A. Grzechnik et Pf. Mcmillan, TEMPERATURE-DEPENDENCE OF THE OH- ABSORPTION IN SIO2 GLASS AND MELT TO 1975K, The American mineralogist, 83(3-4), 1998, pp. 331-338
FTIR absorbance spectra of SiO2 glass containing 1200 ppm OH- groups w
ere recorded in situ to 1975 K. There are only minor changes in peak h
eight to 1700 K, indicating that the molar extinction coefficient meas
ured at ambient conditions, at the peak maximum, is applicable for OH-
determination at high temperature. However the integrated peak intens
ity shows a slight decrease with increasing temperature over the entir
e temperature range, due to changes in the band shape associated with
small modifications to the hydrogen bonding environment and loss of hy
drous component at the highest temperatures.