The magnetic aftereffect and induced uniaxial anisotropy Ku have been studied between 50° and 300°C in the Co
xFe
3-xO
4+γsystem with

0.0150. A peak of disaccommodation (DA) found between 110° and 140°C is followed at higher temperature by a new phenomenon called "accommodation of the permeability" (A) that gives, according to the composition, a negative minimum on the DA curve located between 200° and 230°C. The amplitude of the minimum increases with x. The maximum amplitudes

on the curves Ku =f (θ) are proportional to x. The two effects A and DA are due to the presence of Co
2+ions. A hypothesis is proposed to explain the A phenomenon.