Abstract
57Fe Mössbauer and X-ray diffraction measurements have been performed on a perovskite CaFeO3 under external high pressure upto 50 GPa at room temperature using a diamond anvil cell. Above 29 GPa the57Fe magnetic hyperfine splitting appears superimposing with usual paramagnetic pattern of CaFeO3. Magnitude of hyperfine field is 16 T and much smaller than 33 T of typical Fe4+ in SrFeO3 suggesting a transition from high-spin S=2 to low-spin S=1 state in CaFeO3.
Similar content being viewed by others
References
S. Nasu, K. Kurimoto, S. Nagatomo, S. Endo and F.E. Fujita, Hyp. Int., 29 (1986) 1583.
M. Pasternak and R.D. Taylor, Hyp., Int., 47 (1989) 415.
S. Nasu, T. Abe, K. Yamamoto, S. Endo, M. Takano and Y. Takeda, Hyp., Int., (1991) in press.
M. Takano and Y. Takeda, Bull, of the Inst. for Chem. Res., 61 (1983) 406.
Y. Takeda et al., Mat. Res. Bull. 13 (1978) 61.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Nasu, S., Abe, T., Yamamoto, K. et al. Mössbauer study of CaFeO3 under external high—Pressure. Hyperfine Interact 70, 1063–1066 (1992). https://doi.org/10.1007/BF02397512
Issue Date:
DOI: https://doi.org/10.1007/BF02397512