Bonding in silicates: Investigation of the Si L2,3 edge by parallel electron energy-loss spectroscopy

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Abstract

The Si L2,3 core-loss edge can be used to probe the crystal chemistry around Si, providing information on the s- and d-like partial density of unoccupied states of the Si-O bonds. We present Si L2,3 edges from 59 silicates, glasses, and amorphous materials acquired by parallel electron energy-loss spectroscopy (PEELS) with a transmission electron microscope (TEM) at an energy resolution of 0.7 eV. The Si L2,3 edge spectrum of α-quartz is interpreted using the results of a recent pseudopotential band-structure calculation. A combination of Si s- and d-like partial density of states derived from this calculation resembles the Si L2,3 energy-loss near-edge structure (ELNES) of α-quartz. The Si L2,3 ELNES of the silicates are interpreted using the results of the band-structure calculation of α-quartz. The Si L2,3 edges of Q4, Q3, Q2, some Q1 silicates, and amorphous materials have ELNES similar to that of α-quartz, and the Q0 and some Q1 silicates have ELNES different from that of α-quartz. A 'coordination fingerprint' is defined for Q4, Q3, and Q2 Si L2,3 ELNES because of their similarity to the α-quartz spectrum. The similarities between the L2,3 core-less edge shapes of the third-row XO4(n-) (X = Al, Si, S, and P) series attests to a common molecular-orbital picture of their bonding. For Q0 and some Q1 spectra a 'structure fingerprint' is defined because the Si L2,3-edge shapes are indicative of the number, distribution, and nature of the non-nearest-neighbor atoms. Spectra of olivine glasses and metamict zircon more closely resemble the α-quartz spectrum than their crystalline analogs. In contrast to previous studies, we show that distortion of the SiO4 tetrahedron is of secondary importance as an ELNES-modifying parameter. Polyhedral distortions become less important with increase in polymerization. There is a positive linear correlation between the energies of the Si L2,3-edge onsets and polymerization, Si 2p and 2s binding energies, and the 29Si NMR isotropic chemical shifts. The shift to higher energies of the edge onsets with polymerization corresponds to an increase in effective charge on the Si atom with higher Q(n). For silicates with isolated SiO4 tetrahedra, increases in L2,3-energy onsets correlate with increases in polarizing power of the next-nearest-neighbor cations. The Si L2,3-edge shapes are affected by the types and coordinations of the next-nearest-neighbor cations. For example, andradite, ilvaite, fayalite, and γ-Fe2SiO4 have FeO6 bonded to SiO4 and exhibit similar ELNES. Topaz, dumortierite, staurolite, and kyanite have similar Si L2,3 ELNES, with AlO(6a) bonded to the SiO4. Their edge shapes are distinct from those of silicates with SiO4 bonded to AlO4, as in the feldspars. A comparison of the Al and Si L2,3 and Al, Si, O, and F K core-loss edges of topaz illustrates the influence of neighbor effects and mixing of unoccupied states. This mixing illustrates the limitations of ab initio methods that model core-loss edges that neglect non-nearest-neighbor interactions.

Original languageEnglish (US)
Pages (from-to)946-964
Number of pages19
JournalAmerican Mineralogist
Volume84
Issue number5-6
DOIs
StatePublished - 1999

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology

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