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Harris, M. J., Dove, M. T., Parker, J. M. (2000) Floppy modes and the Boson peak in crystalline and amorphous silicates: an inelastic neutron scattering study. Mineralogical Magazine, 64 (3) 435-440 doi:10.1180/002646100549490

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Reference TypeJournal (article/letter/editorial)
TitleFloppy modes and the Boson peak in crystalline and amorphous silicates: an inelastic neutron scattering study
JournalMineralogical Magazine
AuthorsHarris, M. J.Author
Dove, M. T.Author
Parker, J. M.Author
Year2000 (June)Volume64
Issue3
PublisherMineralogical Society
DOIdoi:10.1180/002646100549490Search in ResearchGate
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Mindat Ref. ID243182Long-form Identifiermindat:1:5:243182:0
GUID0
Full ReferenceHarris, M. J., Dove, M. T., Parker, J. M. (2000) Floppy modes and the Boson peak in crystalline and amorphous silicates: an inelastic neutron scattering study. Mineralogical Magazine, 64 (3) 435-440 doi:10.1180/002646100549490
Plain TextHarris, M. J., Dove, M. T., Parker, J. M. (2000) Floppy modes and the Boson peak in crystalline and amorphous silicates: an inelastic neutron scattering study. Mineralogical Magazine, 64 (3) 435-440 doi:10.1180/002646100549490
Abstract/NotesAbstractWe present the results of an inelastic neutron scattering study of a crystalline polymorph of SiO2 (α-quartz), and a number of silicate glasses (pure silica, SiO2, and three glasses in the alkali series (K,Li)2Si2O5). We demonstrate the presence of the Boson peak in the inelastic spectra of the crystalline and amorphous materials and argue that it arises simply from the dispersion characteristics of transverse acoustic modes. Furthermore, we investigate the role of the lower-energy floppy modes in the inelastic spectra, and show that they are controlled by chemical effects.


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