Journal of Mineralogical and Petrological Sciences
Online ISSN : 1349-3825
Print ISSN : 1345-6296
ISSN-L : 1345-6296

この記事には本公開記事があります。本公開記事を参照してください。
引用する場合も本公開記事を引用してください。

Elastic wave velocity measurements of Na2Si2O5 glass at high pressure
Tatsuya SAKAMAKI Yamato ARAKINaoki TAKAHASHIAkio SUZUKI
著者情報
ジャーナル オープンアクセス 早期公開

論文ID: 260128

この記事には本公開記事があります。
詳細
抄録

Elastic wave velocities of sodium disilicate (Na2Si2O5; NS2) glass were determined up to 7 GPa using an ultrasonic pulse–echo overlap technique combined with synchrotron X-ray imaging in a Kawai-type multi-anvil apparatus. NS2 glass represents an intermediate degree of polymerization (NBO/T = 1), bridging the compositional gap between fully polymerized and depolymerized silicate glasses. The compressional wave velocity (VP) increases monotonically with pressure, whereas the shear wave velocity (VS) remains nearly constant up to ∼4 GPa before rising at higher pressures. In comparison with fully polymerized (silica, jadeite, albite) and depolymerized (diopside, enstatite) glasses, the pressure dependence of NS2 glass resembles that of depolymerized compositions. These results indicate that the transition between polymerized and depolymerized elastic behavior occurs near NBO/T = 1. Consequently, mafic melts (NBO/T < 1) may exhibit anomalous elastic properties under upper-mantle conditions, whereas ultramafic melts (NBO/T > 1) are expected to stiffen monotonically with increasing pressure.

著者関連情報
© 2026 Japan Association of Mineralogical Sciences

This is an open access article distributed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0), which permits non-commercially distribute and reproduce an unmodified in any medium, provided the original work is properly cited.
https://creativecommons.org/licenses/by-nc-nd/4.0/
feedback
Top