Physical scaling laws in dislocation microstructures and avalanches from dislocation dynamics simulations
Missipsa Aissaoui, Charlie Kahloun, Oguz Umut Salman, Sylvain Queyreau
TL;DR
This work tackles the variability of avalanche statistics in crystal plasticity by performing large-scale 3D Dislocation Dynamics simulations of Cu across wide ranges of dislocation density and crystal orientation under a fixed strain rate. The study demonstrates a robust power-law regime with $α \approx -1.6$ to $-1.7$ that is invariant to density and loading direction, and identifies a density- and orientation-dependent upper cutoff for avalanche sizes, roughly obeying $\Delta \gamma_{max} \approx D_{hkl} - C_{hkl} b \sqrt{\rho_{obs}}$; it also shows that triggering stresses $τ_c$, when rescaled by the local obstacle density and averaged stress, collapse to a Frechet distribution, and that per-system avalanche dynamics exhibit clear correlations among slip systems. These findings reconcile disparate experimental and simulation reports by providing precise scaling laws linking mesoscopic dislocation interactions to macroscopic plasticity, enabling improved upscaling to mesoscale and continuum models. The results also emphasize that dislocation-density evolution modulates the statistics, underscoring the need for controlling strain rate and microstructure in predictive constitutive laws.
Abstract
Avalanche-like plastic bursts in crystalline materials follow power law statistics, but the scaling exponents and cutoff parameters vary widely in the literature ($α$ ranging from -1 to -2.2), hindering predictive modeling. Since distributions do not follow Gaussian behavior, the average of plastic kinetics is not correctly defined. Larger-scale models that rely on average behavior are therefore fundamentally flawed. We performed extensive 3D Dislocation Dynamics simulations of FCC Cu deformation across three orders of magnitude in dislocation density ($ρ= 5 \ 10^{10} \ \text{à} \ 2 \ 10^{12} \ \text{m}^{-2}$) under constant strain rates. Our results demonstrate that the power law exponent ($α\approx $ -1.6 to -1.7 ) is invariant to both dislocation density and loading direction, resolving previous inconsistencies. However, dislocation density strongly controls the power law truncation scaling ($Δγ_{max} \propto \ b/\sqrtρ$) and the distribution of avalanche triggering stresses. We quantify correlations between slip system activities and show how individual system contributions evolve with avalanche size. These findings reconcile experimental scatter in avalanche statistics and provide quantitative scaling laws for mesoscale-to-continuum plasticity models.
