On the bulk compaction of brittle granular materials, Part III: Brittle‐to‐ductile transition and yield strength ^*

Abstract A new and simple method is presented that enables the estimation of the yield strength ( σ y ) of brittle materials (e.g., ceramics, glasses). It results from the combination of sufficiently high‐stress compaction of their granular form, postmortem analysis of the crushed particles to identify the critical particle size corresponding to their brittle‐to‐ductile transition, and the use of a developed and simple analytical expression. This method was an outcome from Part I of this three‐paper series. To execute it, a granular brittle material is compacted to a sufficiently high stress, whereby the acting comminution produces both a fraction of particles having a sufficiently small size formed by ductile or plastic‐like deformation and a remaining fraction of larger particles formed from brittle fracture. Postmortem microscopy is then used to identify the smallest particle size whose morphology indicates it formed from brittle fracture ( d B2D ). The brittle material's σ y can then be estimated using a combination of the d B2D , Kendall's and Griffith's theories, a priori knowledge of the material's fracture toughness ( K Ic ), and a fracture mechanics shape factor constant ( Y ) using σ y = √((32 π K Ic 2 )/(3 Y 2 d B2D )). The method's development and its use to estimate σ y for several vitreous silicates, α‐quartzes, and NaCl are provided.