Details
| Original language | English |
|---|---|
| Pages (from-to) | 45-61 |
| Number of pages | 17 |
| Journal | Phase transitions |
| Volume | 76 |
| Issue number | 1-2 |
| Publication status | Published - 1 Jan 2003 |
Abstract
It is well established that near-infrared (NIR) combination bands at 4500 and 5200cm-1 can be used to measure the concentrations of OH groups and H2O molecules, respectively, in hydrous silicate glasses at room temperature. However, the variations of hydrous species concentrations and molar absorption coefficients for the combination bands with temperature in the glass and in the melt have been controversial in the past decade. Three different approaches are used to determine hydrous species at elevated temperatures: (i) long term isothermal heating nearby the glass transition terminated by a rapid quench, (ii) controlled cooling after heating the melt above the liquidus and (iii) in situ measurements. Each of these techniques has its advantage and disadvantage. In the case of highly polymerized alkali aluminosilicates, consistent data are obtained by the different approaches. Fictive temperatures of glasses, calculated on the basis of relaxation theory, are close to the equilibrium temperatures for the H2O speciation determined by in situ measurements. This indicates that the relaxation of hydrous species is coupled to relaxation of the silicate network.
Keywords
- HO speciation, In situ measurements, IR spectroscopy, Silicate glass and melt
ASJC Scopus subject areas
- Physics and Astronomy(all)
- Instrumentation
- Materials Science(all)
- General Materials Science
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In: Phase transitions, Vol. 76, No. 1-2, 01.01.2003, p. 45-61.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Quantification of H2O speciation in silicate glasses and melts by IR spectroscopy - In situ versus quench techniques
AU - Behrens, H.
AU - Nowak, M.
PY - 2003/1/1
Y1 - 2003/1/1
N2 - It is well established that near-infrared (NIR) combination bands at 4500 and 5200cm-1 can be used to measure the concentrations of OH groups and H2O molecules, respectively, in hydrous silicate glasses at room temperature. However, the variations of hydrous species concentrations and molar absorption coefficients for the combination bands with temperature in the glass and in the melt have been controversial in the past decade. Three different approaches are used to determine hydrous species at elevated temperatures: (i) long term isothermal heating nearby the glass transition terminated by a rapid quench, (ii) controlled cooling after heating the melt above the liquidus and (iii) in situ measurements. Each of these techniques has its advantage and disadvantage. In the case of highly polymerized alkali aluminosilicates, consistent data are obtained by the different approaches. Fictive temperatures of glasses, calculated on the basis of relaxation theory, are close to the equilibrium temperatures for the H2O speciation determined by in situ measurements. This indicates that the relaxation of hydrous species is coupled to relaxation of the silicate network.
AB - It is well established that near-infrared (NIR) combination bands at 4500 and 5200cm-1 can be used to measure the concentrations of OH groups and H2O molecules, respectively, in hydrous silicate glasses at room temperature. However, the variations of hydrous species concentrations and molar absorption coefficients for the combination bands with temperature in the glass and in the melt have been controversial in the past decade. Three different approaches are used to determine hydrous species at elevated temperatures: (i) long term isothermal heating nearby the glass transition terminated by a rapid quench, (ii) controlled cooling after heating the melt above the liquidus and (iii) in situ measurements. Each of these techniques has its advantage and disadvantage. In the case of highly polymerized alkali aluminosilicates, consistent data are obtained by the different approaches. Fictive temperatures of glasses, calculated on the basis of relaxation theory, are close to the equilibrium temperatures for the H2O speciation determined by in situ measurements. This indicates that the relaxation of hydrous species is coupled to relaxation of the silicate network.
KW - HO speciation
KW - In situ measurements
KW - IR spectroscopy
KW - Silicate glass and melt
UR - http://www.scopus.com/inward/record.url?scp=0346827887&partnerID=8YFLogxK
U2 - 10.1080/0141159031000076048
DO - 10.1080/0141159031000076048
M3 - Article
AN - SCOPUS:0346827887
VL - 76
SP - 45
EP - 61
JO - Phase transitions
JF - Phase transitions
SN - 0141-1594
IS - 1-2
ER -