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Raman Spectroscopy of nanomaterials - institut de chimie et des ...

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ARTICLE IN PRESS+ MODELG. Goua<strong>de</strong>c, Ph. Colomban / Progress in Crystal Growth and Characterization <strong>of</strong> Materials 23xx (2007) 1e56obvious from the figure that the GeO 4 t<strong>et</strong>rahedra as well as GeO 6 octahedra are more distortedin the mesoporous glass than in the gel phase [298]. In the example <strong>of</strong> the perovskite-relatedniobiates from Fig. 10b, the NbeO mo<strong>de</strong>s around 800 cm 1 are split because <strong>of</strong> the occasionalpresence <strong>of</strong> oxygen vacancies in the NbO 6 octahedra. The (T 0 ,R 0 ) mo<strong>de</strong>s involving the Baatoms located at the corners <strong>of</strong> the unit-cell are not modified by these vacancies in Ba 6 Nb 2 O 11(hence the fine peaks) but are split again in Ba 4 Ca 2 Nb 2 O 11 because chemical and mass <strong>de</strong>couplingisolate the Ba and Ca sub-lattices [299]. The same kind <strong>of</strong> vibrational <strong>de</strong>coupling due to<strong>de</strong>fects has been observed for many silicates [296,297,300].Two silicate spectra are shown in Fig. 11a and b. Most types <strong>of</strong> glass contain nanom<strong>et</strong>riccrystallites and the spectrum <strong>of</strong> silicates (SiO 2 t<strong>et</strong>rahedral n<strong>et</strong>work) is intermediate b<strong>et</strong>weenthat <strong>of</strong> a disor<strong>de</strong>red n<strong>et</strong>work and the superposition <strong>of</strong> contributions from <strong>de</strong>finite vibrational entities:t<strong>et</strong>rahedra rings in vitreous silica (the narrow <strong>de</strong>fect bands in Fig. 11a originate from thevibrations <strong>of</strong> threefold (D 2 ) and fourfold (D 1 ) rings [301e304]) and complex arrangements <strong>of</strong>SiO 4 t<strong>et</strong>rahedra in alkali/earth-alkali silicates [301]. The <strong>de</strong>formation (d SieOeSi w 500 cm 1 )and elongation (n SieO w 800e1200 cm 1 ) mo<strong>de</strong>s <strong>de</strong>pend on the connectivity <strong>of</strong> the SiO 4 t<strong>et</strong>rahedraand can be fitted with components called Q n and Q 0 n , respectively (n represents thenumber <strong>of</strong> SieOeSi bridges per t<strong>et</strong>rahedron) [305e307]. The position and area <strong>of</strong> these componentsthen constitute characteristic param<strong>et</strong>ers <strong>of</strong> silicate glass nanostructures and can beused for garnering additional information such as the original composition or the sintering temperature[305,306].The most specific part <strong>of</strong> glass spectra is a band peaking at w50 to 100 cm 1 , which iscalled the Boson Peak (BP) because its intensity obeys a BoseeEinstein distribution. Since(a)Bendingmo<strong>de</strong>sStr<strong>et</strong>chingmo<strong>de</strong>s(b)MolecularsignatureD 1*D 2Wavenumber / cm -1Intensity / a.u.**BosonPeakBosonPeak00 75 150 500 1000Fig. 11. (a) <strong>Raman</strong> spectrum <strong>of</strong> pure glassy silica (macro-configuration, l ¼ 406 nm; D 1 and D 2 : see text). (b) <strong>Raman</strong>spectrum <strong>of</strong> a highly <strong>de</strong>polymerised potassium-rich calcium silicate stained glass (macro-configuration, l ¼ 413 nm;stars indicate plasma lines from the laser).Please cite this article in press as: G. Goua<strong>de</strong>c, Ph. Colomban, Prog. Cryst. Growth Charact. Mater. (2007),doi:10.1016/j.pcrysgrow.2007.01.001

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