Modified Z-Phase Formation in a 12% Cr Tempered Martensite Ferritic Steel during Long-Term Creep

TL;DR

This study investigates the formation and evolution of modified Z-phase in 12Cr tempered martensite ferritic steel during long-term creep at 550°C and 120 MPa, revealing its correlation with MX precipitate dissolution and creep strain.

Contribution

It provides detailed quantitative analysis of Z-phase formation, MX precipitate dissolution, and microstructural changes during long-term creep in 12Cr steel.

Findings

Modified Z-phase precipitates in creep-ruptured steel samples.

MX precipitates dissolve progressively during creep.

Creep strain promotes localized Z-phase formation.

Abstract

The formation of modified Z-phase in a 12Cr1MoV (German grade: X20) tempered martensite ferritic (TMF) steel subjected to interrupted long-term creep-testing at 550$^{\circ}$C and 120 MPa was investigated. Quantitative volumetric measurements collected from thin-foil and extraction replica samples showed that modified Z-phase precipitated in both the uniformly-elongated gauge ($f_v$: 0.23 $\pm$ 0.02 %) and thread regions ($f_v$: 0.06 $\pm$ 0.01 %) of the sample that ruptured after 139 kh. The formation of modified Z-phase was accompanied by a progressive dissolution of MX precipitates, which decreased from ($f_v$: 0.16 $\pm$ 0.02 %) for the initial state to ($f_v$: 0.03 $\pm$ 0.01 %) in the uniformly-elongated gauge section of the sample tested to failure. The interparticle spacing of the creep-strengthening MX particles increased from ($\lambda_{3D}$: 0.55 $\pm$ 0.05 $\mu m$) in the initial state to ($\lambda_{3D}$: 1.01 $\pm$ 0.10 $\mu m$) for the uniformly-elongated gauge section of the ruptured sample, while the thread region had an interparticle spacing of ($\lambda_{3D}$: 0.60 $\pm$ 0.05 $\mu m$). The locally deformed fracture region had an increased phase fraction of modified Z-phase ($f_v$: 0.40 $\pm$ 0.20 %), which implies that localised creep-strain strongly promotes the formation of modified Z-phase. The modified Z-phase precipitates did not form only on prior-austenite grain boundaries and formed throughout the tempered martensite ferritic grain structure.