Abstract
Pine cone is the surface produced by fracture along P-segregated martensite/austenite interfaces which form at prior austenitic grain boundaries and is caused by reverted austenite at the grain boundaries. Intercritical tempering promotes austenite formation thereby enhances the irregularity of the grain boundary and reduces the fraction of intergranular fracture. The retained austenite at the grain boundaries transforms to martensite during fracture.
| Original language | English |
|---|---|
| Pages (from-to) | 808-814 |
| Number of pages | 7 |
| Journal | Transactions of the Iron and Steel Institute of Japan |
| Volume | 23 |
| Issue number | 10 |
| Publication status | Published - 1983 Oct |
| Externally published | Yes |
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ASJC Scopus subject areas
- Engineering(all)
Cite this
TEMPER EMBRITTLEMENT AND PINE CONE LIKE FRACTURE SURFACE OF 5. 5% Ni CRYOGENIC STEELS. / Murakami, Masato; Shibata, Koji; Nagai, Kotobu; Fujita, Toshio.
In: Transactions of the Iron and Steel Institute of Japan, Vol. 23, No. 10, 10.1983, p. 808-814.Research output: Contribution to journal › Article
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TY - JOUR
T1 - TEMPER EMBRITTLEMENT AND PINE CONE LIKE FRACTURE SURFACE OF 5. 5% Ni CRYOGENIC STEELS.
AU - Murakami, Masato
AU - Shibata, Koji
AU - Nagai, Kotobu
AU - Fujita, Toshio
PY - 1983/10
Y1 - 1983/10
N2 - Pine cone is the surface produced by fracture along P-segregated martensite/austenite interfaces which form at prior austenitic grain boundaries and is caused by reverted austenite at the grain boundaries. Intercritical tempering promotes austenite formation thereby enhances the irregularity of the grain boundary and reduces the fraction of intergranular fracture. The retained austenite at the grain boundaries transforms to martensite during fracture.
AB - Pine cone is the surface produced by fracture along P-segregated martensite/austenite interfaces which form at prior austenitic grain boundaries and is caused by reverted austenite at the grain boundaries. Intercritical tempering promotes austenite formation thereby enhances the irregularity of the grain boundary and reduces the fraction of intergranular fracture. The retained austenite at the grain boundaries transforms to martensite during fracture.
UR - http://www.scopus.com/inward/record.url?scp=0020829707&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0020829707&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0020829707
VL - 23
SP - 808
EP - 814
JO - ISIJ International
JF - ISIJ International
SN - 0915-1559
IS - 10
ER -