The microstructure evolution and softening processes during high-temperature deformation of a 21Cr–10Ni–3Mo duplex stainless steel

• Published in: Acta materialia Vol. 106; pp. 129 - 143
• Main Author: Cizek, P.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01-03-2016
• Subjects: Austenite; Boundaries; Deformation mechanisms; Duplex stainless steel; Duplex stainless steels; Dynamic softening; Dynamics; Ferrite; High-temperature deformation; Microstructure; Softening; Ferrite; Duplex stainless steel; High-temperature deformation; Dynamic softening; Austenite
• ISSN: 1359-6454; 1873-2453
• DOI: 10.1016/j.actamat.2016.01.012

The austenite and ferrite microstructure evolution and softening mechanisms have been investigated in a 21Cr–10Ni–3Mo duplex stainless steel, containing about 60% austenite, deformed in torsion at 1200 °C using a strain rate of 0.7 s−1. The above experimental conditions led to the formation of a small volume fraction of new austenite grains through discontinuous dynamic recrystallization (DDRX), which could not account for the observed large softening on the flow curve. DDRX grains mainly formed through the strain-induced migration of the pre-existing austenite grain boundaries, known to dominate in single-phase austenite, complemented by subgrain growth in the interface regions with ferrite. A significant portion of austenite dynamic softening has been attributed to the large-scale subgrain coalescence, the extent of which increased with strain, which seems to have contributed substantially to the observed flow stress decrease. The above process thus appears to represent an alternative mode of austenite dynamic softening to the classical DDRX in the duplex austenite/ferrite microstructure, characterised by limited availability of the pre-existing austenite/austenite high-angle boundaries, deformed at a high temperature. The softening mechanism within ferrite has been classified as “continuous DRX”, characterised by a gradual increase in misorientations between neighbouring subgrains with strain and resulting in the progressive conversion of subgrains into “crystallites” bounded partly by low-angle and partly by large-angle boundaries.
[Display omitted]