Loading…

Single-ion model of the surface anisotropy in YIG films: Axial D fields

This paper introduces a simple model to calculate the surface anisotropy in (001), (111) and (110) yttrium iron garnet (YIG) films. We use single-ion anisotropy model for the Fe3+ ions in YIG. Our model takes into account the contribution from the Fe3+ ions sitting in a very thin surface layer, and...

Full description

Saved in:
Bibliographic Details
Published in:Journal of magnetism and magnetic materials 2013-08, Vol.340, p.32-37
Main Authors: Manuilov, S.A., Grünberg, P.A.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:This paper introduces a simple model to calculate the surface anisotropy in (001), (111) and (110) yttrium iron garnet (YIG) films. We use single-ion anisotropy model for the Fe3+ ions in YIG. Our model takes into account the contribution from the Fe3+ ions sitting in a very thin surface layer, and crystalline defects: substitutes and vacancies which behave similar to diamagnetic ions on the octahedral and tetrahedral sites of YIG. The calculated surface anisotropies are on the order of 10−2erg/cm2 at 295K for all crystalline orientations. •We used the single-ion anisotropy model for the calculation of the surface anisotropy in yttrium iron garnet (YIG) films.•We took into account such crystalline defects as Fe3+ vacancies and non-magnetic substitutes.•We took into account the ultrathin surface layer that originates from the YIG structure.•The three different film orientations (001), (111) and (110) were studied.•The absolute values of the surface anisotropies were found to be below 10−2erg/cm2.
ISSN:0304-8853
DOI:10.1016/j.jmmm.2013.03.020