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The 57Fe Mössbauer spectra have been recorded at 300 K from an Fe4 + -containing oxygen-deficient perovskite-related SrFeO3 phase and its fluorinated derivative. The fluorinated phase shows complex magnetically split hyperfine patterns reflecting the interactions between Fe3 + ions which are not possible in oxides containing Fe4 + . The 57Fe Mössbauer spectra recorded in situ above 300 K enable the...
The 57Fe Mössbauer spectra have been recorded at 300 K from an Fe4 + -containing oxygen-deficient perovskite-related SrFeO3 phase and its fluorinated derivative. The fluorinated phase shows complex magnetically split hyperfine patterns reflecting the interactions between Fe3 + ions which are not possible in oxides containing Fe4 + . The 57Fe Mössbauer spectra recorded in situ above 300 K enable the...
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