Bulletin of the American Physical Society
APS March Meeting 2019
Volume 64, Number 2
Monday–Friday, March 4–8, 2019; Boston, Massachusetts
Session Y10: Surface Science of Organic Molecular Solids, Films, and Nanostructures - Materials Synthesis, Deposition, and Device preparation
11:15 AM–1:51 PM,
Friday, March 8, 2019
BCEC
Room: 151B
Sponsoring
Units:
DMP DCMP
Chair: Dane McCamey,
Abstract: Y10.00001 : Magnetism of ultra-short one dimensional atomic chains*
11:15 AM–11:51 AM
Presenter:
Nicolas Vargas
(Physics, University of California, San Diego)
Authors:
Nicolas Vargas
(Physics, University of California, San Diego)
Carlos Monton
(Physics and Astronomy, University of Texas at San Antonio)
Felipe Torres
(Physics, Universidad de Chile)
Miguel G Kiwi
(Physics, Universidad de Chile)
Dora Altbir
(Physics, Universidad de Santiago de Chile)
Vagson Carvalho-Santos
(Physics, Universidade Federal de Viçosa)
Alexander A. Baker
(Condensed Matter and Materials Division, Lawrence Livermore National Laboratory)
Trevor M Willey
(Condensed Matter and Materials Division, Lawrence Livermore National Laboratory)
Ivan Schuller
(Physics, University of California, San Diego)
We report structural and magnetic properties of one-dimensional Fe chains as a function of length in the 10 to 200 atoms range. These Fe chains are grown using iron phthalocyanine (FePc) thin films and FePc/ metal-free-phthalocyanine (H2Pc) superlattices (SLs). The length of 1D Fe chains is precisely controlled by the deposited thickness of the FePc layers.
Although structurally identical, 1D Fe chains formed in films and superlattices have different magnetic behavior. In films, the coercive field remains almost constant whereas in SLs increases with the length of the chain. This difference can be explained using a semi-classical model, which combines short range direct Exchange and Dzyaloshinskii-Moriya interactions. The increase of the coercive field in SLs is attributed to a magnetization reversal process which is governed by chiral symmetry breaking produced by a weak magnetic anisotropy. This anisotropy originates at the extreme of the Fe chains by proximity with the H2Pc layers and is observable by element selective X-ray absorption spectroscopy (XAS).
*Work supported by the Department of Energy’s Office of Basic Energy Science under grant DE FG02 87ER-45332, the National Science Foundation under grant No. 1804414 and 1805585, and AFOSR Grant FA9550-16-1-0122.
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