Oxygen ordering and the orthorhombic-to-tetragonal phase transition in YBa2Cu3O7x

J. D. Jorgensen, M. A. Beno, D. G. Hinks, L. Soderholm, K. J. Volin, R. L. Hitterman, J. D. Grace, Ivan K. Schuller, C. U. Segre, K. Zhang, and M. S. Kleefisch
Phys. Rev. B 36, 3608 – Published 1 September 1987
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Abstract

In situ neutron powder diffraction measurements show that the orthorhombic-to-tetragonal phase transition in YBa2Cu3O7x, which occurs near 700°C in a pure oxygen atmosphere, is an order-disorder transition in which the disordering of oxygen atoms into a normally vacant site destroys the one-dimensional Cu-O chains present in the room-temperature orthorhombic structure. For both structures, the oxygen stoichiometry decreases monotonically with increasing temperature. The transition temperature depends on the oxygen partial pressure and occurs when the stoichiometry is near YBa2Cu3O6.5. The tetragonal structure has a partially occupied, nearly octahedral Cu-O arrangement, in contrast to the orthorhombic structure which has one-dimensional Cu-O chains. The observed depression of the superconducting transition temperature in tetragonal YBa2Cu3O7x, which has been quenched from high temperature, could result either from the disordering of oxygen atoms which destroys the one-dimensional chains or from the absence of Cu3+ ions.

  • Received 2 June 1987

DOI:https://doi.org/10.1103/PhysRevB.36.3608

©1987 American Physical Society

Authors & Affiliations

J. D. Jorgensen, M. A. Beno, D. G. Hinks, L. Soderholm, K. J. Volin, R. L. Hitterman, J. D. Grace*, and Ivan K. Schuller

  • Argonne National Laboratory, Argonne, Illinois 60439

C. U. Segre, K. Zhang, and M. S. Kleefisch

  • Illinois Institute of Technology, Chicago, Illinois 60616

  • *Permanent address: Department of Geology, Western Michican University, Kalamazoo, MI 49008.
  • Also at Amoco Research Laboatories, Naperville, IL 60540.

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Vol. 36, Iss. 7 — 1 September 1987

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