Abstract
The mixed valence iron silicate ilvaite, CaFe 2+2 Fe3+Si2O8(OH), displays electron delocalization associated with Fe2+→Fe3+ charge transfer as observed by Mössbauer spectroscopy. Previous studies report the observation of an ‘electron hopping phenomenon’ with resolution of discrete valence states below 320 K. Mössbauer spectra of a suite of naturally occurring ilvaites were recorded over a temperature range, 80 K to 575 K. Five quadrupole doublets were resolved by computer fitting and assigned to Fe2+(A), Fe2+(B), Fe3+(A), and Fe2+(A)→Fe3+(A)‖c and ⊥c. Contrary to prior work, doublets associated with electron delocalization are resolved at 80 K and preclude the use of a Verwey-type order-disorder model. We propose a thermal activation model and discuss its criteria from molecular orbital and mineralogical viewpoints.
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Nolet, D.A., Burns, R.G. Ilvaite: A study of temperature dependent electron delocalization by the mössbauer effect. Phys Chem Minerals 4, 221–234 (1979). https://doi.org/10.1007/BF00307946
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DOI: https://doi.org/10.1007/BF00307946