Factors affecting line shapes and intensities of Q3 and Q4 Raman bands of Cs silicate glasses

被引:28
作者
Nesbitt, H. Wayne [1 ]
O'Shaughnessy, Cedrick [2 ]
Henderson, Grant S. [2 ]
Bancroft, G. Michael [3 ]
Neuville, Daniel R. [4 ]
机构
[1] Univ Western Ontario, Dept Earth Sci, London, ON, Canada
[2] Univ Toronto, Dept Earth Sci, Toronto, ON, Canada
[3] Univ Western Ontario, Dept Chem, London, ON, Canada
[4] CNRS IPGP, Geomateriaux, 1 Rue Jussieu, F-75005 Paris, France
关键词
Raman spectra of Cs-silicate glasses; Q species abundances; Raman line shapes; Raman Linewidths; Lorentzian line shapes; PHOTOELECTRON-SPECTROSCOPY XPS; DOUBLE-QUANTUM NMR; BRIDGING OXYGEN; K2O-SIO2; GLASSES; MELTS; SPECTRA; TEMPERATURE; SPECIATION; SODIUM; SI;
D O I
10.1016/j.chemgeo.2018.12.009
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Raman spectra of glasses containing 0 to 30 mol% Cs2O have been fit successfully with line shapes of dominantly Lorentzian character for the Q(3) species, allowing quantification of Q(3) and Q(4) species intensities (Q represents a Si tetrahedron and the superscript indicates the number of bridging oxygen atoms, BOs, bonded to Si.) The intensity of the Q(4) species A(1) symmetric stretch is exceptionally weak in vitreous silica (v-SiO2) but it increases dramatically with addition of small amounts of Cs2O to the glass. We propose that Cs, where in close proximity to BO of Q(4) species, promotes the polarizability of Q(4) tetrahedra and these primed Q(4) species (Q(4)-p) produce a strong Q(4) signal. There are, therefore, two variants of the Q(4) species, a Q(4)-p species which produces a strong signal, and an unprimed species (Q(4)-u) which yields a very weak signal. The increase in the abundance of the primed Q(4) species (Q(4)-p) can be modelled as a function of alkali content using a simple, upper-bounded growth model: XQ4-p = (1 - e(-kx)) where XQ4-p is the fraction of polarizable Q(4) species, k is a constant and x is the mol% counter oxide in the glass (here Cs2O). Comparison of calculated XQ(4-p) values with experimental results indicates that its cross-section is similar to that of the Q(3) species. There is no evidence for a similar to 1050 cm(-1) band in the 5 mol% Cs2O glass spectrum but in the 30 mol% Cs2O glass spectrum about 11% of spectral intensity is observed at about this frequency. The intensity likely results from development of asymmetry on the Q(3) band, which increases with Cs2O content of the glass. The asymmetry results from weakened Si-O force constants of some Q(3) tetrahedra due to charge transfer via Cs-BO bonds. As evidence, Si 2p and O 1s X-ray Photoelectron Spectroscopic (XPS) studies demonstrate that the electron density over Si and BO atoms of Q(4) species increases with Cs2O content. With charge transfer to tetrahedra, the negative charge accumulates preferentially on Si atoms thus decreasing Si-O coulombic interactions, weakening Si-O force constants, and shifting the Q(3) A(1) symmetric stretch vibrational frequencies to lower values (e.g., from similar to 1100 cm(-1) to similar to 1050 cm(-1)). The fraction of affected Q(3) species increases with alkali content, as does the Q(3) peak asymmetry. The Raman shifts of the Q(4) species are also affected by increased Cs2O contents.
引用
收藏
页码:1 / 11
页数:11
相关论文
共 59 条
[1]   Lorentzian dominated lineshapes and linewidths for Raman symmetric stretch peaks (800-1200 cm-1) in Qn (n=1-3) species of alkali silicate glasses/melts [J].
Bancroft, G. Michael ;
Nesbitt, H. Wayne ;
Henderson, Grant S. ;
O'Shaughnessy, Cedrick ;
Withers, Anthony C. ;
Neuville, Daniel R. .
JOURNAL OF NON-CRYSTALLINE SOLIDS, 2018, 484 :72-83
[2]   RAMAN SPECTROSCOPIC INVESTIGATION OF STRUCTURE OF SILICATE-GLASSES .1. BINARY ALKALI SILICATES [J].
BRAWER, SA ;
WHITE, WB .
JOURNAL OF CHEMICAL PHYSICS, 1975, 63 (06) :2421-2432
[3]  
Briggs D., 1990, PRACTICAL SURFACE AN, V1
[4]   STRUCTURE OF GLASSES IN THE SYSTEMS MG2SIO4-FE2SIO4, MN2SIO4-FE2SIO4, MG2SIO4-CAMGSIO4, AND MN2SIO4-CAMNSIO4 [J].
COONEY, TF ;
SHARMA, SK .
JOURNAL OF NON-CRYSTALLINE SOLIDS, 1990, 122 (01) :10-32
[5]   Resolution of bridging oxygen signals from O 1s spectra of silicate glasses using XPS: Implications for O and Si speciation [J].
Dalby, Kim N. ;
Nesbitt, H. Wayne ;
Zakaznova-Herzog, Valentina P. ;
King, Penelope L. .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2007, 71 (17) :4297-4313
[6]   The medium range structure of sodium silicate glasses: a molecular dynamics simulation [J].
Du, J ;
Cormack, AN .
JOURNAL OF NON-CRYSTALLINE SOLIDS, 2004, 349 :66-79
[7]   Compositional dependence of the first sharp diffraction peaks in alkali silicate glasses: A molecular dynamics study [J].
Du, Jincheng ;
Corrales, L. Rene .
JOURNAL OF NON-CRYSTALLINE SOLIDS, 2006, 352 (30-31) :3255-3269
[8]   RAMAN-SPECTRA AND STRUCTURE OF BAO-SIO2, SRO-SIO2 AND CAO-SIO2 MELTS TO 1600-DEGREES-C [J].
FRANTZ, JD ;
MYSEN, BO .
CHEMICAL GEOLOGY, 1995, 121 (1-4) :155-176
[9]   RAMAN-SPECTROSCOPIC INVESTIGATION OF THE STRUCTURE OF SILICATE-GLASSES .3. RAMAN INTENSITIES AND STRUCTURAL UNITS IN SODIUM-SILICATE GLASSES [J].
FURUKAWA, T ;
FOX, KE ;
WHITE, WB .
JOURNAL OF CHEMICAL PHYSICS, 1981, 75 (07) :3226-3237
[10]   Novel opportunities for studying the short and medium range order of glasses by MAS NMR, 29Si double quantum NMR and IR spectroscopies [J].
Glock, K ;
Hirsch, O ;
Rehak, P ;
Thomas, B ;
Jager, C .
JOURNAL OF NON-CRYSTALLINE SOLIDS, 1998, 232 :113-118