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Title: Electronic state of {sup 57}Fe used as Moessbauer probe in the perovskites LaMO{sub 3} (M=Ni and Cu)

Journal Article · · Journal of Solid State Chemistry
 [1];  [2];  [1]; ; ;  [1]
  1. Lomonosov Moscow State University, 119992 Leninskie Gory, Moscow (Russian Federation)
  2. ICMCB, CNRS, University BORDEAUX 1 'Sciences and Technologies', site de l'ENSCPB-87, Avenue du Dr A. Schweitzer, 33608 PESSAC Cedex (France)

For the first time a comparative study of rhombohedral LaNiO{sub 3} and LaCuO{sub 3} oxides, using {sup 57}Fe Moessbauer probe spectroscopy (1% atomic rate), has been carried out. In spite of the fact that both oxides are characterized by similar crystal structure and metallic properties, the behavior of {sup 57}Fe probe atoms in such lattices appears essentially different. In the case of LaNi{sub 0.99}Fe{sub 0.01}O{sub 3}, the observed isomer shift ({delta}) value corresponds to Fe{sup 3+} (3d{sup 5}) cations in high-spin state located in an oxygen octahedral surrounding. In contrast, for the LaCu{sub 0.99}Fe{sub 0.01}O{sub 3}, the obtained {delta} value is comparable to that characterizing the formally tetravalent high-spin Fe{sup 4+}(3d{sup 4}) cations in octahedral coordination within Fe(IV) perovskite-like ferrates. To explain such a difference, an approach based on the qualitative energy diagrams analysis and the calculations within the cluster configuration interaction method have been developed. It was shown that in the case of LaNi{sub 0.99}Fe{sub 0.01}O{sub 3}, electronic state of nickel is dominated by the d{sup 7} configuration corresponding to the formal ionic 'Ni{sup 3+}-O{sup 2-}' state. On the other hand, in the case of LaCu{sub 0.99}Fe{sub 0.01}O{sub 3} a large amount of charge is transferred via Cu-O bonds from the O:2p bands to the Cu:3d orbitals and the ground state is dominated by the d{sup 9}L configuration ('Cu{sup 2+}-O' state). The dominant d{sup 9}L ground state for the (CuO{sub 6}) sublattice induces in the environment of the {sup 57}Fe probe cations a charge transfer Fe{sup 3+}+O{sup -}(L){yields}Fe{sup 4+}+O{sup 2-}, which transforms 'Fe{sup 3+}' into 'Fe{sup 4+}' state. The analysis of the isomer shift value for the formally 'Fe{sup 4+}' ions in perovskite-like oxides clearly proved a drastic influence of the 4s iron orbitals population on the Fe-O bonds character. - Graphical abstract: Moessbauer spectroscopy study of LaCuO{sub 3} doped with the Moessbauer probe {sup 57}Fe.

OSTI ID:
21043750
Journal Information:
Journal of Solid State Chemistry, Vol. 180, Issue 11; Other Information: DOI: 10.1016/j.jssc.2007.09.016; PII: S0022-4596(07)00391-X; Copyright (c) 2007 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved; Country of input: International Atomic Energy Agency (IAEA); ISSN 0022-4596
Country of Publication:
United States
Language:
English