Abstract
Mössbauer spectra of Fe(Cr, Al)2O4 spinels are reported and interpreted using partial quadrupole splitting theory. Fe2+T site quadrupole splittings are calculated for different next-nearest neighbour configurations. Assuming random distribution of the Cr3+ and Al3+ in the octahedral M sites, good semiquantitative agreement between calculated and observed quadrupole splittings and absorption intensities is obtained.
Original language | English (US) |
---|---|
Pages (from-to) | 623-625 |
Number of pages | 3 |
Journal | Solid State Communications |
Volume | 47 |
Issue number | 8 |
DOIs | |
State | Published - Aug 1983 |
ASJC Scopus subject areas
- Chemistry(all)
- Condensed Matter Physics
- Materials Chemistry