How glass breaks -- Damage explains the difference between surface and fracture energies in amorphous silica
Gergely Molnár, Etienne Barthel
TL;DR
The paper addresses why fracture energy in amorphous silica exceeds the free surface energy by separating surface formation energy from a diffuse damage contribution that spans roughly $l\approx$16–23 Å. It combines atomistic simulations with a phase-field fracture model and calibrates a FEMU approach to quantify damage-driven energy dissipation, yielding a fracture toughness consistent with experiments (notably $2\gamma/g_c \approx 0.23$). The results reveal a nonlocal damage zone around cracks that dominates energy loss, while plasticity is negligible, bridging atomic-scale mechanisms with continuum fracture concepts. This work enhances understanding of brittle fracture in glasses and suggests broader applicability of phase-field damage descriptions to other brittle amorphous materials and possibly metallic glasses under fatigue or dynamic loading.
Abstract
The difference between free surface energy and fracture toughness in amorphous silica is studied via multi-scale simulations. We combine the homogenization of a molecular dynamics fracture model with a phase-field approach to track and quantify the various energy contributions. We clearly separate free surface energy localized as potential energy on the surface and damage diffusion over a 16-23 A range around the crack path. The plastic contribution is negligible. These findings, which clarify brittle fracture mechanisms in amorphous materials, align with toughness measurements in silica.
