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Phys. Rev. B 76, 014526 (2007) [8 pages]

Upper limit on spontaneous supercurrents in Sr2RuO4

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J. R. Kirtley1,2,3, C. Kallin4, C. W. Hicks1, E.-A. Kim5,6, Y. Liu7, K. A. Moler1,5, Y. Maeno8, and K. D. Nelson7
1Department of Applied Physics, Stanford University, Palo Alto, California 94305, USA
2IBM Watson Research Center, Yorktown Heights, New York 10598, USA
3Faculty of Science and Technology and MESA+ Institute for Nanotechnology, University of Twente, 7500 AE Enschede, The Netherlands
4Department of Physics and Astronomy, McMaster University, Hamilton, Ontario, Canada L8S 4M1
5Department of Physics, Stanford University, Palo Alto, California 94305, USA
6Stanford Institute of Theoretical Physics, Stanford University, Palo Alto, California 94305, USA
7Department of Physics, Pennsylvania State University, University Park, Pennsylvania, 16802, USA
8Department of Physics, Kyoto University, Kyoto 606-8502, Japan

Received 25 April 2007; published 26 July 2007

It is widely believed that the perovskite Sr2RuO4 is an unconventional superconductor with broken time-reversal symmetry. It has been predicted that superconductors with broken time-reversal symmetry should have spontaneously generated supercurrents at edges and domain walls. We have done careful imaging of the magnetic fields above Sr2RuO4 single crystals using scanning Hall bar and superconducting quantum interference device microscopies, and see no evidence for such spontaneously generated supercurrents. We use the results from our magnetic imaging to place upper limits on the spontaneously generated supercurrents at edges and domain walls as a function of domain size. For a single domain, this upper limit is below the predicted signal by 2 orders of magnitude. We speculate on the causes and implications of the lack of large spontaneous supercurrents in this very interesting superconducting system.

© 2007 The American Physical Society

URL:
http://link.aps.org/doi/10.1103/PhysRevB.76.014526
DOI:
10.1103/PhysRevB.76.014526
PACS:
74.50.+r, 74.72.−h, 73.40.Gk, 73.40.Rw