Influence of Reverted Austenite on Tensile Deformation and Fracture in 18Ni 250 Maraging Steel

奥氏体 材料科学 马氏体 马氏体时效钢 加工硬化 冶金 极限抗拉强度 体积分数 应变率 流动应力 硬化(计算) 变形(气象学) 复合材料 微观结构 图层(电子)
作者
Benjamin Rohit,M. Nageswara Rao
出处
期刊:Journal of Testing and Evaluation [ASM International]
卷期号:51 (2): 766-783
标识
DOI:10.1520/jte20220122
摘要

Abstract Overaging of C250 maraging steel leads to reversion of austenite. The percentage of reverted austenite in the microstructure increases with an increasing extent of overaging. The effect of volume fraction of reverted austenite on the deformation behavior during tensile testing was studied. Specimens in the solution-annealed condition of the steel were overaged using different temperature/time combinations to produce a range of reverted austenite volume fractions. Changes in the lattice parameter of the martensite phase as a function of overaging treatment were monitored. X-ray diffraction technique was used to measure the volume fraction of reverted austenite and monitor the changes in lattice parameter of martensite. True stress–true strain curves were calculated from the engineering stress–engineering strain diagrams obtained for different overaging treatments, and plots showing the rate of work hardening as a function of true strain were derived. The present investigation shows that the reverted austenite produced at 538°C and 620°C induces serrated flow during tensile testing, whereas reverted austenite produced at 510°C does not. It is believed that the reverted austenite formed at the two higher temperatures is not stable because of the relatively lower amount of nickel and transforms to martensite on tensile deformation, leading to serrated flow. After aging at 510°C and 538°C, after the initial steep drop in the work hardening rate, the rate remains nearly constant over a certain range of true strain before it starts dropping again. After aging at 620°C, in contrast, the work hardening rate continuously decreases with increasing true strain. The precipitates formed after aging at 510°C/538°C are believed to be important contributions to the occurrence of the plateau. The results show that not only the quantity of reverted austenite but also the temperature at which reversion took place influence the fracture mechanisms and fracture surface appearance.
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