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Magnetismus Poster: Do., 13:00–15:30 D-P261<br />

Neutron Diffraction Study of the Manganites Heavily Doped By Fe and Cr<br />

Iions<br />

I. O. Troyanchuk 1 , M. V. Bushinsky 1 , K. Baerner 2 , H. Szymczak 3<br />

1 Joint Institute of Solid State and Semiconductor Physics, National Academy of Sciences<br />

– 2 IV. Physikalisches Institut Bunsenstrasse 13, D37073 Göttingen, Germany<br />

– 3 Institute of Physics, National Academy of Science, al. Lotnikov 32/36, Warsaw,<br />

Poland<br />

At present there are many manganite systems studied in which manganese ions are<br />

substituted for other 3d- or diamagnetic ones. It is found that Cr and Fe ions have<br />

the strongest effect on magnetic properties, small additions of them can result in a<br />

change of the ground magnetic state. However the magnetic structure of manganites<br />

heavily doped by Cr and Fe is unknown. So we have performed neutron diffraction<br />

and magnetic studies for NdMn1−xFexO3 and NdMn1−xCrxO3 manganites in a wide<br />

range of Fe and Cr dopants. Crystal structure of compound with x=0.5 has been<br />

refined in space groups Pnma and P21/n. However, the refinement in P21/n group<br />

did not improve significantly the reliability factors in comparison with the space group<br />

Pnma what points the absence of the Mn and Cr ions ordering. Oxygen octahedron<br />

around 3d-ions is rather elongated along one of the axes. This may be expected in<br />

the case of Jahn-Teller stabilization of dz2 orbitals of manganese ions. The angles<br />

O-Mn/Cr-O and O-Mn/Fe-O are close to 1520, what is much less than in manganites<br />

of lanthanum doped with alkaline earth. In NdMn0.5Cr0.5O3 the magnetic structure<br />

has been revealed consisting of both ferromagnetic and G-type antiferromagnetic components<br />

resulting from a 3d-ions magnetic moments ordering. Magnetic moments of<br />

Nd-ions are parallel to the ferromagnetic component. In NdMn0.5Fe0.5O3 only the<br />

antiferromagnetic G-type structure has been revealed whereas Nd-sublattice is not ordered.<br />

According to spectroscopic data both Cr and Fe ions in manganites adopt 3+<br />

oxidative state. The magnetic moments of 3d-ions calculated from neutron diffraction<br />

data are much less than one can expect in the ionic model where the magnetic moments<br />

should be definitely localized. One can suppose the significant part of 3d-ions magnetic<br />

moments to be in the spin glass state and not contribute therefore into the coherent<br />

magnetic scattering of neutrons. Magnetic phase diagrams have been constructed for<br />

the both systems, interpreted assuming superexchange interactions Mn 3+ -O-Cr 3+ to<br />

be positive and Mn 3+ -O-Fe 3+ negative and taking into account the disordered arrangement<br />

of Mn and Cr ions in the crystal structure sublattice. The sign of Mn 3+ -O-Mn 3+<br />

superexchange interaction is governed with a dynamic nature of Jahn-Teller effect.<br />

Magnetic phase separation phenomenon has been ascribed to the intrinsic chemical<br />

inhomogeneity of solid solutions.

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