Abstract
We present a x-ray magnetic circular dichroism (XMCD) study performed at the Fe K edge in R6Fe23 compounds exhibiting magnetic compensation (R=Ho and Y). The Fe K-edge XMCD signal has been identified as due to both Fe itself and rare-earth contributions. Following a simple two-sublattices model for the analysis of the dichroic signal the contribution of the rare-earth sublattice to total Fe K-edge XMCD signal has been extracted and proven to be directly correlated to the R magnetic moment.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
