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The high sensitivity of the satellite-transition (ST) MAS NMR technique was exploited to obtain high-resolution  17 O MAS NMR spectra of the three polymorphs of Mg 2 SiO 4 : forsterite (α-Mg 2 SiO 4 ), wadsleyite (β-Mg 2 SiO 4 ), and ringwoodite (γ-Mg 2 SiO 4 ). High NMR sensitivity was important in this application because  17 O-enriched, Fe-free materials are required for  17 O 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.

High-resolution 17 O MAS NMR spectroscopy of forsterite (α-Mg 2 SiO 4 ), wadsleyite (β-Mg 2 SiO 4 ), and ringwoodite (γ-Mg 2 SiO 4 )