A mathematical model is considered and equations are obtained for esti
mating the parameters of critical reduction-product nuclei in multicom
ponent systems. For the Fe-O-Si system, it is shown that the nuclei ar
e of complex composition, in the form of solutions of SiO2 and FeO, wi
th sharp reduction in the cationic proportion of FeO from 0.48 to 0.06
; this leads to anomalous reduction in the rate of steady nucleation (
by 36 orders of magnitude) in the interval [Si] = 0.004-0.006% (when [
O] = 0.2% at 1600 degrees C).