Crystallographic Analysis of Lower Bainite Transformation in Fe-0.7%c Alloy

23Citations
Citations of this article
7Readers
Mendeley users who have this article in their library.

Abstract

Lower bainite transformation in an Fe-0.7 mass% C alloy has been investigated by means of transmission electron microscopy. The results obtained can be explained consistently in terms of the Bowles-Mackenzie theory assuming the [101]a(111)a lattice invariant shear and the dilatation parameter δ=0.990. This contraction can equally be replaced by the austenite lattice expansion. Cementite platelets nucleate on the ferrite ledges probably formed by lattice invariant shears at the austenite/ferrite interphase boundaries. In addition to this, the lattice expansion of austenite in the vicinity of a bainite plate corresponding to δ=0.990 suggests that partitioning of carbon atoms occurs and the carbon concentration in the austenite layer surrounding the bainite is enriched up to 1–2 mass% during the transformation. Since the cementite particles grow in size within the bainite plates, the initially formed bainites are thought to be significantly super-saturated in carbon. © 1989, The Japan Institute of Metals. All rights reserved.

Cite

CITATION STYLE

APA

Ohmori, Y. (1989). Crystallographic Analysis of Lower Bainite Transformation in Fe-0.7%c Alloy. Materials Transactions, JIM, 30(7), 487–497. https://doi.org/10.2320/matertrans1989.30.487

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free