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‘Twinning’ and Fracture in Chromium

Abstract

Two types of brittle-to-ductile transition in tension have been found in chromium. In the annealed condition chromium is brittle at relatively elevated temperatures and low stresses in the strain-ageing region1,2, while in the warm-worked condition2 or after alloying, a transition occurs more typical of other body-centred cubic metals, at low temperature and high stresses3. Explanations of the high-temperature brittleness follow well-known models of dislocation locking4 or modifications involving fine precipitates2; however, these mechanisms do not wholly explain either the abrupt nature of the transition or the low stresses at which it occurs.

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References

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WEAVER, C. ‘Twinning’ and Fracture in Chromium. Nature 193, 265–266 (1962). https://doi.org/10.1038/193265a0

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