Abstract
In order to clarify the difference between the deformation-induced ε-martensite (ε 1) and the pressure-induced ε-iron (ε 2), high-pressure quasi-hydrostatic experiments were performed on a low-carbon, high-alloy metastable austenitic steel. In situ synchrotron X-ray diffraction measurements as well as post-mortem investigations of the microstructure by electron backscatter diffraction were carried out to study the microstructural transformations. Three processes were observed during compression experiments: first, the formation of deformation-induced hexagonal ε 1-martensite, as well as small nuclei of deformation-induced bcc α′-martensite (α 1′) within the fcc γ-matrix due to non-hydrostaticity in the experiments; second, the onset of the phase transformation from the metastable fcc γ-austenite into the hexagonal pressure-induced ε 2-iron phase occurred at around 6 GPa; third, during decompression, the hexagonal pressure-induced ε 2-iron transformed partially into bcc α′-martensite (α 2′). Completely different characteristics with regard to habitus as well as to orientation relationships were observed between the pressure-induced phases (ε 2-iron phase and α 2′-martensite) and the deformation-induced martensites (ε 1- and α 1′-martensite).
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Acknowledgments
The authors wish to thank the German Research Foundation for its financial support of the Collaborative Research Centre “TRIP-Matrix Composites” (CRC 799). Dr. A. Jahn and Dr. T. Kreschel (Institute of Iron and Steel Technology) are gratefully acknowledged for providing the material used and for the heat treatment, respectively. Dr. S. Guk (Institute of Metal Forming) is acknowledged for the hot rolling of the material. Furthermore, the authors thank Ms. K. Zuber, Ms. Y. Klemm, and Mr. C. Segel (Institute of Materials Engineering) for specimen preparation and further experimental assistance. All institutes mentioned belong to the TU Bergakademie Freiberg, Germany.
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Ackermann, S., Martin, S., Schwarz, M.R. et al. Investigation of Phase Transformations in High-Alloy Austenitic TRIP Steel Under High Pressure (up to 18 GPa) by In Situ Synchrotron X-ray Diffraction and Scanning Electron Microscopy. Metall Mater Trans A 47, 95–111 (2016). https://doi.org/10.1007/s11661-015-3082-2
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DOI: https://doi.org/10.1007/s11661-015-3082-2