We report a study of aftereffect processes in magnetite with magnesium subs
titutions. The study observed the processes by means of disaccommodation te
chniques. We have recorded the time evolution of the initial magnetic susce
ptibility after sample demagnetization of polycrystalline specimens with no
minal composition MgxFe3-xO4, 0 less than or equal to x less than or equal
to 1 in the temperature range from 200 K to 500 K. We find that magnesium s
ubstitutions reveal interesting results about magnetic aftereffects in oxid
e spinels.