Abstract

• The effect of typical basal texture on the fracture behaviors and associated mechanisms of Ti under biaxial tension was for the first time elucidated by experiments and Finite Element modeling. • The presence of typical basal texture induced significant mechanical anisotropy in Ti, contributing to a two-stage fracture behavior consisting of a first normal fracture perpendicular to the rolling direction (RD) and a secondary shear fracture along the 45° direction relative to the RD. • An anisotropy parameter K , defined as the ratio of the equivalent effective traction stress to the yield strength, was proposed for the first time to predict the fracture path with the impact of crystallographic preferred orientation. The fracture behaviors and associated mechanisms of metallic materials under biaxial stress are vital for their manufacturability and service performance. In this work, the fracture behaviors of commercially pure titanium (CP-Ti) under quasi-uniaxial and equi-biaxial tension were investigated by using the digital image correlation technique and finite element modeling. The fracture behaviors under quasi-uniaxial tension were characterized by a general normal fracture. In contrast, normal fracture firstly occurred perpendicular to the rolling direction (RD) under equi-biaxial tension, followed by secondary shear fracture along the 45° direction relative to the RD. The normal fracture was attributed to the lower strain hardening ability in RD compared to the transverse direction (TD) induced by the TD-split type basal texture. The different hardening abilities introduced large shear stress in the 45° direction, which contributed significantly to the secondary shear fracture. An anisotropy parameter K ( Δ S s / σ s ), defined as the ratio of the equivalent effective traction stress to the yield strength, was proposed for the first time, to predict the fracture path with the impact of crystallographic preferred orientation.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.