A thermodynamically self-consistent damage equation for grain size evolution during dynamic recrystallization

Details A thermodynamically self-consistent damage equation for grain size evolution during dynamic recrystallization A thermodynamically self-consistent damage equation for grain size evolution during dynamic recrystallization

Feb 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011geoji.184..719r&link_type=abstract

Geophysical Journal International, Volume 184, Issue 2, pp. 719-728.

Physics

2

Plasticity, Diffusion And Creep, Creep And Deformation, Fault Zone Rheology, Dynamics Of Lithosphere And Mantle, High Strain Deformation Zones, Rheology, Crust And Lithosphere

Scientific paper

We employ basic non-equilibrium thermodynamics to propose a general equation for the mean grain size evolution in a deforming medium, under the assumption that the whole grain size distribution remains self-similar. We show that the grain size reduction is controlled by the rate of mechanical dissipation in agreement with recent findings. Our formalism is self consistent with mass and energy conservation laws and allows a mixed rheology. As an example, we consider the case where the grain size distribution is lognormal, as is often experimentally observed. This distribution can be used to compute both the kinetics of diffusion between grains and of dynamic recrystallization. The experimentally deduced kinetics of grain size coarsening indicates that large grains grow faster than what is assumed in classical normal grain growth theory. We discuss the implications of this model for a mineral that can be deformed under both dislocation creep and grain size sensitive diffusion creep using experimental data of olivine. Our predictions of the piezometric equilibrium in the dislocation-creep regime are in very good agreement with the observations for this major mantle-forming mineral. We show that grain size reduction occurs even when the average grain size is in diffusion creep, because the largest grains of the grain size distribution can still undergo recrystallization. The resulting rheology that we predict for olivine is time-dependent and more non-linear than in dislocation creep. As the deformation rate remains an increasing function of the deviatoric stress, this rheology is not localizing.

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