Published February 2012 | Version v1
Journal article

Microstructure and crystallography of borides and secondary precipitation in 18 wt.% Cr–4 wt.% Ni–1 wt.% Mo–3.5 wt.% B–0.27 wt.% C steel

  • 1. State Key Laboratory for Mechanical Behaviour of Materials, School of Materials Science and Engineering, Xi'an Jiaotong University, Xi'an, Shaanxi Province 710049 (China)
  • 2. Research Institute of Advanced Materials Processing Technology, School of Materials Science and Engineering, Beijing University of Technology, Beijing 100124 (China)

Description

The microstructure and crystallography of eutectic borides and secondary precipitations in 18 wt.% Cr–4 wt.% Ni–1 wt.% Mo–3.5 wt.% B–0.27 wt.% C steel have been investigated extensively. The results show that the as-cast microstructure of Cr–Ni–Mo-containing Fe–B steel is composed of a dendritic martensite with large interdendritic eutectic borides. Transmission electron microscopy (TEM) results confirm that the borides are indexed to Cr- and Mo-rich M2B-type borides with the chemical formulas of Fe(1.35–1.36)Cr(0.92–1.05)B0.96 and Fe0.73Cr0.45Mo0.78B, respectively. The cluster-like boride possesses a possible orientation relationship between body-centred orthorhombic Cr-rich M2B and martensite with 〈11¯0〉M2B//〈1 1 0〉α growth direction. After destabilization, M23(C, B)6 secondary borocarbide with a specific orientation relationship precipitates first and thereafter coarsens following the appearance of M7(C, B)3 precipitation with the increasing destabilization temperature at the same soaking time, thus leading to a large decrease of Cr content in the martensite. However, no M6(C, B) secondary borocarbide is found in as-destabilized Fe–B steel. Destabilization treatment has no effect on the morphology of eutectic borides. The secondary borocarbides have the stoichiometry of (Fe18.26Cr4.74)(B, C)6 and (Fe3.86Cr3.14)(B, C)3 respectively. The high-resolution TEM results indicate that the nucleation and precipitation of M23(C, B)6 occur at the grain/subgrain boundaries as well as partial within martensite, and a subsequent transformation from M23(C, B)6 to M7(C, B)3 takes place in situ, which is probably owing to the crystalline defects of dislocations and stacking faults in the structures caused by lattice distortion.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.actamat.2011.11.004

Additional details

Identifiers

DOI
10.1016/j.actamat.2011.11.004;
PII
S1359-6454(11)00780-4;

Publishing Information

Journal Title
Acta Materialia
Journal Volume
60
Journal Issue
3
Journal Page Range
p. 831-843
ISSN
1359-6454
CODEN
ACMAFD

Optional Information

Copyright
Copyright (c) 2011 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.