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Structure of spinel at high temperature using in-situ XANES study at the Al and Mg K-edge

D de Ligny et al 2009 J. Phys.: Conf. Ser. 190 012178 (4pp)   doi: 10.1088/1742-6596/190/1/012178  Help

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D de Ligny1, D R Neuville2, A-M Flank3 and P Lagarde3
1 Université Claude Bernard Lyon 1, LPCML, 69622 Villeurbanne, France
2 Physique des Minéraux et Magmas, Géochimie-Cosmochimie, CNRS-IPGP, 4 place Jussieu, 75005 Paris, France
3 Synchrotron SOLEIL, L'Orme des Merisiers, Saint Aubin, 91192 France
E-mail: deligny@pcml.univ-lyon1.fr

Abstract. We present structural information obtained on spinel at high temperature (298–2400 K) using in situ XANES at the Mg and Al K-edge. Spinel, [4](Alx,Mg1-x)[6](Al2-x,Mgx)O4, with increasing temperature, show a substitution of Mg by Al and Al by Mg in their respective sites. This substitution corresponds to an inversion of the Mg and Al sites. Furthermore, both experiments at the Al and Mg K-edges are in good agreement with XANES calculation made using FDMNES code.

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