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- W2565321504 abstract "Steel, particularly carbon steel, is an ancient material. However, steel is still a new material since we do not fully understand the relationship between its microstructure and mechanical properties. A new metastable ω-Fe with a hexagonal structure and a 〜0.407 nm and c 〜0.248 nm, which is similar to the ω phase in Ti and Zr alloys, has been characterized by TEM [ 1 , 2 ] and XRD. The ω-Fe has the ultrafine particle-like morphology and a special orientation relationship with bcc-ferrite. In particular, in quenched carbon steel, there are three crystalline phases: retained austenite (fcc) with carbon, ferrite (bcc) without carbon and the ω-Fe with carbon [ 1 ]. Traditional so-called “bct” XRD pattern can be well explained by ferrite and ω-Fe in our current XRD results since an extra diffraction peak, which has a d-spacing of about 0.251nm, has been detected from low-carbon to high carbon steels. The proposed bct martensite, which appears commonly in our textbook, cannot explain this peak. With the ω-Fe, the various transformation products in carbon steel can be easily understood [ 3 ]." @default.
- W2565321504 created "2017-01-06" @default.
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- W2565321504 date "2015-11-01" @default.
- W2565321504 modified "2023-09-25" @default.
- W2565321504 title "B22-O-04The discovery of ω-Fe in common steels by TEM and XRD" @default.
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- W2565321504 doi "https://doi.org/10.1093/jmicro/dfv149" @default.
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