Abstract
We present a systematic x-ray magnetic-circular-dichroism (XMCD) study performed at the Fe $K$ edge on the ${R}_{2}{\mathrm{Fe}}_{14}\mathrm{B}$ series ($R=\mathrm{rare}\mathrm{earth}\mathrm{and}\mathrm{Y}$). The magnetic XMCD signal has been identified as due to the addition of two components associated with the magnetic contributions from the iron and the rare-earth sublattices. The contribution of the rare-earth sublattice has been extracted from the total XMCD signal. The integrated XMCD signal of the $R$ component is proven to be directly correlated with the $R$ magnetic moment.
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