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Purton, J., Urch, D. S. (1989) High-resolution silicon Kβ X-ray spectra and crystal structure. Mineralogical Magazine, 53 (370) 239-244 doi:10.1180/minmag.1989.053.370.11

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Reference TypeJournal (article/letter/editorial)
TitleHigh-resolution silicon Kβ X-ray spectra and crystal structure
JournalMineralogical MagazineISSN0026-461X
AuthorsPurton, J.Author
Urch, D. S.Author
Year1989 (April)Volume53
Issue370
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_53/53-370-239.pdf+
DOIdoi:10.1180/minmag.1989.053.370.11Search in ResearchGate
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Mindat Ref. ID1497Long-form Identifiermindat:1:5:1497:1
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Full ReferencePurton, J., Urch, D. S. (1989) High-resolution silicon Kβ X-ray spectra and crystal structure. Mineralogical Magazine, 53 (370) 239-244 doi:10.1180/minmag.1989.053.370.11
Plain TextPurton, J., Urch, D. S. (1989) High-resolution silicon Kβ X-ray spectra and crystal structure. Mineralogical Magazine, 53 (370) 239-244 doi:10.1180/minmag.1989.053.370.11
In(1989, April) Mineralogical Magazine Vol. 53 (370) Mineralogical Society
Abstract/NotesAbstractHigh-resolution X-ray emission spectra (XES) are presented for minerals with a variety of structures. The participation of the Si 3p orbitals in bonding is influenced by the local structure around the silicon atom. In orthosilicates the distortion of the SiO44--tetrahedron influences both peak-width and the intensity of the high-energy shoulder of the Si-Kβ spectrum. In minerals containing Si-O-Si bonds there is mixing of the Si 3s and 3p orbitals giving rise to a peak on the low-energy side of the main Si-Kβ peak. When combined with X-ray photoelectron spectra (XPS), a complete molecular orbital picture of bonding can be established.


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