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Morphology of bainite and Widmanstaetten ferrite

Journal Article · · Metallurgical Transactions, A (Physical Metallurgy and Materials Science); (United States)
OSTI ID:7157400
; ;  [1]; ;  [2]
  1. Ehime Univ., Matsuyama (Japan). Dept. of Materials Science and Engineering
  2. Sumitomo Metal Industries, Amagasaki (Japan). Iron and Steel Research Labs.
Morphology of bainite and Widmanstaetten ferrite in various steels has been investigated by means of microstructural and surface relief observations. It was shown that upper and lower bainite should be classified by ferrite morphology, i.e., lathlike or platelike, and that the morphology of cementite precipitation cannot be the index for the classification. Widmanstaetten ferrite formed in the upper C-nose where ferrite grain-boundary allotriomorphs nucleate exhibits quite similar appearance with bainitic ferrite that forms in the lower C-nose of bainitic reaction. The only difference between them exists in the fact that Widmanstaetten ferrite laths grow in the temperature range where primary ferrite forms and often terminate at a grain boundary ferrite but that bainitic ferrite has its own C-curve at temperatures below B[sub s] and nucleates directly at an austenite grain boundary. The mechanisms for their formations are discussed.
OSTI ID:
7157400
Journal Information:
Metallurgical Transactions, A (Physical Metallurgy and Materials Science); (United States), Journal Name: Metallurgical Transactions, A (Physical Metallurgy and Materials Science); (United States) Vol. 25:9; ISSN 0360-2133; ISSN MTTABN
Country of Publication:
United States
Language:
English

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