Analytical interpretation of temperature dependent combined quadrupolar and magnetic hyperfine interaction in Fe2+ Fe3 2+(PO4)2(OH)2 (barbosalite)
Résumé
Synthetic barbosalite Fe2+ Fe32+(PO 4)2(OH)2 measured between 4.2 to 295 K by Mössbauer Spectroscopy shows a magnetic phase transition at 162 K. The spectra presenting combined quadrupolar and magnetic hyperfine interactions are interpreted using an analytical method.
Origine : Accord explicite pour ce dépôt
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