Abstract

Hydrogen embrittlement (HE) and hydrogen diffusion in medium‑carbon high-strength steel tempered at various temperatures were investigated by in situ slow strain rate testing and electrochemical hydrogen permeation, respectively. Synergistic correlations between the various microstructural components and reversible/irreversible hydrogen traps were established. Dislocations and the size, shape, distribution, and volume fraction of cementite were found to considerably influence the HE susceptibility. High dislocation density and interconnected needle-like cementite with a high aspect ratio, oriented along grain boundaries, were produced at a low tempering temperature (560 °C); this facilitated the decohesion of atoms at the cementite–matrix interface, enabling them to act as crack propagation sites and inducing brittle intergranular fracture. However, a significantly improved HE resistance associated with a quasi-cleavage-based fracture morphology was achieved at a high tempering temperature (680 °C) owing to the low dislocation density and the presence of uniformly distributed spheroidised cementite.

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