| Literature DB >> 17813310 |
U Colombo, F Gazzarrini, G Lanzavecchia, G Sironi.
Abstract
All magnetites are oxidized topotactically with formation of solid solution at temperatures below 400 degrees C. The oxidation of hematite-free magnetites proceeds to gammaFe(2)O(3), whereas in the presence of hematite epitaxial growth of alphaFe(2)O(3) takes place, with excess iron ions being returned to the solid solution. A method for synthesizing maghemite from natural magnetites is indicated.Entities:
Year: 1965 PMID： 17813310 DOI： 10.1126/science.147.3661.1033
Source DB: PubMed Journal: Science ISSN： 0036-8075 Impact factor: 47.728