Magnetization measurements of the ferrite system Mg1+xMnxFe2-2xO4 were
undertaken primarily to study variation of the saturation magnetizati
on with manganese concentration and to gain information about the type
of magnetic ordering. The observations indicate the existence of Yafe
t-Kittel (YK) type of magnetic ordering in this system which is well s
upported by results of Mossbauer effect measurements. A molecular fiel
d analysis of the YK spin ordering using the three-sublattice model is
shown to explain the experimental data satisfactorily.