TY - JOUR
T1 - Thermochemistry and structure of glasses along the join NaAlSi3O8-NaBSi3O8
AU - Geisinger, K. L.
AU - Oestrike, R.
AU - Navrotsky, A.
AU - Turner, G. L.
AU - Kirkpatrick, R. J.
N1 - Funding Information:
Acknowledgements-This work was supportedb y grantst o A.N., NSF EAR 851391a6n dD OE DE FGO2-85ER1343a7n dto R.J.K., NSF EAR8408421W. e would also like to thankt he Smithsonian Institutionf or providings ampleso f them ineralr eedmergneriutes ed in this study.B enM ontezc ollectesdo meo f the spectraR. eviewsb y Prof. J. Stebbinsa nda n anonymousre viewesr ubstantialliym proved the manuscript.
PY - 1988/10
Y1 - 1988/10
N2 - Glasses along the join NaAlSi3O8-NaBSi3O8 and the end-member crystalline phases albite and reedmergnerite were investigated using 11B, 23Na, 27Al and 29Si MAS NMR spectroscopy and oxide-melt solution calorimetry. The glasses have substantial positive enthalpies of mixing described by the equation ΔHmix (kcal · mol t ̄1) = 4.4(±1.0)X(1 - X), where X is the mole fraction Rd component. 11B MAS NMR spectra show that boron occurs in both trigonal and tetrahedral coordination in the glasses, with the percentage of B in trigonal coordination decreasing from about 60% at Rd20Ab80 to about 29% at Rd100. Thus, the glasses are structurally more complex than the end-member crystals which are tetrahedral framework minerals. The NMR data suggest that all or most of the Si, Al and tetrahedral B occur in Q4 (framework) sites. They are also consistent with the ideas that most of the tetrahedral B does not extensively copolymerize with trigonal boron, that at least some of the non-bridging oxygens formed by the presence of trigonal boron are located on SiO4 tetrahedra, and that Si and trigonal B do not occur as next-nearest neighbors. Both the NMR and the Δ Hmix results indicate the presence of clustering. Such clustering might involve separation into framework regions and regions dominated by trigonal boron and/or into B-rich and Al-rich framework regions.
AB - Glasses along the join NaAlSi3O8-NaBSi3O8 and the end-member crystalline phases albite and reedmergnerite were investigated using 11B, 23Na, 27Al and 29Si MAS NMR spectroscopy and oxide-melt solution calorimetry. The glasses have substantial positive enthalpies of mixing described by the equation ΔHmix (kcal · mol t ̄1) = 4.4(±1.0)X(1 - X), where X is the mole fraction Rd component. 11B MAS NMR spectra show that boron occurs in both trigonal and tetrahedral coordination in the glasses, with the percentage of B in trigonal coordination decreasing from about 60% at Rd20Ab80 to about 29% at Rd100. Thus, the glasses are structurally more complex than the end-member crystals which are tetrahedral framework minerals. The NMR data suggest that all or most of the Si, Al and tetrahedral B occur in Q4 (framework) sites. They are also consistent with the ideas that most of the tetrahedral B does not extensively copolymerize with trigonal boron, that at least some of the non-bridging oxygens formed by the presence of trigonal boron are located on SiO4 tetrahedra, and that Si and trigonal B do not occur as next-nearest neighbors. Both the NMR and the Δ Hmix results indicate the presence of clustering. Such clustering might involve separation into framework regions and regions dominated by trigonal boron and/or into B-rich and Al-rich framework regions.
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U2 - 10.1016/0016-7037(88)90297-9
DO - 10.1016/0016-7037(88)90297-9
M3 - Article
AN - SCOPUS:0024252609
SN - 0016-7037
VL - 52
SP - 2405
EP - 2414
JO - Geochimica et Cosmochimica Acta
JF - Geochimica et Cosmochimica Acta
IS - 10
ER -