Tetsu-to-Hagane
Online ISSN : 1883-2954
Print ISSN : 0021-1575
ISSN-L : 0021-1575
Regular Article
Hydrogen Embrittlement and Local Characterization at Crack Initiation Associated with Phase Transformation of High-strength Steel Containing Retained Austenite
Taku NagaseTakuya ItoYoshiro NishimuraHiroshi SuzukiKenichi Takai
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2016 Volume 102 Issue 9 Pages 534-543

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Abstract

States of hydrogen present in high-strength steels for use as bearing steel SUJ2 and hydrogen embrittlement susceptibility were examined using thermal desorption analysis (TDA) and tensile tests. SUJ2 specimens containing retained austenite phase (γR) in the martensite phase exhibited three hydrogen desorption peaks in the TDA profile. Two of the peaks desorbed at higher temperatures decreased with a decreasing amount of γR, indicating they corresponded to desorption associated with γR. Fracture strength in the presence of hydrogen increased with a decreasing amount of γR and with an increasing strain rate. When the specimens contained γR and hydrogen, a flat facet at the crack initiation site and a quasi-cleavage (QC) fracture in the initial crack propagation area were observed on the fracture surface. Local characterization using electron back-scattered diffraction (EBSD) revealed that the flat facet on the fracture surface corresponded not to γR but to stress-induced martensite. In addition, the facet was {112} plane of martensite, which is the slip plane or deformation twin plane of body-centered-cubic metals. The reason for high hydrogen embrittlement susceptibility of the specimens containing γR was attributed to the stress-induced phase transformation at the crack initiation site of the flat facet and in the initial crack propagation area of the QC fracture. Furthermore, the strain rate dependency of hydrogen embrittlement susceptibility is presumably ascribable to local plastic deformation, i.e., the interaction between dislocations and hydrogen.

Crack initiation and propagation areas of [SUJ2] specimen with hydrogen after tensile test at a strain rate of 2×10–6 s–1 at 30°C. (a) image of crack initiation on fracture surface observed by SEM. (b) IPF map of flat facet at crack initiation on fracture surface analyzed by EBSD. The flat facet is {112} plane of martensite which is slip plane in bcc lattice. (c) IPF map of cross section near flat facet at crack initiation analyzed by EBSD. The flat facet is {112} plane of martensite which is slip plane in bcc lattice. (d) Phase map of cross section near flat facet of crack initiation analyzed by EBSD. The phase of flat facet and near the area is not retained austenite but martensite. (Online version in color.) Fullsize Image
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© 2016 The Iron and Steel Institute of Japan

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