Ice dynamic recrystallization within Europa's ice shell: Implications for solid-state convection Article Swipe
Solid-state convection has been proposed to occur within Europa's ice shell based both on the interpretation of observed geological activity during Galileo spacecraft exploration and theoretical investigations. Laboratory experiments have investigated the effect of grain size insensitive creep and grain size sensitive creep on the ductile behaviour of polycrystalline ice. The ice grain size and the ice impurities content and, consequently, the viscosity of the ice within Europa's ice shell are poorly constrained, limiting the possibility to understand if solid-state convection can occur under Europa's ice shell conditions. To investigate how diurnal tidal flexing and the internal dynamics of Europa's ice shell influence the ice grain crystals' evolution, we adopted a thermal-mechanical numerical model that uses finite differences and marker-in-cell techniques, implementing the dynamic recrystallization of the ice and the ice grain evolution in a self-consistent way with the numerical model. We found that solid-state convection within Europa's ice shell can occur if it is diurnally tidally deformed, as the tidal stresses within the ice shell operate to reduce the ice grain sizes and the ice viscosity. We discuss future radio science experiments, in combination with radar sounder investigations, that will be capable of characterizing the possible presence of solid-state convection within Europa's ice shell.
Related Topics
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1016/j.icarus.2023.115648
- OA Status
- hybrid
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- 3
- References
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- OpenAlex ID
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Raw OpenAlex JSON
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https://openalex.org/W4378975853Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1016/j.icarus.2023.115648Digital Object Identifier
- Title
-
Ice dynamic recrystallization within Europa's ice shell: Implications for solid-state convectionWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2023Year of publication
- Publication date
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2023-06-01Full publication date if available
- Authors
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Giuseppe MitriList of authors in order
- Landing page
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https://doi.org/10.1016/j.icarus.2023.115648Publisher landing page
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YesWhether a free full text is available
- OA status
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hybridOpen access status per OpenAlex
- OA URL
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https://doi.org/10.1016/j.icarus.2023.115648Direct OA link when available
- Concepts
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Sea ice growth processes, Amorphous ice, Geology, Ice crystals, Recrystallization (geology), Convection, Geophysics, Mechanics, Sea ice, Materials science, Arctic ice pack, Sea ice thickness, Meteorology, Petrology, Climatology, Physics, Chemistry, Amorphous solid, Organic chemistryTop concepts (fields/topics) attached by OpenAlex
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3Total citation count in OpenAlex
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2025: 1, 2024: 2Per-year citation counts (last 5 years)
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68Number of works referenced by this work
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10Other works algorithmically related by OpenAlex
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