Combined mechanical and melting damage model for geomaterials

被引:6
|
作者
Liu, Jie [1 ]
Karrech, Ali [2 ]
Regenauer-Lieb, Klaus [1 ,3 ]
机构
[1] Univ Western Australia, Sch Earth & Environm, Lab Multiscale Earth Syst Dynam & Geothermal Res, Crawley, WA 6009, Australia
[2] Univ Western Australia, Sch Civil & Resource Engn, Crawley, WA 6009, Australia
[3] CSIRO Earth Sci & Resource Engn, Kensington, WA 6151, Australia
基金
澳大利亚研究理事会;
关键词
Plasticity; diffusion; and creep; Dynamics of lithosphere and mantle; Magma genesis and partial melting; DEFORMATION; PERIDOTITE; STATE; LITHOSPHERE; FRICTION; RHEOLOGY; BENEATH; GROWTH; ENERGY; CREEP;
D O I
10.1093/gji/ggu200
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present a new damage model combining mechanics and partial melting in accordance with the principles of non-equilibrium thermodynamics. On the mechanical side, elasto-viscoplactic damage is considered based on a self-consistent far from equilibrium thermodynamic framework; on the melt side, partial melting is calculated by using the thermodynamic MELTS Gibbs energy minimizer. In this framework, the partial melt appears as an additional damage parameter. The numerical implementations are accomplished by using Abaqus solver and the extendable User Material Subroutine. A simplified continental extension model is used to test the approach. This new model can be applied to geodynamic problems involving brittle and ductile faulting, partial melting, magma generation and the interaction between these activities.
引用
收藏
页码:1319 / 1328
页数:10
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