Aluminum coordination and the densification of high-pressure aluminosilicate glasses

被引:197
作者
Allwardt, JR [1 ]
Stebbins, JF
Schmidt, BC
Frost, DJ
Withers, AC
Hirschmann, MM
机构
[1] Stanford Univ, Dept Geog & Environm Sci, Stanford, CA 94305 USA
[2] Univ Bayreuth, Bayer Geoinst, D-95440 Bayreuth, Germany
[3] Univ Minnesota, Dept Geol & Geophys, Minneapolis, MN 55455 USA
关键词
D O I
10.2138/am.2005.1836
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
To better understand the relationship between atomic-scale structures and densities of aluminosilicate glasses and liquids, we used Al-27 MAS NMR to determine the speciation of aluminum ions in K3AlSi3O9, Na3AlSi3O9, and Ca3Al2Si6O18 glasses quenched from melts at 3 to 10 GPa. These data are a first approximation of high-pressure melt structure and illustrate the effects of the type of modifier cation. High field strength modifier cations (e.g., Ca) clearly induce more high-coordinated Al than lower field strength cations (e.g., Na and K), Measured glass densities show that, especially with rapid decompression, a significant portion of the total densification observed in-situ in melts is retained on return to ambient temperature and pressure. Observed increases in Al coordination are well correlated with decreased volume, which suggests that this structural change is a major part of the mechanism for recovered densification of high-pressure melts. Additionally, Na-23 MAS NMR, combined with the Al-27 MAS spectra and density determinations, reveal that other changes, such as the compression of modifier cation sites and/or decreased network bond angles, must also be significant, especially at low pressure.
引用
收藏
页码:1218 / 1222
页数:5
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