The solution behavior of H2O in peralkaline aluminosilicate melts at high pressure with implications for properties of hydrous melts

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Solubility and solution mechanisms of H2O in depolymerized melts in the system Na2O Al2O3 SiO2 were deduced from spectroscopic data of glasses quenched from melts at 1100 °C at 0.8 2.0 GPa. Data were obtained along a join with fixed nominal NBO/T = 0.5 of the anhydrous materials [Na2Si4O9 Na2(NaAl)4O9] with Al/(Al+Si) = 0.00 0.25. The H2O solubility was fitted to the expression, XO=0.20+0.0020fO-0.7X+0.9(X), where XO is the mole fraction of H2O (calculated with O = 1), fO the fugacity of H2O, and XAl = Al/(Al+Si). Partial molar volume of H2O in the melts, VHOmelt¯, calculated from the H2O-solulbility data assuming ideal mixing of melt H2O solutions, is 12.5 cm3/mol for Al-free melts and decreases linearly to 8.9 cm3/mol for melts with Al/(Al+Si) ˜ 0.25. However, if recent suggestion that VHOmelt¯ is composition-independent is applied to constrain activity composition relations of the hydrous melts, the activity coefficient of H2O, γHOmelt, increases with Al/(Al+Si). Solution mechanisms of H2O were obtained by combining Raman and 29Si NMR spectroscopic data. Degree of melt depolymerization, NBO/T, increases with H2O content. The rate of NBO/T-change with H2O is negatively correlated with H2O and positively correlated with Al/(Al+Si). The main depolymerization reaction involves breakage of oxygen bridges in Q4-species to form Q2 species. Steric hindrance appears to restrict bonding of H+ with nonbridging oxygen in Q3 species. The presence of Al3+ does not affect the water solution mechanisms significantly.

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