Abstract
Abstract We present a systematic X-ray Magnetic Circular Dichroism (XMCD) study performed at the Fe K-edge of the RFe 11 Ti intermetallic materials. We have investigated the contribution of the rare-earth sublattice to the dichroism of the transition metal. The existence of a magnetic contribution of the rare-earth has been identified and isolated from the whole spectrum. This contribution is found to be related to the rare-earth moment even when one is looking at the Fe K-edge absorption.
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