Derivation of $\mathbf{F}=\mathbf{F}^e\mathbf{F}^p$ as the continuum limit of crystalline slip
Celia Reina, Anja Schl\"omerkemper, Sergio Conti

TL;DR
This paper rigorously proves that the classical multiplicative decomposition of deformation gradient into elastic and plastic parts emerges as a continuum limit from a detailed mesoscopic model of dislocations in 2D crystals.
Contribution
It provides a mathematical proof that the standard continuum kinematic relation in crystal plasticity arises from mesoscopic dislocation models via homogenization.
Findings
The classical multiplicative decomposition is recovered in the continuum limit.
The dislocation density tensor is identified as the curl of the plastic deformation gradient.
The proof applies to large deformations of 2D single crystals.
Abstract
In this paper we provide a proof of the multiplicative kinematic description of crystal elastoplasticity in the setting of large deformations, i.e. , for a two dimensional single crystal. The proof starts by considering a general configuration at the mesoscopic scale, where the dislocations are discrete line defects (points in the two-dimensional description used here) and the displacement field can be considered continuous everywhere in the domain except at the slip surfaces, over which there is a displacement jump. At such scale, as previously shown by two of the authors, there exists unique physically-based definitions of the total deformation tensor and the elastic and plastic tensors and that do not require the consideration of any non-realizable intermediate configuration and do not assume any a priori…
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