Spectroscopic technique for the measurement of residual stress in sintered Al2O3

Abstract

Using the R‐line fluorescence of trace Cr³⁺ in sintered Al₂O₃ as an example, a method of analysis is outlined for determining the residual microstress and macrostress in a polycrystalline aggregate. It uses the shift and broadening, induced by residual stress, of a line due to a transition in an atomic system dissolved in the aggregate. For sintered Al₂O₃ from three different manufacturers, but made for the same purpose, the isotropic and shearing components of the residual microstress and macrostress are listed in tabular form. For the isotropic component of the microstress a distribution is found, with a mean value of ∼2 kbar, in which tension and compression are equally probable.