Conductivity Anisotropy in the Antiferromagnetic State of Iron Pnictides

B. Valenzuela, E. Bascones, and M. J. Calderón
Phys. Rev. Lett. 105, 207202 – Published 9 November 2010
PDFHTMLExport Citation

Abstract

Recent experiments on iron pnictides have uncovered a large in-plane resistivity anisotropy with a surprising result: The system conducts better in the antiferromagnetic x direction than in the ferromagnetic y direction. We address this problem by calculating the ratio of the Drude weight along the x and y directions, Dx/Dy, for the mean-field Q=(π,0) magnetic phase diagram of a five-band model for the undoped pnictides. We find that Dx/Dy ranges between 0.2<Dx/Dy<1.7 for different interaction parameters. Large values of the orbital ordering favor an anisotropy opposite to the one found experimentally. On the other hand, Dx/Dy is strongly dependent on the topology and morphology of the reconstructed Fermi surface. Our results point against orbital ordering as the origin of the observed conductivity anisotropy, which may be ascribed to the anisotropy of the Fermi velocity.

  • Figure
  • Figure
  • Figure
  • Received 28 July 2010

DOI:https://doi.org/10.1103/PhysRevLett.105.207202

© 2010 The American Physical Society

Authors & Affiliations

B. Valenzuela*, E. Bascones, and M. J. Calderón

  • Instituto de Ciencia de Materiales de Madrid, ICMM-CSIC, Cantoblanco, E-28049 Madrid, Spain

  • *belenv@icmm.csic.es
  • leni@icmm.csic.es
  • calderon@icmm.csic.es

Article Text (Subscription Required)

Click to Expand

Supplemental Material (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 105, Iss. 20 — 12 November 2010

Reuse & Permissions
Access Options
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review Letters

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×