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.
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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
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