We have performed small-angle polarized-neutron scattering from ultra-
fine ZnFe2O4 particles to confirm the intraparticle magnetic structure
, which has been considered the origin of its peculiar magnetic featur
es. On the basis of the Q-dependent differential neutron-scattering in
tensity, we were unable to detect any magnetic structure consisting of
magnetically inactive surface layer with magnetic core. Thus, the mag
netic behavior of ultra-fine ZnFe2O4 particles is explained in terms o
f a deviation in cation distribution from the normal spinel structure.