Title: POSCO Lectures on Bainite
1POSCO Lectures on Bainite
- Microstructure
- Mechanism
- Properties
- Superbainite
Graduate Institute of Ferrous Technology
2http//cml.postech.ac.kr/
3To understand bainite, we must consider all other
microstructures in steels
4Bundy (1965)
5Allotropes of iron in three dimensions
6Cementite Fe3C
7Steel Fe-C
ferrite
austenite
8Fe3C
9Diffusionless
Diffusion
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12AllotriomorpicIdiomorphicferrite
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18Pearlite
19 20 µm
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22Jaramillo et al., 2004
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26Martensite
27Ferrite
Austenite
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30transformation twins (Wayman)
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33austenite
34Chang and Bhadeshia
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36Bainite
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38upper bainite
1 µm
39lower bainite
40Surface 1
Surface 2
50 µm
Srinivasan Wayman, 1968
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4550 µm
46Bhadeshia and Waugh, 1981
47Takahashi and Bhadeshia
48Fe-0.4C wt
Decarburisation time / s
Temperature / C
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51Bhadeshia Edmonds, 1979
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54TRIP-assisted steel Fe-0.29C-1.41Si-1.42Mn wt
(Jacques, 2001)
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56Growth is diffusionless.
Strain energy must be accounted for.
57Takahashi and Bhadeshia
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59Oka and Okamoto
60Ohmori and Honeycombe
61Summary
The mechanism of transformation is
displacive. Transformation temperature higher
than martensite. Bainite grows without
diffusion. But carbon then escapes into the
residual austenite. Shape deformation plastically
accommodated. Sub-unit mechanism of growth
62Think of bainite as martensite which tempers
during transformation
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65DISPLACIVE
RECONSTRUCTIVE
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72Watson and McDougall, 1973
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76Summary
Mechanism displacive but carbon must partition
during growth. Pairs of plates grow together to
minimise strain.
77Nucleation of martensite, bainite, Widmanstätten
ferrite
78Thermodynamics
g
a
Gibbs free energy
x
Carbon
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81Each point represents a different steel
Bhadeshia, 1981
82The nucleation of bainite must involve the
partitioning of carbon
Why does the required free energy vary linearly
with T?
83hexagonal close-packed
cubic close-packed
Christian, 1951
84Brooks, Loretto and Smallman, 1979
85Olson Cohen, 1976
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89Nucleation of bainite must involve the
partitioning of carbon.
Mechanism of nucleation is otherwise identical to
that of martensite.
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