Abstract
Using diamond anvil cell, the57Fe Mössbauer spectra of pure iron foil and α-Fe2O3 powder under high pressure have been measured at room temperature.57Fe Mössbauer spectra of α-Fe were measured from 15 GPa to 45 GPa. Isomer shift value decreased and the quadrupole splitting slightly increased as the pressure increased.57Fe Mössbauer spectra of Fe2O3 under high pressure up to 72 GPa were observed. Above 52 GPa, the new lines appeared at the center portion of the spectrum corresponding to the new high pressure phase. The spectrum of new high pressure phase consisted of 6-line splitting and doublet, suggesting the existence of the two different kinds of iron states in it.
Similar content being viewed by others
References
H.G. Drickamer and C.W. Frank, Electronic Transitions and High Pressure Chemistry and Physics, (Chapman and Hall, London, 1973).
D.L. Williamson, Mössbauer Isomer shift, edited bz G.K. Shenoy and F.E. Wagner, (North-Holland, 1978), p.317.
D.L. Williamson, S. Bukshpan and R. Ingalls, Phys. Rev., 11 (1972) 4194.
Y. Syono, A. Ito, S. Morimoto, T. Suzuki, T. Yagi and S. Akimoto, Solid State Comm., 50 (1984) 97.
W.A. Basserr, T. Takahashi and P.W. Stook, Rev. Sci. Instr. 38 (1967) 37.
P.M. Bell and H.K. Mao, Carnegie Inst. Wash. Yearb., 74 (1975) 399.
R.W. Vaugham and H.G. Drickamer, J. Chem. Phys. 47 (1967) 1530.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Nasu, S., Kurimoto, K., Nagatomo, S. et al. 57Fe Mössbauer study under high pressure; ε-Fe and Fe2O3 . Hyperfine Interact 29, 1583–1586 (1986). https://doi.org/10.1007/BF02399539
Issue Date:
DOI: https://doi.org/10.1007/BF02399539