Numéro |
J. Phys. I France
Volume 7, Numéro 6, June 1997
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Page(s) | 777 - 784 | |
DOI | https://doi.org/10.1051/jp1:1997191 |
J. Phys. I France 7 (1997) 777-784
57Fe Mössbauer Spectroscopy on Two Romanian Carpathian Pumpellyites
S. Constantinescu1, Gh. Udubasa2 and S. Calogero31 Institute of Physics and Technology of Materials, PO Box Mg-07, Bucharest, Romania
2 Geological Institute of Romania, 78344, Bucharest, Romania
3 Universita Ca'Foscari, Dipartamento di Chimica-Fisica, 30123 Venezia, Italy
(Received 13 January 1997, revised 20 February 1997, accepted 8 March 1997)
Abstract
The authors obtained the Fe
57 Mössbauer spectra of two pumpellyite samples obtained from two different mineral sources in the Romanian Carpathians. Using
a specialized computation program of the quadrupole splitting spectral parameter, QSCOMP, the observed quadrupole doublets
were attributed to the ferric and ferrous ions in octahedral sites. The refined analysis of spectral parameters permitted
us to characterize both the oxidation state, the electronic configuration and the coordination symmetry with the distortions
and occupancies of pumpellyite constituting iron ions. The differences of the spectral parameters giving the data of the iron
abundance, the chemical iron-oxygen bonds, the deformation and occupancies of iron octahedra, observed at the two studied
samples, are discussed and correlated by the different genesis conditions of two pumpellyite-bearing occurrences.
© Les Editions de Physique 1997