A 29Si MAS NMR study of sub-Tg amorphization of stishovite at ambient pressure

Xianyu Xue, Jonathan F. Stebbins, Masami Kanzaki

Research output: Contribution to journalArticle

19 Citations (Scopus)

Abstract

Stishovite, a high-pressure SiO2 polymorph in which each Si is coordinated by six O atoms, transforms to an amorphous phase when undergoing heat treatment below the glass transition temperature at ambient pressure. We have applied 29Si magic angle spinning nuclear magnetic resonance spectroscopy (MAS NMR) to study this amorphization process. We found that the amorphous phase generated after heating stishovite for up to 3 days at around 600 ° C consisted exclusively of four-coordinate Si, similar to glasses quenched from melts at ambient pressure. Furthermore, our data suggest that there are subtle structural differences between the amorphous phase transformed from stishovite at 600 ° C and glasses quenched from melts at ambient pressure: the amorphous phase from stishovite had a smaller mean Si-O-Si angle initially, and it gradually relaxed toward the latter with increasing heating time. There was no detectable change in the stishovite structure even after about 80% of it had been converted to the amorphous phase. The mechanism of the amorphization of stishovite is discussed in light of these results.

Original languageEnglish
Pages (from-to)480-485
Number of pages6
JournalPhysics and Chemistry of Minerals
Volume19
Issue number7
DOIs
Publication statusPublished - Feb 1993
Externally publishedYes

Fingerprint

stishovite
Magic angle spinning
Amorphization
Nuclear magnetic resonance spectroscopy
nuclear magnetic resonance
spectroscopy
glass
Heating
Glass
melt
heating
Polymorphism
Heat treatment
transform
Atoms

ASJC Scopus subject areas

  • Materials Science(all)
  • Geochemistry and Petrology
  • Earth and Planetary Sciences(all)
  • Environmental Science(all)

Cite this

A 29Si MAS NMR study of sub-Tg amorphization of stishovite at ambient pressure. / Xue, Xianyu; Stebbins, Jonathan F.; Kanzaki, Masami.

In: Physics and Chemistry of Minerals, Vol. 19, No. 7, 02.1993, p. 480-485.

Research output: Contribution to journalArticle

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