Cr对低碳含Ti微合金钢奥氏体等温分解行为的影响

  • 熊杰 ,
  • 蓝慧芳 ,
  • 李林鲜 ,
  • 唐帅 ,
  • 刘振宇 ,
  • 王国栋
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  • 东北大学 数字钢铁全国重点实验室  沈阳 110819

收稿日期: 2024-08-28

  修回日期: 2025-02-26

  网络出版日期: 2025-04-15

基金资助

国家自然科学基金项目;国家自然科学基金项目

Effect of Cr on the Isothermal Decomposition Behavior of Austenite in Low-Carbon Ti Bearing Microalloyed Steel

  • XIONG Jie ,
  • LAN Hui-Fang ,
  • LI Lin-Xian ,
  • TANG Shuai ,
  • LIU Zhen-Yu ,
  • YU Guo-Dong
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  • State Key Laboratory of Digital Steel, Northeastern University, Shenyang 110819, China

Received date: 2024-08-28

  Revised date: 2025-02-26

  Online published: 2025-04-15

Supported by

National Natural Science Foundation of China;National Natural Science Foundation of China

摘要

在析出强化型铁素体钢中,Cr元素有利于细化碳化物尺寸,提高铁素体强度。析出行为与铁素体相变密切相关,然而,Cr对铁素体相变动力学的影响还存在争议。本工作通过实验和数值模拟研究了Cr对低碳含Ti微合金钢奥氏体等温分解行为的影响,利用Thermo-calc热动力学计算了铁素体和珠光体转变驱动力和铁素体生长动力学,结合第一性原理计算阐述了Cr促进珠光体形成的原因。等温实验结果表明,Cr元素抑制铁素体形核和长大,促进奥氏体分解为珠光体。热动力学计算表明,Cr降低了γα相变驱动力,导致临界形核半径(r*)和临界形核功(ΔG*)增加;此外,Cr显著降低C在奥氏体中的扩散系数,增加扩散激活能(Qc),2者综合作用导致铁素体形核缓慢。铁素体生长期间,在可忽略配分的局域平衡(NPLE)模式下,相变由C扩散控制,Cr通过降低奥氏体中C扩散系数,降低铁素体生长速率;在配分局域平衡(PLE)模式下,相变由合金元素扩散控制,由于扩散系数DCr < DMn < DSi,导致铁素体生长速率更慢。Cr元素可以大幅降低渗碳体Gibbs自由能,增加珠光体转变驱动力。结合第一性原理计算,Cr原子倾向置换(Fe, Mn)3C合金渗碳体中Fe和Mn原子,特别是Fe原子,可以显著降低渗碳体形成能,促进渗碳体析出,从而促进珠光体转变。

本文引用格式

熊杰 , 蓝慧芳 , 李林鲜 , 唐帅 , 刘振宇 , 王国栋 . Cr对低碳含Ti微合金钢奥氏体等温分解行为的影响[J]. 金属学报, 0 : 0 -0 . DOI: 10.11900/0412.1961.2024.00301

Abstract

Ferrite precipitation-strengthened steel characterized by a large amount of nano-carbide precipitation has been widely used in the automotive industry to meet its growing energy-reduction requirements. Because of its high strength and excellent tensile flange properties, it has always been of great interest to researchers. Among the topics of interest, the composition of nanoscale carbides and their precipitation behavior have always been a popular subject area of research. In recent years, studies have confirmed that the addition of Cr is beneficial to the formation of nanoscale complex carbide in ferrite and can refine the size of and increase the number density of precipitates, thereby enhancing the strength of the ferrite. The precipitation behavior of carbides is closely related to the phase transformation of ferrite. However, there is controversy about how Cr affects the kinetics of the ferrite phase transition. This study investigated the effect of Cr on the isothermal decomposition behavior of austenite in low-carbon Ti-bearing microalloyed steel using experimental and numerical simulation methods. The driving forces behind the transformation of ferrite and pearlite, as well as the growth kinetics of ferrite, were calculated using Thermo-Calc software for thermodynamics. The reasons for Cr promoting the formation of pearlite were elucidated through first-principles calculations. The isothermal experimental results indicate that Cr element inhibits the nucleation and growth of ferrite and promotes the decomposition of austenite into pearlite. Thermodynamic calculations show that Cr reduces the driving force behind the γ-to-α phase transition, which results in an increase in the critical nucleation radius (r*) and critical nucleation work (ΔG*). Moreover, Cr significantly reduces the diffusion coefficient of C in austenite and increases austenite’s diffusion activation energy (Qc). The combined effect of both factors leads to the slow nucleation of ferrite. During the growth of ferrite, its phase transformation under negligible-partitioned local equilibrium (NPLE) mode is controlled by C diffusion. Cr reduces the diffusion coefficient of C in austenite, thereby decreasing the growth rate of ferrite. Under partitioned local equilibrium (PLE) mode, the phase transformation is controlled by the diffusion of the alloying elements. Because the diffusion coefficients (Di) of element i follow the order DCrDMn DSi, the growth rate of ferrite is slow. Furthermore, Cr element can significantly reduce the Gibbs free energy of the cementite, thereby increasing the driving force of the transformation of pearlite. According to first-principle calculations, Cr atoms tend to substitute for Fe and Mn atoms in cementite, a (Fe, Mn)3C alloy. Particularly for the Fe atoms, they can markedly decrease the formation energy and promote the precipitation of cementite, thereby facilitating the transformation to pearlite.

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