Nanostructured ZnFe2O4 ferrites with different grain sizes were prepared by
high energy ball milling for various milling times. Both the average grain
size and the root mean square strain were estimated from the x-ray diffrac
tion line broadening. The lattice parameter initially decreases slightly wi
th milling and it increases with further milling. The magnetization is foun
d to increase as the grain size decreases and its large value is attributed
to the cation inversion associated with grain size reduction. The Fe-57 Mo
ssbauer spectra were recorded at 300 K and 77 K for the samples with grain
sizes of 22 and 11 nm. There is no evidence for the presence of the Fe2+ ch
arge state. At 77 K the Mossbauer spectra consist of a magnetically ordered
component along with a doublet due to the superparamagnetic behaviour of s
mall crystalline grains with the superparamagnetic component decreasing wit
h grain size reduction. At 4.2 K the sample with 11 nm grain size displays
a magnetically blocked state as revealed by the Mossbauer spectrum. The Mos
sbauer spectrum of this sample recorded at 10 K in an external magnetic fie
ld of 6 T applied parallel to the direction of gamma rays clearly shows fer
rimagnetic ordering of the sample. Also, the sample exhibits spin canting w
ith a large canting angle, maybe due to a spin-glass-like surface layer or
grain boundary anisotropies in the material.