Hydrogen embrittlement (HE) in advanced high-strength steels (AHSS) arises from the interaction of absorbed hydrogen with microstructural features, leading to premature cracking and failure under stress. The main mechanisms include:
Hydrogen Enhanced Localized Plasticity (HELP): Hydrogen increases dislocation mobility, leading to highly localized plastic deformation and micro-crack initiation.
Hydrogen Enhanced Decohesion (HEDE): Hydrogen weakens atomic bonds at grain boundaries, interfaces, or inclusions, reducing cohesive strength and promoting intergranular fracture.
Hydrogen-Vacancy Interactions: Hydrogen stabilizes vacancies and defect clusters, causing void nucleation and microstructural instability.
Hydride Formation (less common in steels, but possible in certain alloys): Localized precipitation of brittle hydride phases can act as crack initiation sites.
Trapping and Diffusion Effects: Microstructural features such as martensite-austenite (M-A) constituents, grain boundaries, and dislocations act as hydrogen traps, influencing its mobility and concentration at critical stress regions.
In AHSS, the complex multiphase microstructure (martensite, retained austenite, ferrite, bainite) amplifies these effects, as hydrogen tends to concentrate in high-stress zones, accelerating crack growth and reducing ductility.