XMCD at Fe L2,3 edges, Fe and S K edges on Fe7S8

被引：0
作者：
Isabelle Letard
Philippe Sainctavit
Catherine Deudon
机构：
[1] ESRF,Institut de Minéralogie et de Physique des Milieux Condensés
[2] CNRS & UPMC,undefined
[3] Institut des Matériaux de Nantes,undefined
来源：
Physics and Chemistry of Minerals | 2007年 / 34卷
关键词：
Iron sulphide; XMCD; Pyrrhotite;
D O I：
暂无
中图分类号：
学科分类号：
摘要：
Pyrrhotite (Fe7S8) is a natural iron sulphide that can participate in rock magnetisation. Its electronic structure is not yet surely described. X-ray magnetic circular dichroism (XMCD) at Fe L2,3 edges on Fe7S8, coupled with multiplet calculations, shows that iron is present only as Fe2+ in this magnetic iron sulphide. It reveals a strong magnetic orbital moment. XMCD at Fe and S K edges shows the quite strong polarization of both Fe and S in Fe7S8.
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页码：113 / 120
页数：7
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