Interaction of carbon partitioning, carbide precipitation and bainite formation during the Q&P process in a low C steel

Journal Article (2016)
Author(s)

Farideh Hajy-Akbary (TU Delft - (OLD) MSE-3, Material Innovation Institute (M2i))

J. Sietsma (TU Delft - (OLD) MSE-3)

Goro Miyamoto (Tohoku University)

T Furuhara (Tohoku University)

M.J. Santofimia (TU Delft - (OLD) MSE-3)

Research Group
(OLD) MSE-3
Copyright
© 2016 F. Hajy Akbary, J. Sietsma, G. Miyamoto, T Furuhara, Maria Jesus Santofimia
DOI related publication
https://doi.org/10.1016/j.actamat.2015.11.032
More Info
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Publication Year
2016
Language
English
Copyright
© 2016 F. Hajy Akbary, J. Sietsma, G. Miyamoto, T Furuhara, Maria Jesus Santofimia
Research Group
(OLD) MSE-3
Volume number
104
Pages (from-to)
72-83
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Abstract

Theoretical understanding of the “quenching and partitioning” (Q&P) process allowed developing microstructures consisting of carbon-depleted martensite and retained austenite that deliver superior mechanical properties. Most of the models describing the Q&P process are limited to systems in which carbide precipitation in martensite and decomposition of austenite to bainite are totally suppressed. However, these reactions are often unavoidable, even in low-carbon steels containing a relatively high concentration of Si and Mn. This work investigates interactions between carbon partitioning, carbide precipitation and carbide-free bainite formation during the Q&P process of a 0.3C–1.6Si–3.5Mn (wt.%) steel with non-homogenous distribution of the alloying elements. It was found that prior to the partitioning step ɛ-carbide forms in martensite. The decomposition of this carbide is required for a full completion of the carbon partitioning from martensite to austenite. Slow kinetics of decomposition of ɛ-carbide retards the carbon partitioning process. Results show that a fraction of austenite becomes stable by carbon partitioning and does not decompose to bainite. In the specimens quenched to lower temperature, a higher fraction of austenite becomes stable and consequently a lower fraction of bainite is formed.

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