Abstract
Thermal decomposition of natural siderite and goethite has been studied using Mössbauer spectroscopy and X-ray diffraction. Hematite and magnetite were the principal compounds formed during high temperature treatment of siderite. Natural goethite transformed to hematite at high temperatures. The crystal structures, stoichiometry and the nuclear magnetic properties of Fe-oxides formed are discussed.
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Musić, S., Popović, S. Mössbauer spectroscopic and X-ray diffraction study of the thermal decomposition of natural siderite and goethite. Journal of Radioanalytical and Nuclear Chemistry, Articles 111, 27–41 (1987). https://doi.org/10.1007/BF02060518
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DOI: https://doi.org/10.1007/BF02060518