USE OF L-EDGE X-RAY-ABSORPTION SPECTROSCOPY TO CHARACTERIZE MULTIPLE VALENCE STATES OF 3D TRANSITION-METALS - A NEW PROBE FOR MINERALOGICALAND GEOCHEMICAL RESEARCH

2p (L2, 3) X-ray absorption spectra are presented for a range of miner als to demonstrate the usefulness of L-edge spectroscopy as a symmetry - and valence-selective probe. 2p XAS provides a sensitive fingerprint of the electronic states of 3d transition metals and can be applied t o phases containing mixtures of such elements. Calculated spectra for 3 d(n) --> 2p5 3 d(n+1) transitions provide a basis for the interpreta tion of the measured spectra. Thus, in principle, multiple valence sta tes of a particular 3 d metal can be precisely characterized from a si ngle L-edge spectrum. Examples of vanadium L-edge spectra are presente d for a range of minerals; these complex spectra hold information conc erning the presence of vanadium in multiple valence states. The Cu L-e dge spectrum of sulvanite (Cu3 VS4) indicates the presence of both Cu and Cu2+; the V L-edge spectrum of the same sample shows that both V2 + and V5+ are present. Spectral simulations representing mixtures of F e d5 and Fe d6 states are used to quantify Fe3+/SIGMAFe in s spinel, a glass, and an amphibole, all of which contain Fe as a major component . To illustrate the sensitivity of 2p XAS in a dilute system, the Fe L -edge spectrum of amethyst (alpha-SiO2 : Fe) has been recorded; this s pectrum shows that approximately 68% of the Fe in amethyst is Fe2+, an d approximately 32% is Fe3+. Although previous studies on amethyst usi ng other spectroscopic methods cite evidence for Fe4+, there is no ind ication in the L-edge spectrum for Fe4+ in amethyst. Comparison of the oretical and experimental spectra not only allows the valence states o f 3 d ions to be recognised, but also provides site-symmetry informati on and crystal field parameters for each ion site.