Hydrogen in stishovite, with implications for mantle water content

Alison R. Pawley*, Paul F. McMillan, John R. Holloway

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    Abstract

    Stishovite, the highest pressure polymorph of silicon dioxide, may be an important mineral in some regions of the Earth's mantle. Fourier transform infrared spectroscopy has been used to determine the hydrogen content of synthetic stishovite. The concentration of hydrogen depends on the aluminum content of the sample and reaches a maximum of 549 ± 23 hydrogen atoms per 106 silicon atoms for an Al2O3 content of 1.51 percent by weight. Stishovite could be a storage site for water in deep subducting slabs and in regions of the mantle that are too hot for hydrous minerals to be stable.

    Original languageEnglish
    Pages (from-to)1024-1026
    Number of pages3
    JournalScience
    Volume261
    Issue number5124
    DOIs
    Publication statusPublished - 1 Jan 1993

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