Nucleation Analysis of Variant Transformed from Austenite with Σ3 Boundary in High-Strength Low-Alloy Steel
来源期刊:Acta Metallurgica Sinica2021年第4期
论文作者:Bin-Bin Wu Zhi-Quan Wang Cheng-Jia Shang Yi-Shuang Yu Devesh Misra
文章页码:523 - 533
摘 要:We elucidate here the effects of annealing twins on phase transformation products based on electron back-scatter diffraction analysis and corresponding microstructure visualization and quantification methods.Martensite and bainite were obtained by rapid continuous cooling and isothermal processing at different temperatures,respectively,which were designed to study variants formed in austenite with Σ3 boundary.The isothermal transformation near martensite start(Ms) temperature was most conducive in obtaining the highest content of twin-related V1/V2 variant pair.Based on the classical nucleation theory of martensite and bainite,respectively,the role of austenite Σ3 boundary in martensite and bainite transformation is illustrated.
Bin-Bin Wu1,Zhi-Quan Wang1,Cheng-Jia Shang1,2,Yi-Shuang Yu1,Devesh Misra3
1. Collaborative Innovation Center of Steel Technology,University of Science and Technology Beijing2. State Key Laboratory of Metal Material for Marine Equipment and Application3. Laboratory for Excellence in Advanced Steel Research,Department of Metallurgical,Materials and Biomedical Engineering,University of Texas at El Paso
摘 要:We elucidate here the effects of annealing twins on phase transformation products based on electron back-scatter diffraction analysis and corresponding microstructure visualization and quantification methods.Martensite and bainite were obtained by rapid continuous cooling and isothermal processing at different temperatures,respectively,which were designed to study variants formed in austenite with Σ3 boundary.The isothermal transformation near martensite start(Ms) temperature was most conducive in obtaining the highest content of twin-related V1/V2 variant pair.Based on the classical nucleation theory of martensite and bainite,respectively,the role of austenite Σ3 boundary in martensite and bainite transformation is illustrated.
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