Phases de type quartz alpha ; structure de FePO4 et spectrometrie Mossbauer du fer-57
Revue de chimie minéralePublished 1 January 1986
Aline Goiffon, Jean‐Claude Jumas, Etienne Philippot
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Abstract
FePO 4 cristallise dans le systeme rhomboedrique, groupe d'espace P3 1 2 1 . Sa structure est affinee jusqu'a R=0,032 a 173°K et jusqu'a R=0,028 a 293°K. Les distorsions des sites tetraedriques diminuent quand la temperature augmente
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ChemistryEarth and Planetary SciencesArts and Humanities