“…[9][10][11] Embrittlement is usually ascribed to spinodal decomposition of the ferrite, namely, the formation of Fe-enriched a¢ phase and Cr-enriched a¢¢ phase, or the formation of Cr-enriched a¢¢ precipitates embedded in a Fe-rich a¢ matrix after aging in the 523 K to 823 K (250°C to 550°C) temperature window. [9,[12][13][14][15][16] Ferrite is not stable within the miscibility gap and, therefore, decomposes into two phases. However, additional phases can also form in the ferrite and coexist with the spinodal decomposition products, such as G and R phase, as well as other secondary phases, [7,[9][10][11][12][17][18][19][20][21][22][23][24][25][26][27] which also can have significant impact on mechanical properties.…”