Reverse α′ → γ transformation mechanisms of martensitic Fe–Mn and age-hardenable Fe–Mn–Pd alloys upon fast and slow continuous heating
Creators
- 1. Laboratory of Metal Physics and Technology, Department of Materials, ETH Zurich, 8093 Zurich (Switzerland)
- 2. Christian Doppler Laboratory for Early Stages of Precipitation, Vienna University of Technology, 1040 Vienna (Austria)
- 3. Center for Advanced Hybrid Materials, Monash University, Department of Materials Engineering, 3800 Clayton (Australia)
- 4. Electron Microscopy ETH Zurich (EMEZ), ETH Zurich, 8093 Zurich (Switzerland)
- 5. Institute of Materials Science and Technology, Vienna University of Technology, 1040 Vienna (Austria)
Description
The mechanisms governing the reverse martensite (α′) to austenite (γ) transformation (α′ → γ) and the effect of prior precipitation on the austenite reversion are investigated for martensitic Fe–Mn alloys containing 5 and 10 wt.% Mn and their age-hardenable variants with the addition of 1 wt.% Pd, respectively. Dilatometric experiments employing heating rates between 0.5 and 200 K min−1, atom-probe tomography measurements on continuously heated specimens and thermo-kinetic simulations were performed. On fast heating (200 K min−1), the α′ → γ transformation appeared in a single stage and can be regarded as a partitionless and interface-controlled reaction. In comparison to the binary alloys, the transformation temperatures of the Pd-containing steels are considerably increased, due to precipitates which act as obstacles to migrating austenite/martensite interfaces. For low heating rates of 0.5 and 2 K min−1, splitting of the α′ → γ transformation into two consecutive stages is observed for both the binary and the ternary alloys. With the assistance of thermo-kinetic simulations, a consistent description of this phenomenon is obtained. The first transformation stage is associated with the decomposition of the martensite matrix into Mn-rich and Mn-deficient regions, and the austenite formation is dominated by long-range diffusion. In the second stage, the austenite reversion mechanism changes and the Mn-depleted regions transform in a predominantly interface-controlled mode. This is corroborated by the results for the ternary alloys. The precipitates mainly impede the austenite formation in the second stage, which occurs over a considerably wider temperature range compared to the binary alloys
Availability note (English)
Available from http://dx.doi.org/10.1016/j.actamat.2014.03.032Additional details
Identifiers
- DOI
- 10.1016/j.actamat.2014.03.032;
- PII
- S1359-6454(14)00179-7;
Publishing Information
- Journal Title
- Acta Materialia
- Journal Volume
- 72
- Journal Page Range
- p. 99-109
- ISSN
- 1359-6454
- CODEN
- ACMAFD
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 46033081
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- AUSTENITE; BINARY ALLOY SYSTEMS; COMPUTERIZED SIMULATION; IRON; MANGANESE; MARAGING STEELS; MARTENSITE; PALLADIUM; PHASE TRANSFORMATIONS; TERNARY ALLOY SYSTEMS; TRANSFORMATIONS
- Descriptors DEC
- ALLOY SYSTEMS; ALLOYS; CARBON ADDITIONS; ELEMENTS; IRON ALLOYS; IRON BASE ALLOYS; MARTENSITIC STEELS; METALS; PLATINUM METALS; SIMULATION; STEELS; TRANSITION ELEMENT ALLOYS; TRANSITION ELEMENTS
Optional Information
- Copyright
- Copyright (c) 2014 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.