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Ellison & Hess 1990
Ellison, A.J.G. and Hess, P.C. (1990). Lanthanides in silicate glasses: A vibrational spectroscopic study. Journal of Geophysical Research 95: doi: 10.1029/90JB00442. issn: 0148-0227.

Parallel- and perpendicular-Polarized Raman and KBr pellet transmission IR spectra of quenched 10K2O-50SiO2-nR2O3 (R=La, Gd, Yb; N=0, 1, 5, 10 mol) glasses are presented. Increasing lanthanide oxide concentration produces partially-polarized high frequency bands at 1030, 940, and 860 cm-1, assigned to the symmetric stretching modes of SiO4 tetrahedra containing 1, 2, and 4 nonbridging oxygen, respectively, in which the nonbridging oxygen coordinate primarily with lanthanides. Lanthanides therefore form silicate anions that are depolymerized relative to the bulk liquid and which have no counterparts in R2O3-SiO2 binary systems. The spectra indicate that there is little sharing of nonbridging oxygen by K and lanthanides. The spectra of glasses contianing different lanthanides at the same concentration are qualitatively and quantitatively very similar. Lathanides have energetically unfavorable interactions with the network structure of polymerized liquids compared to cations of lower valence. If lanthanides coordinate nonbridging oxygen without the aide of K, then lanthanide saturation concentrations will show modes increases with increasing (Na,K)/Al in peralkaline liquids, except in liquids in which P2O5 concentration is comparable to the total lanthanide concentration. Since differences in lanthanide ionic radii have small effects upon the spectra, lanthanide solution mechanisms in silicate glasses (and by inference siliate liquids) are probably very similar. ¿American Geophysical Union 1990

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Abstract

Keywords
Mineralogy and Petrology, Minor and trace element composition, Mineral Physics, X ray, neutron, and electron spectroscopy and diffraction
Journal
Journal of Geophysical Research
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American Geophysical Union
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