SILICATE MELTS AT MAGMATIC TEMPERATURES - IN-SITU STRUCTURE DETERMINATION TO 1651-DEGREES-C AND EFFECT OF TEMPERATURE AND BULK COMPOSITION ON THE MIXING BEHAVIOR OF STRUCTURAL UNITS
Bo. Mysen et Jd. Frantz, SILICATE MELTS AT MAGMATIC TEMPERATURES - IN-SITU STRUCTURE DETERMINATION TO 1651-DEGREES-C AND EFFECT OF TEMPERATURE AND BULK COMPOSITION ON THE MIXING BEHAVIOR OF STRUCTURAL UNITS, Contributions to Mineralogy and Petrology, 117(1), 1994, pp. 1-14
The abundance of coexisting structural units in K-, Na-, and Li-silica
te melts and glasses from 25-degrees to 1651-degrees-C has been determ
ined with in-situ micro-Raman spectroscopy. From these data an equilib
rium constant, K(x), for the disproportionation reaction among the str
uctural units coexisting in the melts, Si2O5(2Q3) double line arrow po
inting left and right SiO3(Q2) + SiO2(Q4), was calculated (K(x) is the
equilibrium constant derived by using mol fractions rather than activ
ities of the structural units). From ln K(x) vs 1/T relationships the
enthalpy (DELTAHx) for the disproportionation reaction is in the range
of -30 to 30 kJ/mol with systematic compositional dependence. In the
potassium and sodium systems, where the disproportionation reaction sh
ifts to the right with increasing temperature, the DELTAH(x) increases
with silica content (M/Si decreases, M = Na, K). For melts and superc
ooled liquids of composition Li2O . 2SiO2 (Li/Si = 1), the DELTAH(x) i
s indistinguishable from 0. By decreasing the Li/Si to 0.667 (composit
ion LS3) and beyond (e.g., LS4), the disproportionation reaction shift
s to the left as the temperature is increased. For a given ratio of M/
Si (M = K, Na, Li), there is a positive, near linear correlation betwe
en the DELTAH(x) and the Z/r2 of the metal cation. The slope of the DE
LTAH(x) vs Z/r2 regression lines increases as the system becomes more
silica rich (i.e., M/Si is decreased). Activity coefficients for the i
ndividual structural units, gamma(i), were calculated from the structu
ral data combined with liquidus phase relations. These coefficients ar
e linear functions of their mol fraction of the form lngamma(i) = a ln
X(i) + b, where a is between 0.6 and 0.87, and X(i) is the mol fractio
n of the unit. The value of the intercept, b, is near 0. The relations
hip between activity coefficients and abundance of individual structur
al units is not affected by temperature or the electronic properties o
f the alkali metal. The activity of the structural units, however, dep
end on their concentration, type of metal cation, and on temperature.