摘要

Hydrogen redistribution under stress-induced hydrogen diffusion and corresponding fracture behaviour of a 960 MPa grade martensitic steel were studied. Slow strain rate tensile (SSRT) tests after hydrogen pre-charging were performed and the fracture surface was observed and analysed. The strain rate ranged from 10(-6) to 10(-4) s(-1). In the pre-charged sample with a certain hydrogen content of 0.62 ppm, hydrogen distribution was homogeneous before the SSRT test. After tensile testing, brittle fracture features appeared in the centre of the fracture surface, while ductile features appeared in the surrounding area. Brittle region size increased with the strain rate slowing down in the range from 10(-4) to 5 x 10(-6) s(-1), while it stabilised at the strain rate slower than 5 x 10(-6) s(-1). Relationship between the strain rate and the brittle region size was established and discussed based on the present data of hydrogen content in the material.