Proceedings of the Physical Society · 1928 · 13 citations · 0 references
Natural SciencesChemistryEarth SciencesInorganic ChemistryMagnetic MaterialsMineralogyFerromagnetic MaterialsFerromagnetismHydrate FormationIron OxidesMagnetic OxidesMetal OxidesCrystalline StructureFeo PhasesFerrous-to-ferric ConversionParamagnetic Species
A brief account is given of work relating to the above subject that has been published during the past eight years. The authors confirm the observation by Messrs. Sosman and Posnjak that lepidocrocite, but not göthite, yields on dehydration a strongly ferromagnetic ferric oxide. As all the specimens of lepidocrocite examined contained three or four per cent. of manganese oxide, they suggest that this substance may be an essential constituent of this crystalline form of the hydrate. They find that the temperature at which the ferromagnetic oxide is permanently transformed into the common paramagnetic kind is largely dependent upon its mode of preparation.