Abstract
Mössbauer study of orthorhombic and tetragonal YBa2(Cu1-xFex)3O7-σ;x=0.02, 0.04, 0.08 has been done to investigate the two inequivalent Cu-sites. Fe substituting Cu having pyramidal oxygen co-ordination is in Fe3+ state while Fe substituting Cu having square planar co-ordination is in Fe3+ and Fe4+ states in dynamic equilibrium.
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Shringi, S.N., Prakash, O.M., Vadnere, R.V. et al. Mössbauer study of Fe-substituted orthorhombic and tetragonal YBa2(Cu1-xFex)3O7-σ system. Pramana - J. Phys. 32, L699–L704 (1989). https://doi.org/10.1007/BF02847391
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DOI: https://doi.org/10.1007/BF02847391