Abstract
The surface magnetism of Fe(001) was studied in an atomic layer-by-layer fashion by using the in situ iron-57 probe layer method with a synchrotron Mössbauer source. The observed internal hyperfine field exhibits a marked decrease at the surface and an oscillatory behavior with increasing depth in the individual upper four layers below the surface. The calculated layer-depth dependencies of the effective hyperfine field , isomer shift , and quadrupole shift agree well with the observed experimental parameters. These results provide the first experimental evidence for the magnetic Friedel oscillations, which penetrate several layers from the Fe(001) surface.
- Received 9 February 2020
- Revised 13 July 2020
- Accepted 16 October 2020
DOI:https://doi.org/10.1103/PhysRevLett.125.236806
© 2020 American Physical Society
Physics Subject Headings (PhySH)
synopsis
Magnetic Oscillations at a Metal Surface
Published 3 December 2020
Predicted 40 years ago, magnetic Friedel oscillations are finally observed in the layers beneath an iron surface.
See more in Physics