth of ice doped with soluble impurities
Qinyu Wang
Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 101408, China
Sheng Fan
Department of Geology, University of Otago, Ōtepoti / Dunedin, Aotearoa / New Zealand
Department of Earth Sciences, University of Cambridge, Cambridge, UK
RSC, Te Whanganui-a-Tara / Wellington, Aotearoa / New Zealand
Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 101408, China
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Related subject area
Discipline: Ice sheets | Subject: Rheology
The role of grain size evolution in the rheology of ice: implications for reconciling laboratory creep data and the Glen flow law
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
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Grain size is a key microphysical property of ice, controlling the rheological behavior of ice sheets and glaciers. In this study, we develop a new model for grain size evolution in ice and show that it accurately predicts grain size in laboratory experiments and in natural ice core data. The model provides a physical explanation for the power-law relationship between stress and strain rate known as the Glen law and can be used as a predictive tool for modeling ice flow in natural systems.
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The Cryosphere, 14, 3875–3905, https://doi.org/10.5194/tc-14-3875-2020, https://doi.org/10.5194/tc-14-3875-2020, 2020
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We performed uniaxial compression experiments on synthetic ice samples. We report ice microstructural evolution at –20 and –30 °C that has never been reported before. Microstructural data show the opening angle of c-axis cones decreases with increasing strain or with decreasing temperature, suggesting a more active grain rotation. CPO intensity weakens with temperature because CPO of small grains is weaker, and it can be explained by grain boundary sliding or nucleation with random orientations.
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Short summary
We explored how the grain size of polycrystalline ice is affected by soluble impurities by conducting experiments on ice-containing salts. Results showed that above/below the eutectic point, impurities enhance/hinder grain growth, due to production of melts/precipitation of salt hydrates. Our findings offer insights into the dynamics of natural ice masses.
We explored how the grain size of polycrystalline ice is affected by soluble impurities by...
