The reduction mechanism of a natural chromite at 1416 °C
- 1 February 1991
- journal article
- Published by Springer Nature in Metallurgical Transactions B
- Vol. 22 (1), 53-63
- https://doi.org/10.1007/bf02672527
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Cation Distribution and Defect Chemistry of Iron‐Aluminate SpinelsJournal of the American Ceramic Society, 1981
- Carbon in solid solution in forsterite—a key to the untractable nature of reduced carbon in terrestrial and cosmogenic rocksGeochimica et Cosmochimica Acta, 1980
- Iron Diffusion in Iron‐Aluminate SpinelsJournal of the American Ceramic Society, 1980
- Defects and Cation Diffusion in Magnetite (II)Berichte der Bunsengesellschaft für physikalische Chemie, 1977
- Omission solid solution in magnetite: Kenotetrahedral magnetite*Zeitschrift für Kristallographie, 1969
- Oxygen penetration into CaF2:Sm2+ crystalsJournal of Physics and Chemistry of Solids, 1968
- The thermodynamics of cation distributions in simple spinelsJournal of Inorganic and Nuclear Chemistry, 1967
- Divalent chromium in magnesium-chromium spinelsJournal of Physics and Chemistry of Solids, 1966
- Existence of Chromous Ion in the Spinel Solid Solution Series FeCr2O4‐MgCr2O4Journal of the American Ceramic Society, 1966
- Oxygen Mobility in Polycrystalline NiCr2O4 and α‐Fe2O3Journal of the American Ceramic Society, 1960