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Magnetic phase transition, aggregate formation, and electrical conductivity in FeCl3-doped polyacetylene

E. K. Sichel, M. F. Rubner, J. Georger, Jr., G. C. Papaefthymiou, S. Ofer, and R. B. Frankel
Phys. Rev. B 28, 6589(R) – Published 1 December 1983
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Abstract

Both Fe3+ and Fe2+ ions occur in FeCl3-doped polyacetylene. At low dopant levels (<0.01 mole fraction) both Fe2+ and Fe3+ ions are paramagnetic down to 4.2 K. At dopant levels >0.01 mole fraction, there is evidence from Mössbauer spectroscopy that Fe2+ ions associate into aggregates which are magnetically ordered below 25 K. Aggregate formation appears to correlate with high electrical conductivity.

  • Received 6 June 1983

DOI:https://doi.org/10.1103/PhysRevB.28.6589

©1983 American Physical Society

Authors & Affiliations

E. K. Sichel, M. F. Rubner, and J. Georger, Jr.

  • GTE Laboratories, 40 Sylvan Rd., Waltham, Massachusetts 02254

G. C. Papaefthymiou, S. Ofer*, and R. B. Frankel

  • Francis Bitter National Magnet Laboratory, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139

  • *Deceased; formerly at Racah Institute of Physics, Hebrew University, Jerusalem, Israel.

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Vol. 28, Iss. 11 — 1 December 1983

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