Six natural crystals from the Sludyanka crystalline complex belonging to the eskolaite (Cr2O3)– karelianite (V2O3)hematite (Fe2O3) solid solution were studied by means of X-ray diffraction and electron microprobe. The Fe3+-poor samples show a general increase in a and c cell parameters with increasing mean cationic radius (MCR), consistent with that shown by the synthetic crystals along the eskolaite–karelianite join. The Fe3+-richer sample deviates significantly from the behaviour shown by the Fe3+-poor ones, similar to synthetic andnatural hematites; with increasing MCR, the a and c cell parameters increase linearly along the eskolaite–karelianite join. However, for the samples rich in Fe3+, from karelianite to hematite, a shows a slightly steeper slope whereas the c parameter decreases strongly. The octahedral distortion increases slightly as a function of MCR along the eskolaite– karelianite join, whereas it increases markedly for Fe3+-rich samples. The evolution of the octahedral edges and of the octahedral distortions as a function of MCR are responsible for the behaviour of the unit-cell parameters along the eskolaite–karelianite–hematite join.

Crystal chemcal study of R-3c natural oxides along the eskolaite - karelianite - hematite (Cr2O3 -V2O3-Fe2O3) join

SECCO, LUCIANO;NESTOLA, FABRIZIO;DAL NEGRO, ALBERTO;
2008

Abstract

Six natural crystals from the Sludyanka crystalline complex belonging to the eskolaite (Cr2O3)– karelianite (V2O3)hematite (Fe2O3) solid solution were studied by means of X-ray diffraction and electron microprobe. The Fe3+-poor samples show a general increase in a and c cell parameters with increasing mean cationic radius (MCR), consistent with that shown by the synthetic crystals along the eskolaite–karelianite join. The Fe3+-richer sample deviates significantly from the behaviour shown by the Fe3+-poor ones, similar to synthetic andnatural hematites; with increasing MCR, the a and c cell parameters increase linearly along the eskolaite–karelianite join. However, for the samples rich in Fe3+, from karelianite to hematite, a shows a slightly steeper slope whereas the c parameter decreases strongly. The octahedral distortion increases slightly as a function of MCR along the eskolaite– karelianite join, whereas it increases markedly for Fe3+-rich samples. The evolution of the octahedral edges and of the octahedral distortions as a function of MCR are responsible for the behaviour of the unit-cell parameters along the eskolaite–karelianite–hematite join.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11577/2471234
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