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American Mineralogist; November-December; v. 88; no. 11-12; p. 1668-1678
© 2003 Mineralogical Society of America
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The structural behavior of Al3+ in peralkaline melts and glasses in the system Na2O-Al2O3-SiO2

Bjorn O. Mysen1,*, Amie Lucier2 and George D. Cody1

1 Geophysical Laboratory, Carnegie Institution of Washington, Washington D.C., U.S.A.
2 University of California at Davis, Davis California, U.S.A.

Correspondence: * E-mail: mysen{at}gl.ciw.edu

The structural behavior of Al3+ in peralkaline glasses and melts along the Na2Si3O7-Na2(NaAl)3O7 join has been examined to 1200 °C at ambient pressure with 29Si MAS NMR and Raman spectroscopy. The distribution of Al3+ among coexisting Q4, Q3, and Q2 structural units in the glasses and melts was determined as a function of bulk Al/(Al + Si) and temperature. The Al3+ resides principally in Q4 structural units, which contain more than 70% of the total amount of Al3+. The Q2 units contain the smallest amount of Al3+ among the Q4, Q3, and Q2 structural units. There is no evidence for temperature-dependent distribution of Al3+ among the coexisting structural units at least to 1100–1200 °C.

The equilibrium constant for the speciation reaction, 2Q3 {leftrightarrow} Q4 + Q2, passes through a maximum with increasing bulk melt Al/(Al + Si) at constant temperature. Its temperature-dependence also depends on bulk melt Al/(Al + Si) so that the enthalpy of the speciation reaction, {Delta}H, passes through a maximum with increasing bulk Al/(Al + Si). This {Delta}H ranges between 13 and 23 kJ/mol for bulk melt Al/(Al + Si) between 0 and 0.33. These composition-dependent maxima in the equilibrium constant (at constant temperature) and {Delta}H of the speciation reaction reflect the changes in Al/(Al + Si) of Q2, Q3, and Q4 structural units with Al/(Al + Si) of the melt.




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