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Titel Iron M-edge x-ray Raman scattering spectroscopy - a tool to determine Fe speciation at conditions of deep Earth
VerfasserIn Alexander Nyrow, Christian Sternemann, Max Wilke, Kolja Mende, Thomas Büning, Robert A. Gordon, Hasan Yavas, Laura Simonelli, Nozumo Hiraoka, Serge Desgreniers, Christoph J. Sahle, Simo Huotari, Giovanni B. Andreozzi, Alan B. Woodland, Metin Tolan, John S. Tse
Konferenz EGU General Assembly 2014
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 16 (2014)
Datensatznummer 250100595
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2014-16578.pdf
 
Zusammenfassung
We present a spectroscopic study of the iron M2,3-edge for several minerals and compounds to reveal information about the oxidation state, local coordination and spin state of iron. We describe a novel approach to probe the iron M-edge bulk sensitively using non-resonant inelastic x-ray scattering. Significant changes in the onset and shape of the Fe M-edge were observed demonstrating the capabilities of x-ray Raman scattering spectroscopy to extract information on the Fe3+/Fetot ratio and local coordination. In-situ measurements of the pressure-induced spin transition in FeS even demonstrate that this technique allows for detection of the spin cross-over as well as characterization of the electronic properties of the low-spin phase. Thus, x-ray Raman spectroscopy is suitable for obtaining detailed insights to the properties of Fe in-situ at high pressure and temperature providing indispensable information for many physical and chemical processes of the deep Earth.