http://www.cnr.it/ontology/cnr/individuo/prodotto/ID29600
Scandium-45 NMR of pyrope-grossular garnets: resolution of multiple scandium sites and comparison with x-ray diffraction and x-ray spectroscopy. (Articolo in rivista)
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- Scandium-45 NMR of pyrope-grossular garnets: resolution of multiple scandium sites and comparison with x-ray diffraction and x-ray spectroscopy. (Articolo in rivista) (literal)
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- 2007-01-01T00:00:00+01:00 (literal)
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- Kim N.; Stebbins J.F.; Quartieri S.; Oberti R. (literal)
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amjun Kim,1 Jonathan F. Stebbins,1,* Simona Quartieri,2,3 and Roberta Oberti3
1Department of Geological and Environmental Sciences, Stanford University, Stanford, California 94305-2115, U.S.A.
2Dipartimento di Scienze della Terra, Università di Messina, Salita Sperone 31, I-98166 Messina S. Agata, Italy
3CNR, Istituto di Geoscienze e Georisorse, unità di Pavia, via Ferrata 1, I-27100 Pavia, Italy (literal)
- Titolo
- Scandium-45 NMR of pyrope-grossular garnets: resolution of multiple scandium sites and comparison with x-ray diffraction and x-ray spectroscopy. (literal)
- Abstract
- Ca3Al2Si3O12), and an 80% grossular-20% pyrope garnet (grs80) that have recently been well-studied by X-ray diffraction and X-ray spectroscopies. Clearly distinct NMR peaks are observed for Sc in the eight-coordinated X site (pyrope and grs80) and in the six-coordinated Y site (grossular and grs80). X-ray and NMR data agree that only eight-coordinated Sc is present in pyrope and that six-coordinated Sc is predominant in grossular; however, the XRD results also indicated significant X and Z site (four-coordinated) Sc in the Ca-rich garnet. Possible reasons for this apparent discrepancy are discussed. We demonstrate that 45Sc NMR is potentially a useful new method for studies of the site occupancies of Sc3+ in oxides and silicates, at least in experimental systems where its concentration is a few percent or greater. (literal)
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