Residual stress analysis on materials with steep stress gradient by using X-ray incidence at higher angles
Ohya Shin-ichi; Yoshioka Yasuo; Maeno Shigeki
Abstract:X-ray stress measurements for isotropic polycrystalline are materials are usually carried out by the sin2y method under the assumption of no stress gradient in X-ray penetration depth. When a steep stress gradient exists in the vicinity of surface layer, however, non-linear sin2y relation is observed and the sin2y method cannot be applied on such cases. Although several X-ray stress analyzers have been developed for materials with steep stress gradient in the surface layer, it is desirable to use diffraction data at higher incident angles of f0 as possible as close on 90 degrees in order to determine the both values of surface stress and stress gradient with high accuracy.