“…Spinodal decomposition in ferrite (δ) to form Fe-enriched (Cr-depleted) α 1 and Cr-enriched (Fe-depleted) α 11 structures, or the nucleation and growth of α 11 -particles embedded in an α 1 -matrix can occur, typically followed by the formation of further precipitates, such as χ, Frank-Kasper R-phase, τ, or Mo-Si enriched G-phase [5,7,[9][10][11][12][13][14][15]. The phase separation products (α 1 + α 11 ), in general, do not exceed dimensions larger than 100 nm, whereas precipitates such as G-or R-phase can grow to sizes larger than 500 nm [6,[10][11][12][13][14]. It should be noted that similar phase reactions have also been reported in austenite, which, however, requires further investigations to make clear statements about their origin [8,9,16,17].…”