Abstract

The convergent beam Kikuchi line diffraction technique has been used to accurately determine the orientation relationships between bainitic ferrite and retained austenite in a hard bainitic steel. A reproducible orientation relationship has been uniquely observed for both the upper and lower bainite. It is ( 1 1 1 ) A 0.70 ± 0.45 ° from ( 1 0 1 ) B , [ 1 ¯ 0 1 ] A 2.5 ± 1.5 ° from [ 1 ¯ 1 1 ] B However, the habit plane of upper bainite is different from that of lower bainite. The former has habit plane that is either within 5° of (2 2 1) A or of (2 5 9) A. The latter only corresponds with a habit plane that is within 5° of (2 5 9) A. The determined orientation relationship is completely consistent with reported results determined using the same technique with an accuracy of ±0.5° in lath martensite in an Fe–20 wt.% Ni–6 wt.% Mn alloy and in a low carbon low alloy steel. It also agrees well with the orientation relationship between granular bainite and austenite in an Fe–19 wt.% Ni–3.5 wt.% Mn–0.15 wt.% C steel. Hence it is believed that, at least from a crystallographic point view, the bainite transformation has the characteristics of martensitic transformation.

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