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American Mineralogist; November 2006; v. 91; no. 11-12; p. 1794-1801; DOI: 10.2138/am.2006.2154
© 2006 Mineralogical Society of America
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Titanium incorporation and VITi3+ -IVTi4+ charge transfer in synthetic diopside

Henrik Skogby1,*, Ulf Hålenius1, Per Kristiansson2 and Haruo Ohashi3

1 Department of Mineralogy, Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden
2 Department of Nuclear Physics, Lund Institute of Technology, Lund University, Box 118, SE-221 00 Lund, Sweden
3 Hashi Institute for Silicate Science, Nishinakanobu 1-9-25, Shinagawa, Tokyo 142-0054, Japan

Correspondence: * E-mail: henrik.skogby{at}nrm.se

A series of Ti-doped diopside samples synthesized by fluxgrowth methods under reducing conditions were investigated by microanalytical methods and optical absorption spectroscopy, to assess Ti incorporation mechanisms, valence states, and related electronic transitions. Chemical characterization show that Ti occurs both in the tri-and tetravalent states, with Ti4+ preferentially ordered to the tetrahedral position whereas Ti3+ is restricted to the M1 position. Charge-balance is maintained by incorporation of Na and minor B, stemming from the flux compound. Polarized optical absorption spectra reveal three major absorption features. Two relatively narrow bands centered at 18 500 and 15 700 cmly polarized in the crystallographic c-direction, display absorbance values that correlate with the calculated Ti3+ (M1) concentration, and are assigned to spin-allowed d-d transitions in Ti3+. A broader band centered around 24 500 cm–1ys absorbance values that are well correlated with the product of VITi3+ and IVTi4+. Based on the spectral characteristics of this band, including a strong polarization in the crystallographic b-direction, we assign this band to an M1Ti3+-TTi4+ intervalence charge transfer process.

Key Words: Crystal synthesis • diopside • optical spectroscopy • pyroxene • major and minor elements • Ti in pyroxene • order-disorder







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