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 language | English |
|---|---|
| Pages (from-to) | 252-262 |
| Number of pages | 11 |
| Journal | Geophysical Journal International |
| Volume | 211 |
| Issue number | 1 |
| DOIs | |
| State | Published - Oct 2017 |
| Externally published | Yes |
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