The independent grain model previously employed in analyzing the effect of stress on remanence ratios with stress parallel to the magnetic field has been extended to include the case of stress perpendicular to the field. In addition, the results have been averaged to obtain more realistic approximations to the stress sensitivities as functions of the magnetic anisotropy constant K
1and magnetostriction constant λ
100and λ
111. From theory, it is concluded that for

, the parallel stress sensitivity is eliminated when

. For the perpendicular case,

with

and

with

. For

, both stress sensitivities may be removed when

. The results of experiments with both single crystal and polycrystalline Y
3Mn
xFe
5-xO
12compositions show qualitative agreement with theory, but also indicate that other mechanisms probably influence changes in remanence ratio.