Moving interfaces that separate loose and compact phases of elastic aggregates: a mechanism for drastic reduction or increase in macroscopic deformation

DOI10.1007/s00161-012-0260-yzbMath1343.74041OpenAlexW2144797689MaRDI QIDQ304142

David R. Owen, Luca Deseri

Publication date: 23 August 2016

Published in: Continuum Mechanics and Thermodynamics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1007/s00161-012-0260-y

zbMATH Keywords

granular materialsphase transitionselastic aggregatesstructured deformations

Mathematics Subject Classification ID

Dynamics of phase boundaries in solids (74N20) Granularity (74E20) Analysis of microstructure in solids (74N15)

Related Items (8)

Stable disarrangement phases arising from expansion/contraction or from simple shearing of a model granular medium ⋮ Submacroscopic disarrangements induce a unique, additive and universal decomposition of continuum fluxes ⋮ Second-order structured deformations: relaxation, integral representation and applications ⋮ The mechanically based non-local elasticity: an overview of main results and future challenges ⋮ Residual stresses in random elastic composites: nonlocal micromechanics-based models and first estimates of the representative volume element size ⋮ Elasticity with hierarchical disarrangements: a field theory that admits slips and separations at multiple submacroscopic levels ⋮ Elasticity with gradient-disarrangements: a multiscale perspective for strain-gradient theories of elasticity and of plasticity ⋮ Stable disarrangement phases of elastic aggregates: a setting for the emergence of no-tension materials with non-linear response in compression

Cites Work

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• Mathematical models of granular matter
• On the ubiquity of fracture in nonlinear elasticity
• Structured deformations of continua
• Toward a field theory for elastic bodies undergoing disarrangements
• Kinetic relations and the propagation of phase boundaries in solids
• Multiple shear band development and related instabilities in granular materials
• First normal stress difference and crystallization in a dense sheared granular fluid
• Submacroscopically Stable Equilibria of Elastic Bodies Undergoing Disarrangements and Dissipation

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