Abstract
The double perovskites contain ions for Zn, Co, and Ni and for and Fe, ions. Annealed samples have ordered and Ru(IV), but samples with ions are atomically disordered and remain oxidized after annealing in a atmosphere. A comparison of quenched, air-annealed, and -annealed samples showed a persistence of a few cation vacancies in the presence of oxygen vacancies In quenched samples, oxygen vacancies are preferentially located between two Ru atoms, where they form a deep two-electron trap state, whereas the two-electron trap state formed at an oxygen vacancy between an and Ru(IV) is shallow. Magnetic as well as transport data indicate the π-bonding electrons at the low-spin Ru atoms occupy itinerant-electron states of a band even in the atomically ordered samples, but strong correlations introduce magnetic transitions among the electrons. The and Ni samples exhibit a magnetic transition at some, if not all, of the electrons on the Ru array below a independent of magnetic ordering on the ions, and below a antiferromagnetic ordering of the -ion spins suppresses any spin on the intervening Ru(IV). The antiferromagnetic superexchange interaction is stronger than the ferromagnetic interaction because of a weak intraatomic exchange with the -electron spins on the Ru(IV) atoms. On the other hand, disordered is ferromagnetic with a magnetization at 5 K of per formula unit (f.u.) in a magnetic field of 50 kOe. This finding is interpreted with a model in which the π-bonding orbitals on both the Mn and Ru are coupled to form a common ferromagnetic band in which only the antibonding electrons are not spin paired. The strong next-nearest-neighbor interaction between Ru atoms made manifest in the ordered double perovskites provides an explanation of why the bandwidth of the perovskite system may increase with
- Received 8 October 2003
DOI:https://doi.org/10.1103/PhysRevB.69.094416
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