Creep and recrystallization of large polycrystalline masses. III. Continuum theory of ice sheets

DOI10.1098/rspa.2006.1698zbMath1149.74318OpenAlexW2030631572MaRDI QIDQ3502059

Sérgio H. Faria

Publication date: 22 May 2008

Published in: Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1098/rspa.2006.1698

zbMATH Keywords

thermodynamicsrecrystallizationmechanicsicepolygonizationcontinuous diversity

Mathematics Subject Classification ID

Crystalline structure (74E15) Glaciology (86A40)

Related Items (5)

A Critical Review of the Mechanics of Polycrystalline Polar Ice ⋮ Comment on the papers ‘Creep and recrystallization of large polycrystalline masses’ by Faria and co-authors ⋮ Thermodynamics of polycrystalline materials treated by the theory of mixtures with continuous diversity ⋮ Continuum-mechanical, anisotropic flow model for polar ice masses, based on an anisotropic flow enhancement factor ⋮ Reply to Gagliardini's comment on ‘Creep and recrystallization of large polycrystalline masses’ by Faria and co-authors

Cites Work

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• Viscous response of polar ice with evolving fabric
• Anisotropic, transversely isotropic nonlinear viscosity of rock ice and rheological parameters inferred from homogenization
• Creep and recrystallization of large polycrystalline masses. I. General continuum theory
• Creep and recrystallization of large polycrystalline masses. II. Constitutive theory for crystalline media with transversely isotropic grains
• A continuum–mechanical formulation for shallow polythermal ice sheets
• Strengthening and weakening of induced anisotropy in polar ice

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