Magnetic irreversibility in ultrafine ZnFe2O4 particles

Citation
Gf. Goya et al., Magnetic irreversibility in ultrafine ZnFe2O4 particles, J APPL PHYS, 87(11), 2000, pp. 8005-8007
Citations number
13
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science
Journal title
JOURNAL OF APPLIED PHYSICS
ISSN journal
00218979 → ACNP
Volume
87
Issue
11
Year of publication
2000
Pages
8005 - 8007
Database
ISI
SICI code
0021-8979(20000601)87:11<8005:MIIUZP>2.0.ZU;2-L
Abstract
Pure ultrafine ZnFe2O4 particles have been obtained from mechanosynthesis o f the ZnO and Fe2O3 oxides. The average grain diameter was estimated from x -ray diffraction to be < d >=36(6) nm. Refinement of neutron diffraction da ta showed that the resulting cubic spinel structure is oxygen deficient, wi th similar to 7% of Fe3+ ions occupying the tetrahedral A sites. Magnetizat ion curves taken at 4.2 K showed the absence of saturation in fields up to H=9 T, associated with a spin-canting produced by the milling process. Fiel d-cooled (FC) and zero-field cooled (ZFC) curves showed irreversible behavi or extending well above room temperature, which is associated with spin dis order. Annealing samples at 300 degrees C yields an average grain size < d >=50(6) nm, and similar to 16% of Fe3+ ions at A sites. Partial oxygen reco very is also deduced from neutron data refinement in annealed samples. Conc urrently, decrease of magnetic irreversibility is noticed, and assigned to partial recovery of the collinear spin structure. Complex Mossbauer spectra were observed at room temperature and 80 K, with broad hyperfine field dis tributions spanning from similar to 10 to similar to 40 T. At T=4.2 K, hype rfine field distributions indicate high disorder in Fe local environments. The above data suggest the existence of Fe-rich clusters, yielding strong s uperexchange interactions between Fe ions at A and B sites of the spinel st ructure. (C) 2000 American Institute of Physics. [S0021-8979(00)05611-5].