Jd. Frantz et Bo. Mysen, RAMAN-SPECTRA AND STRUCTURE OF BAO-SIO2, SRO-SIO2 AND CAO-SIO2 MELTS TO 1600-DEGREES-C, Chemical geology, 121(1-4), 1995, pp. 155-176
Raman spectra were collected for barium silicate, strontium silicate a
nd calcium silicate melts at temperatures ranging from the glass trans
ition region to temperatures as high as 1600 degrees C. For melts less
polymerized than disilicate, the spectra were used to determine the r
elative abundances of the Q(3), Q(2) and Q(1) tetrahedra and the Si2O5
2-,SiO32- and Si2O76- structural units in the melts. A concentration c
onstant was computed for the reaction: 4SiO(3)(2-) reversible arrow Si
2O52- + Si2O76- and was found to vary with composition from approximat
ely log(10) K-c = 0.5 for barium silicate melts with NBO/Si = 1.143 to
log(10) K-c = -1.75 for calcium metasilicate melts with NBO/Si = 2. L
ittle difference was found to exist in the structural behavior of the
melts on the three alkaline-earth silicate binary joins. Activity coef
ficients were computed for the SiO32- structural unit as a function of
bulk composition. The logarithm of the activity coefficients and mole
fraction of the structural unit are linearly correlated.