“…The scattering intensities, perpendicular to H, for the two polarization states and interference terms for samples tempered for 0 h, 1 h, and The interference term and the corresponding γ-profile as a function of tempering time depend on the evolution in chemical composition, magnetic properties, and the average dimension of the formed precipitates. From the STEM-EDS and APT results, it is known that the ATcarbides consisted of Fe and C, with no dissolution of other alloying elements [30]. These AT-carbides are believed to be replaced by cementite when heating up to a tempering temperature, of 550 • C or 600 • C. With further heating, cementite particles get increasingly enriched in substitutional elements like Cr and Mn while Si is rejected.…”