Abstract:The homogeneous and stoichiometric crystallization of the barium disilicate (BaSi2O5) glass makes it possible to follow the structural evolution of Raman bands from the supercooled liquid to the crystalline phase. We monitored the crystallization of supercooled liquid BaSi2O5 at 790°C over 440 minutes revealing a three‐stage crystallization process: stage 1 involves changes in the barium sites toward a bonding environment that is similar to that in orthorhombic low barium disilicate. The end of stage 1 is mark… Show more
“…Assuming that the vibrational modes in the crystalline phase have similar origins to those in the glass (c.f. Brawer and White 1975), as has been demonstrated in the case of BaSi O 5 (Moulton et al 2018), we offer several critical comments. First, the spectra of barium silicates show that the intense stretching modes may originate from the bonds between Si and either BO or NBO atoms, or both.…”
Section: Discussionmentioning
confidence: 74%
“…We conclude by emphasizing some of the implications for the interpretation of Raman spectra of silicate liquids and glasses (e.g. Moulton et al 2018), where hetero-connectivity is the rule rather than the exception.…”
Barium silicates may be found in contact aureoles and are used in several important technologies (e.g. LEDs). The BaO-SiO 2 system stabilizes 13 crystalline phases with different silicate tetrahedral and connectivity profiles. Aside from phases composed of a single structural unit (isolated or homo-connected tetrahedra) one encounters the relatively rare case of heteroconnected tetrahedra in which varying proportions of several Q n species are linked together. Here, we analyze the 29 Si MAS NMR and Raman spectroscopic manifestations of the connectivities in seven barium silicates: Ba 2 SiO 4 , high-BaSiO 3 , Ba 4 Si 6 O 16 , Ba 5 Si 8 O 21 , Ba 6 Si 10 O 26 , high-BaSi 2 O 5 and sanbornite (low-BaSi 2 O 5 ). The structures and purity of these phases were confirmed by Rietveld refinement. From the Raman spectroscopic database on 144predominantly homo-connected crystalline silicates, the mean Q n mode frequencies (ν Qn ± 1σ) are found at 827.7 (±13.8) cm -1 for Q 0 , 905.3 (±22.1) cm -1 for Q 1 , 993.5 (±25.9) cm -1 for Q 2 , and 1068.4 (±17.6) cm -1 for Q 3 units. Experimentally, homo-connected barium silicates show good agreement with these values whereas the hetero-connected phases show a wider range of ν Q2 than of ν Q3 frequencies. While the 29 Si NMR chemical shifts of the barium silicates are in agreement with known structural trends, those measured for the Q 2 resonances remain essentially constant, which may be caused by the lattice distortion around the large Ba 2+ cations. To complement and rationalize experimental measurements, first-principles calculations, at the This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America.The published version is subject to change. Cite as Authors (Year) Title. American Mineralogist, in press.
“…Assuming that the vibrational modes in the crystalline phase have similar origins to those in the glass (c.f. Brawer and White 1975), as has been demonstrated in the case of BaSi O 5 (Moulton et al 2018), we offer several critical comments. First, the spectra of barium silicates show that the intense stretching modes may originate from the bonds between Si and either BO or NBO atoms, or both.…”
Section: Discussionmentioning
confidence: 74%
“…We conclude by emphasizing some of the implications for the interpretation of Raman spectra of silicate liquids and glasses (e.g. Moulton et al 2018), where hetero-connectivity is the rule rather than the exception.…”
Barium silicates may be found in contact aureoles and are used in several important technologies (e.g. LEDs). The BaO-SiO 2 system stabilizes 13 crystalline phases with different silicate tetrahedral and connectivity profiles. Aside from phases composed of a single structural unit (isolated or homo-connected tetrahedra) one encounters the relatively rare case of heteroconnected tetrahedra in which varying proportions of several Q n species are linked together. Here, we analyze the 29 Si MAS NMR and Raman spectroscopic manifestations of the connectivities in seven barium silicates: Ba 2 SiO 4 , high-BaSiO 3 , Ba 4 Si 6 O 16 , Ba 5 Si 8 O 21 , Ba 6 Si 10 O 26 , high-BaSi 2 O 5 and sanbornite (low-BaSi 2 O 5 ). The structures and purity of these phases were confirmed by Rietveld refinement. From the Raman spectroscopic database on 144predominantly homo-connected crystalline silicates, the mean Q n mode frequencies (ν Qn ± 1σ) are found at 827.7 (±13.8) cm -1 for Q 0 , 905.3 (±22.1) cm -1 for Q 1 , 993.5 (±25.9) cm -1 for Q 2 , and 1068.4 (±17.6) cm -1 for Q 3 units. Experimentally, homo-connected barium silicates show good agreement with these values whereas the hetero-connected phases show a wider range of ν Q2 than of ν Q3 frequencies. While the 29 Si NMR chemical shifts of the barium silicates are in agreement with known structural trends, those measured for the Q 2 resonances remain essentially constant, which may be caused by the lattice distortion around the large Ba 2+ cations. To complement and rationalize experimental measurements, first-principles calculations, at the This is the peer-reviewed, final accepted version for American Mineralogist, published by the Mineralogical Society of America.The published version is subject to change. Cite as Authors (Year) Title. American Mineralogist, in press.
“…When doped with rare-earth elements, these materials can be used as light emitting diode materials [23,24]. Although interesting behaviors have been shown, there is a lack of clarity regarding the origin and significance of the vibrational modes and their transitions during crystallization processes [21,[25][26][27][28].…”
Section: Introductionmentioning
confidence: 99%
“…In such cases it is impossible to make an unambiguous assignment if the calculated intensities are so model-dependent that they cannot be used as an aid. Quantum-chemical computations predicting frequencies and spectral intensities are essential to complement the interpretation of experimental spectra, particularly for complex materials where the high density of states results in spectral complexity [26].…”
We report here the analysis of vibrational properties of the sanbornite (low-BaSi2O5) and Ba5Si8O21 using theoretical and experimental approaches, as well as results of high temperature experiments up to 1100-1150˚C. The crystal parameters derived from Rietveld refinement and calculations show excellent agreement, within 4%, while the absolute mean difference between the theoretical and experimental results for the IR and Raman vibrational frequencies was <6 cm-1. The temperature-dependent Raman study renders that both sanbornite and Ba5Si8O21 display specific Ba and Si sites and their Ba-O and Si-O bonds. In the case of the stretching modes assigned to specific Si sites, the frequency dependence on the Si-O bond length exhibited very strong correlations. Both phases showed that for a change of 0.01 Å, the vibrational mode shifted 10 ± 2 cm-1. These results are promising for using Raman spectroscopy to track in situ reactions under a wide variety of conditions, especially during crystallization.
“…The MBE and TE samples, as well as some of the RF-sputter deposited samples, show the presence of two additional but low intensity peaks at ∼560 cm −1 and ∼580 cm −1 that could stem from Ba-Si-O phases such as Ba 3 Si 5 O 13 , Ba 2 Si 3 O 8 , or BaO-SiO 2 15,16 that can also be discerned in some of the collected XRD patterns. The Raman spectra of the TE sample show two additional peaks at around 260 cm −1 and 315 cm −1 that may arise from BaO-SiO 2 and/or Ba 2 Si 3 O 8 15,16 indicating a higher degree of oxidation than the MBE sample. In turn, RF-sputter deposited samples reveal the presence of a sharp 250 cm −1 peak that diminishes with increased thickness of the a-Si cap layer and that can be attributed to the presence of oxides in the sub-surface layer, namely, BaO (242 cm −1 ), 17 SiO 2 (245 cm −1 ), 18 and/or BaSiO 3 (247 cm −1 ).…”
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