![](https://d3ilqtpdwi981i.cloudfront.net/9nRw73AZhYB2qLOSEuU_LCYGcq0=/0x5:299x391/425x550/smart/https://bepress-attached-resources.s3.amazonaws.com/uploads/c4/d1/44/c4d14492-7a83-4785-9964-81cb5b144114/jpccck.2014.118.issue-24.largecover.jpg)
In spite of the various theoretical and experimental efforts performed to understand the origin of ferromagnetism in Fe and Co codoped ZnO, there are still serious controversies in the reported data. While theoretical studies predicted the relative spin alignment and location of Co2+ and Fe2+ as the main source of magnetism, experimental studies have reported Co2+and superficial Fe3+. In this work, we performed a careful experimental study on Zn1–2xFexCoxO (x = 0, 0.01, 0.03, and 0.05) nanoparticles prepared by a sol–gel method and have found new interesting results. We detected only Fe3+ ions located in tetrahedral-core and pseudo-octahedral-surface sites. The Co ions displayed 2+ and 3+ oxidation states, with Co2+ ions in high spin state located mostly in the tetrahedral-core sites, while Co3+ in low spin states located presumably in pseudo-octahedral-surface sites. We detected isolated Fe3+ ions and weakly ferromagnetic coupled Co2+ ions. The most important finding is that the saturation magnetization (Ms) did not depend on the magnetic interactions involving the high spin Co2+or Fe3+; but Ms and Co3+ concentration increased systematically with x, indicating that multivalent ionic states may be playing a crucial role in the observed ferromagnetism.
Available at: http://works.bepress.com/alex_punnoose/52/