Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5361570 | Applied Surface Science | 2008 | 4 Pages |
Abstract
The spinel CoFe2O4 has been synthesized by combustion reaction technique. X-ray photoelectron spectroscopy shows that samples are near-stoichiometric, and that the specimen surface both in the powder and bulk sample is most typically represented by the formula (Co0.4Fe0.6)[Co0.6Fe1.4]O4, where cations in parentheses occupy tetrahedral sites and those within square brackets in octahedral sites. The results demonstrate that most of the iron ions are trivalent, but some Fe2+ may be present in the powder sample. The Co 2p3/2 peak in powder sample composed three peaks with relative intensity of 45%, 40% and 15%, attributes to Co2+ in octahedral sites, tetrahedral sites and Co3+ in octahedral sites. The O 1s spectrum of the bulk sample is composed of two peaks: the main lattice peak at 529.90Â eV, and a component at 531.53Â eV, which is believed to be intrinsic to the sample surface. However, the vanishing of the O 1s shoulder peak of the powder specimen shows significant signs of decomposition.
Related Topics
Physical Sciences and Engineering
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Physical and Theoretical Chemistry
Authors
Zhongpo Zhou, Yue Zhang, Ziyu Wang, Wei Wei, Wufeng Tang, Jing Shi, Rui Xiong,