轨道钢片层珠光体在压缩变形下的组织演变

K. Aksenova, V. Gromov, Y. Ivanov, E. Vashchuk, O. Peregudov
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引用次数: 0

摘要

本文介绍了轨钢珠光体在单轴压缩变形作用下片层状缺陷亚结构演变的分析结果。所研究的钢在这种变形下的应变硬化具有多阶段特征。钢的变形伴随着珠光体晶粒的破碎,随着变形程度的增加,珠光体晶粒的破碎程度加剧,在ε = 50%时达到所研究箔体积的0.4。铁氧体板上形成的碎片被低角度边界隔开。结果表明,随着变形程度的增加,铁氧体薄片的平均尺寸从240 nm (ε = 15%)减小到200 nm (ε = 50%)。渗碳体板出现碎裂。结果表明,裂纹大小在15 ~ 20 nm之间,与钢的变形程度关系不大。渗碳体薄片的断裂是由渗碳体的溶蚀和移动位错切割引起的。碳原子从渗碳体的晶格过渡到位错,进入层间空间,形成三级渗碳体颗粒,其尺寸为2 ~ 4 nm。在钢的变形过程中,由于渗碳体颗粒对位错的减速作用,形成了不均匀位错亚结构。变形程度的增加伴随着位错的标量和过量密度的降低,这可能是由于位错逃逸到低角度边界中,以及它们的湮灭。确定了内部应力场的来源为珠光体晶粒与菌落之间的界面、珠光体晶粒中的渗碳体板、位于铁素体板体积中的第二相颗粒。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evolution of structure of rail steel lamellar pearlite under compression deformation
The article presents the results of analysis of evolution of the defective substructure of rail steel pearlite with lamellar morphology under deformation by uniaxial compression. The strain hardening of the studied steel under such deformation has a multistage character. Deformation of steel is accompanied by fragmentation of pearlite grains, which intensifies as the degree of deformation increases and reaches 0.4 of the studied foil volume at ε = 50 %. Fragments formed in ferrite plates are separated by low-angle boundaries. It was established that the average sizes of ferrite plate fragments decrease from 240 nm (ε = 15 %) to 200 nm (ε = 50 %) with an increase in the deformation degree. Fragmentation of cementite plates was revealed. It was found that the size of the fragments varies within 15 – 20 nm and weakly depends on the degree of steel deformation. Fracture of cementite lamellae, proceeding by their dissolution and cutting by mobile dislocations, was discovered. Carbon atoms that have passed from the crystal lattice of cementite to dislocations are carried out into the interlamellar space and form particles of tertiary cementite, the size of which is 2 – 4 nm. In the process of steel deformation, an inhomogeneous dislocation substructure is formed, which is due to the deceleration of dislocations by cementite particles. It was found that an increase in the deformation degree is accompanied by a decrease in the scalar and excess density of dislocations, which may be due to the escape of dislocations into low-angle boundaries, as well as their annihilation. It was established that the sources of internal stress fields are the interfaces between pearlite grains and colonies, cementite plates in pearlite grains, particles of the second phase located in the volume of ferrite plates.
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