“…For the a-site formation to occur, the reduced Fe 2+ atoms should convert into a new stable state, in which they lose their ability to react with O 2 and thus make the step (1) irreversible. The process of the Fe 2+ stabilization appeared to depend on the chemical composition of the matrix and is strongly facilitated by the presence of water vapor [20,26,30,71,78]. Presumably, the stabilization can occur in the form of complex (III), in which Fe 2þ 2 entities are strongly incorporated into a silicate fragment of the zeolite matrix and have a more distant position as compared to complex (II), thus making impossible their reoxidation into the latter complex.…”