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Phys. Rev. B 67, 020409(R) (2003) [4 pages]

Polaronic orbital polarization in a layered colossal magnetoresistive manganite

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B. J. Campbell1,*, S. K. Sinha2,3, R. Osborn1, S. Rosenkranz1, J. F. Mitchell1, D. N. Argyriou1, L. Vasiliu-Doloc4, O. H. Seeck4, and J. W. Lynn5
1Materials Science Division, Argonne National Laboratory, Argonne, Illinois 60439
2Department of Physics, University of California at San Diego, La Jolla, California 92093
3Los Alamos Neutron Science Center, Los Alamos National Laboratory, Los Alamos, New Mexico 87545
4Advanced Photon Source, Argonne National Laboratory, Argonne, Illinois 60439
5NIST Center for Neutron Research, National Institute of Standards and Technology, Gaithersburg, Maryland 20899

Received 30 August 2002; published 31 January 2003

The striking anisotropy observed in Huang scattering distributions near the intense Bragg reflections of La1.2Sr1.8Mn2O7 is shown to be the result of orbitally polarized polarons in the paramagnetic insulating state above TC. X-ray single-crystal diffuse scattering patterns from this bilayered colossal magnetoresistive manganite are calculated in terms of the polaronic local structure and compared with experimental measurements. At 300 K, the polaronic eg electrons occupy “out-of-plane” (i.e., 3z2-r2) orbitals, leading to MnO6 octahedra that are Jahn-Teller elongated along the c axis, perpendicular to the perovskite layers. Between 300 K and TC, however, the “orbital polarization” is shown to shift into the a-b plane (i.e., 3x2-r2 and 3y2-r2 orbitals), allowing the formation of nanoscale polaron correlations above TC.

© 2003 The American Physical Society

URL:
http://link.aps.org/doi/10.1103/PhysRevB.67.020409
DOI:
10.1103/PhysRevB.67.020409
PACS:
75.47.Gk, 71.30.+h, 71.38.-k, 71.45.Lr

*Present address: Department of Physics and Astronomy, Brigham Young University, Provo, UT 84602.