Continuum dynamics of the formation, migration and dissociation of self-locked dislocation structures on parallel slip planes

TL;DR

This paper develops a continuum model for dislocation dynamics on parallel slip planes, introducing new velocity fields and a flow stress formula that better captures dislocation pattern formation and correlations compared to traditional models.

Contribution

The paper presents a novel continuum dislocation dynamics model with two velocity fields and a new flow stress formula that incorporates short-range correlations and matches discrete simulations.

Findings

Flow stress increases with dislocation density up to a minimum distance

Flow stress transitions smoothly to zero for geometrically necessary dislocations

Inhomogeneity growth regime validated by discrete dislocation simulations

Abstract

In continuum models of dislocations, proper formulations of short-range elastic interactions of dislocations are crucial for capturing various types of dislocation patterns formed in crystalline materials. In this article, the continuum dynamics of straight dislocations distributed on two parallel slip planes is modelled through upscaling the underlying discrete dislocation dynamics. Two continuum velocity field quantities are introduced to facilitate the discrete-to-continuum transition. The first one is the local migration velocity of dislocation ensembles which is found fully independent of the short-range dislocation correlations. The second one is the decoupling velocity of dislocation pairs controlled by a threshold stress value, which is proposed to be the effective flow stress for single slip systems. Compared to the almost ubiquitously adopted Taylor relationship, the derived flow stress formula exhibits two features that are more consistent with the underlying discrete dislocation dynamics: i) the flow stress increases with the in-plane component of the dislocation density only up to a certain value, hence the derived formula admits a minimum inter-dislocation distance within slip planes; ii) the flow stress smoothly transits to zero when all dislocations become geometrically necessary dislocations. A regime under which inhomogeneities in dislocation density grow is identified, and is further validated through comparison with discrete dislocation dynamical simulation results. Based on the findings in this article and in our previous works, a general strategy for incorporating short-range dislocation correlations in continuum models of dislocations is proposed.