Kinetic Modeling of Grain Boundary Cementite Evolution

被引:2
|
作者
Vogric, M. [1 ]
Kozeschnik, E. [2 ]
Svoboda, J. [3 ]
Fuhrer, M. [1 ]
Kreyca, J. [4 ]
Wei, W. [1 ]
Povoden-Karadeniz, E. [1 ,2 ]
机构
[1] TU Wien, Inst Mat Sci & Technol, Christian Doppler Lab Interfaces & Precipitat Eng, A-1060 Vienna, Austria
[2] TU Wien, Inst Mat Sci & Technol, A-1060 Vienna, Austria
[3] Acad Sci Czech Republ, Inst Phys Mat, Brno 61600, Czech Republic
[4] Voestalpine Forsch Serv Gesell Donawitz GmbH, A-8700 Leoben, Austria
关键词
MULTICOMPONENT MULTIPHASE SYSTEMS; GROWTH-KINETICS; IRREVERSIBLE-PROCESSES; RECIPROCAL RELATIONS; DIFFUSIONAL GROWTH; HABIT PLANE; FERRITE; LEDGES; MICROSTRUCTURE; TRANSFORMATION;
D O I
10.1007/s11661-022-06784-1
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Prediction of grain boundary cementite growth kinetics in hypereutectoid steels is necessary to control its thickness. It is a question of major industrial importance but has remained unresolved to date. This paper presents and compares two different and new modeling approaches. The first one relies on diffusion-based nucleation and growth of cementite precipitates using a modified SFFK model with short-circuit grain boundary diffusion and accounting for heterogeneous nucleation site energy during isothermal treatments and continuous cooling. It is compared to previously published simulations of diffusion-controlled reaction with moving phase boundaries and a similar simulation using the software Dictra. The second approach implies that cementite thickening is driven by the nucleation of ledges at the stepped austenite/cementite interface, controlled by a structure barrier to ledge formation previously assumed in the literature.([1]) We suggest a semi-empirical formulation of this barrier to ledge nucleation during isothermal transformation. Both approaches lead to an excellent match to experimental data for an almost pure Fe-C system. This implies that modeling the stepped structure of the austenite/cementite interface is not imperative for simulation of thickening kinetics, but also that understanding the governing physics of ledge formation allows for a comprehensive description of secondary cementite formation.
引用
收藏
页码:3759 / 3773
页数:15
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