RAMAN-SPECTRA AND STRUCTURE OF BAO-SIO2, SRO-SIO2 AND CAO-SIO2 MELTS TO 1600-DEGREES-C

被引:203
作者
FRANTZ, JD [1 ]
MYSEN, BO [1 ]
机构
[1] WOODS HOLE OCEANOG INST,WOODS HOLE,MA 02543
基金
美国国家科学基金会;
关键词
D O I
10.1016/0009-2541(94)00127-T
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
Raman spectra were collected for barium silicate, strontium silicate and calcium silicate melts at temperatures ranging from the glass transition region to temperatures as high as 1600 degrees C. For melts less polymerized than disilicate, the spectra were used to determine the relative abundances of the Q(3), Q(2) and Q(1) tetrahedra and the Si2O52-,SiO32- and Si2O76- structural units in the melts. A concentration constant was computed for the reaction: 4SiO(3)(2-) reversible arrow Si2O52- + Si2O76- and was found to vary with composition from approximately 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. Little difference was found to exist in the structural behavior of the melts on the three alkaline-earth silicate binary joins. Activity coefficients 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.
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页码:155 / 176
页数:22
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