• journal_title：American Mineralogist
• Contributor：Sharon E. Ashbrook ; Andrew J. Berry ; William O. Hibberson ; Stefan Steuernagel ; Stephen Wimperis
• Publisher：Mineralogical Society of America
• Date：2005-
• Format：text/html
• Language：en
• Identifier：10.2138/am.2005.1915
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：90
• issue：11-12
• firstpage：1861
• section：Articles

The high sensitivity of the satellite-transition (ST) MAS NMR technique was exploited to obtain high-resolution ¹⁷O MAS NMR spectra of the three polymorphs of Mg₂SiO₄: forsterite (α-Mg₂SiO₄), wadsleyite (β-Mg₂SiO₄), and ringwoodite (γ-Mg₂SiO₄). High NMR sensitivity was important in this application because ¹⁷O-enriched, Fe-free materials are required for ¹⁷O NMR and high-pressure syntheses of the dense β and γ polymorphs result in a only a few milligrams of these solids. In all, eight distinct O species were identified and assigned: three in forsterite, four in wadsleyite, and one in ringwoodite, in agreement with the number of O sites in their crystal structures. The isotropic chemical shifts extracted are in excellent agreement with a previously published correlation with Si-O bond length. However, unexpectedly large quadrupolar coupling constants were found for the non-bridging O species in the dense polymorphs wadsleyite and ringwoodite.