A comparative study of Maxwell viscoelasticity at large strains and rotations

Christoph E. Schrank*, Ali Karrech, David A. Boutelier, Klaus Regenauer-Lieb

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

3 Scopus citations

Abstract

We present a new Eulerian large-strain model for Maxwell viscoelasticity using a logarithmic co-rotational stress rate and the Hencky strain tensor. This model is compared to the smallstrain model without co-rotational terms and a formulation using the Jaumann stress rate. Homogeneous isothermal simple shear is examined for Weissenberg numbers in the interval [0.1; 10]. Significant differences in shear stress and energy evolution occur at Weissenberg numbers > 0.1 and shear strains > 0.5. In this parameter range, the Maxwell-Jaumann model dissipates elastic energy erroneously and thus should not be used. The small-strain model ignores finite transformations, frame indifference and self-consistency. As a result, it overestimates shear stresses compared to the new model and entails significant errors in the energy budget. Our large-strain model provides an energetically consistent approach to simulating non-coaxial viscoelastic deformation at large strains and rotations.

Original languageEnglish
Pages (from-to)252-262
Number of pages11
JournalGeophysical Journal International
Volume211
Issue number1
DOIs
StatePublished - Oct 2017
Externally publishedYes

Bibliographical note

Publisher Copyright:
© The Authors 2017.

Keywords

  • Creep and deformation
  • Fault zone rheology
  • Rheology and friction of fault zones
  • Rheology: crust and lithosphere

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology

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