Zinc ferrite belongs to the class of normal spinels where it is assume
d to have a cation distribution of Zn2+(Fe3+)(2)(O2-)(4), and it is pu
rported to be showing zero net magnetisation. However, there have been
recent reports suggesting that zinc ferrite exhibits anomaly in its m
agnetisation. Zinc ferrite samples have been prepared by two different
routes and have been analysed using low energy ion scattering, Mossba
uer spectroscopy and magnetic measurements. The results indicate that
zinc occupies octahedral sites, contrary to the earlier belief that zi
nc occupies only the tetrahedral sites in a normal spinel. The amount
of zinc on the B site increases with decrease in particle size. The LE
IS results together with the Mossbauer results and the magnetic measur
ements lead to the conclusion that zinc occupies the B site and the ma
gnetisation exhibited by ultrafine particles of zinc is due to short r
ange ordering. (C) 1998 Elsevier Science B.V. All rights reserved.