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Title: On the Site-Decomposition of Magnetocrystalline Anisotropy Energy Using Ome-Electron Eigenstates

Abstract

We discuss two di erent schemes for decomposing the magnetocrystalline anisotropy energy into atomic site-speci c contributions, and show that one of these, which uses projected single-particle states, is inherently ill-de ned in practical applications. We therefore argue that the other decomposition scheme, involving ground state matrix elements of the spin-orbit operator, is preferable for the numerical prediction of one-site contributions to the anisotropy.

Authors:
 [1];  [1];  [1]
  1. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Publication Date:
Research Org.:
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1239183
Report Number(s):
LLNL-TR-678619
DOE Contract Number:  
AC52-07NA27344
Resource Type:
Technical Report
Country of Publication:
United States
Language:
English
Subject:
75 CONDENSED MATTER PHYSICS, SUPERCONDUCTIVITY AND SUPERFLUIDITY

Citation Formats

Aberg, Daniel, Sadigh, Babak, and Benedict, Lorin X. On the Site-Decomposition of Magnetocrystalline Anisotropy Energy Using Ome-Electron Eigenstates. United States: N. p., 2015. Web. doi:10.2172/1239183.
Aberg, Daniel, Sadigh, Babak, & Benedict, Lorin X. On the Site-Decomposition of Magnetocrystalline Anisotropy Energy Using Ome-Electron Eigenstates. United States. https://doi.org/10.2172/1239183
Aberg, Daniel, Sadigh, Babak, and Benedict, Lorin X. 2015. "On the Site-Decomposition of Magnetocrystalline Anisotropy Energy Using Ome-Electron Eigenstates". United States. https://doi.org/10.2172/1239183. https://www.osti.gov/servlets/purl/1239183.
@article{osti_1239183,
title = {On the Site-Decomposition of Magnetocrystalline Anisotropy Energy Using Ome-Electron Eigenstates},
author = {Aberg, Daniel and Sadigh, Babak and Benedict, Lorin X.},
abstractNote = {We discuss two di erent schemes for decomposing the magnetocrystalline anisotropy energy into atomic site-speci c contributions, and show that one of these, which uses projected single-particle states, is inherently ill-de ned in practical applications. We therefore argue that the other decomposition scheme, involving ground state matrix elements of the spin-orbit operator, is preferable for the numerical prediction of one-site contributions to the anisotropy.},
doi = {10.2172/1239183},
url = {https://www.osti.gov/biblio/1239183}, journal = {},
number = ,
volume = ,
place = {United States},
year = {Mon Oct 26 00:00:00 EDT 2015},
month = {Mon Oct 26 00:00:00 EDT 2015}
}