Solid-state NMR and XANES studies of lithium and silver silicate gels synthesized by the sol–gel route
The objective of this study is to understand the effect of low temperature sol–gel synthesis on the microstructural properties of lithium [ xLi 2O–(1− x)SiO 2; x=0.1–0.8 in steps of 0.1] and silver [ xAg 2O–(1− x)SiO 2; x=0.1–0.8 in steps of 0.1] silicate xerogels via solid state nuclear magnetic re...
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Veröffentlicht in: | Journal of non-crystalline solids 2003-04, Vol.318 (3), p.296-304 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The objective of this study is to understand the effect of low temperature sol–gel synthesis on the microstructural properties of lithium [
xLi
2O–(1−
x)SiO
2;
x=0.1–0.8 in steps of 0.1] and silver [
xAg
2O–(1−
x)SiO
2;
x=0.1–0.8 in steps of 0.1] silicate xerogels via solid state nuclear magnetic resonance (NMR) and X-ray absorption near edge structure (XANES) techniques. The Li silicate xerogels were analyzed with solid-state
7Li and
29Si NMR and the Ag silicate xerogels were studied with Ag XANES. At high Li loading,
7Li NMR shows quadrupolar satellite transitions attributed to LiNO
3, a phase also found with X-ray diffraction (XRD). At low Li loading, both NMR and XRD results show an amorphous xerogel. The silicate network is monitored with
29Si NMR and shows evidence of Li incorporation. For the Ag silicate xerogels, Ag–L-III XANES spectral studies show a local environment similar to AgNO
3 for low Ag loading levels, and an increased Ag oxidation for higher Ag loading levels. Si K edge spectra show only an amorphous phase, with no evidence of a crystalline quartz phase. The electrical conductivity of the lithium silicates was estimated from impedance data and the highest conductivity is exhibited by the 0.3Li
2O–0.7SiO
2 composition xerogel. The conductivity dependence on loading level strongly suggests that the observed conductivity is due to Li
+ mobility. However, further experimental studies are needed to rule out the possibility that the conductivity is, at least in part, due to H
+ mobility. Variation in conductivity is explained qualitatively using existing theoretical models. |
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ISSN: | 0022-3093 1873-4812 |
DOI: | 10.1016/S0022-3093(02)01890-2 |