Abstract
The Mössbauer spectra of five samples of Fe x O with compositions in the range 1.00>x>0.95 have been recorded at 298 K and 4.2 K. The spectrum of Fe x O at 298 K consists of an asymmetric doublet which was fitted to one Fe2+ singlet, two Fe2+ doublets and 1 Fe3+ singlet. The Mössbauer parameters vary consistently with the increasing density of defects as x decreases. The Mössbauer spectrum of Fe x O at 4.2 K consists of a large number of unresolved lines. The data were fitted to a series of singlets to enable the rough calculation of quantities relating to the mean Fe2+ and Fe3+ environments. The results of the fits to the 298 K spectra are briefly discussed in terms of a physical model for the defect structure of Fe x O.
Similar content being viewed by others
References
Andersson B, Sletnes JO (1977) Decomposition and ordering in Fe1−x O. Acta Crystollogr A33:268–276
Bauer E, Pianelli A (1980) Mise au point sur la structure lacunaire de la wüstite et necessite de nouvelles recherches experimentales. Mat Res Bull 15:177–188
Boyd FR, England JL (1960) Apparatus for phase-equilibrium measurements at pressures up to 50 kilobars and temperatures up to 1,750° C. J Geophys Res 65:741–748
Checherskaya LF, Romanov VP, Tatsienko PA (1973) Mössbauer effect in wüstite. Phys Status Solidi 19A: K177-K182
Cranshaw TE (1974) Mössbauer spectroscopy. J Phys E 7:497–505
Elias DJ, Linnett JW (1969) Oxidation of metals and alloys. III. Mössbauer spectrum and structure of wüstite. Trans Faraday Soc 65:2673–2677
Giddings RA, Gordon RS (1973) Review of oxygen activities and phase boundaries in wüstite as determined by electromotive-force and gravimetric methods. J Am Ceram Soc 56:111–116
Greenwood NN, Howe AT (1972) Mössbauer studies of Fe1−x O. Part 1. The defect structure of quenched samples. J Chem Soc Dalton Trans: 110–116
Hentschel B (1970) Stoichiometric FeO as metastable intermediate of the decomposition of wüstite at 225° C. Z Naturforsch 25:1996–1997
Johnson DP (1969) Mössbauer study of the local environments of 57Fe in FeO. Solid State Commun 7:1785–1788
Katsura T, Iwasaki B, Kimura S, Akimoto S (1967) High-pressure synthesis of the stoichiometric compound FeO. J Chem Phys 47:4559–4560
Koch F, Cohen JB (1969) The defect structure of Fe1−x O. Acta Crystallogr B25:275–287
Kurash VV, Gol'danskii VI, Malysheva TV, Urusov VS (1972) Mössbauer spectrum of wüstite at low temperaturs. Inorg Mater (USSR) 8:1183–1184
McCammon CA, Liu L (1984) The effects of pressure and temperature on nonstoichiometric wüstite, Fe x O: The iron-rich phase boundary. Phys Chem Minerals 10:106–113
Price DC (1981) Empirical lineshape for computer fitting of spectral data. Aust J Phys 34:51–56
Ringwood AE, Major A (1968) Apparatus for phase transformation studies at high pressures and temperatures. Phys Earth Planet Inter 1:164–168
Romanov VP, Checherskaya LF (1972) Mössbauer spectra of non-stoichiometric and stoichiometric wüstites. Phys Status Solidi 49B:K183-K187
Roth WL (1960) Defects in the crystal and magnetic structures of ferrous oxide. Acta Crystallogr 13:140–149
Simons B, Seifert F (1979) High-pressure wüstite cell parameters and Mössbauer spectra. Ann Rep Geophys Lab 78:625–626
Violet CE, Pipkorn DN (1971) Mössbauer line positions and hyperfine interactions in α iron. J Appl Phys 11:4339–4342
Willis BTM, Rooksby HP (1953) Change of structure of ferrous oxide at low temperature. Acta Crystallogr 6:827–831
Window B, Dickson BL, Routcliffe P, Srivastava KKP (1974) A versatile multiple Mössbauer spectrometer. J Phys E Sci Instru 7:916–921
Yamamoto A (1982) Modulated structure of wüstite (Fe1−x O) (three-dimensional modulation). Acta Crystallogr B38:1451–1456
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
McCammon, C.A., Price, D.C. Mössbauer spectra of Fe x O (x>0.95). Phys Chem Minerals 11, 250–254 (1985). https://doi.org/10.1007/BF00307402
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/BF00307402