Crystallography of [0 1 1]/54.7° lath boundary and cementite in tempered 0.2C steel

Abstract

The crystallographic structures of the [0 1 1]/54.7° lath boundary and the intralath and interlath cementite precipitates in a 0.2C steel tempered at 400 °C have been observed by high resolution transmission electron microscopy and discussed in terms of the O-lattice model. The [0 1 1]/54.7° lath boundary which is composed of one Kurdjumov–Sachs variant ( α1) and one Nishiyama–Wasserman variant ( α2) is likely to facet on the (0 12 7) α1 //(5 19 14) α2 irrational plane. The O-lattice analysis indicated that the facet coincides with a plane with a high density of O-points. Intralath cementite obeys the Isaichev orientation relationship (OR) with ferrite and has a habit plane of (1 0 1) θ //(1 2 1) α . Interlath cementite precipitating on the [0 1 1]/54.7° boundary maintains a strict Bagaryatskii OR with the ferrite on one side of the boundary and has a (1 0 0) θ habit plane.