Raman microspectroscopy of some iron oxides and oxyhydroxides

Hematite (α‐Fe2O3), magnetite (Fe3O4), wüstite (FeO), maghemite (γ‐Fe2O3), goethite (α‐FeOOH), lepidocrocite (γ‐FeOOH) and δ‐FeOOH were studied by Raman microscopy. Such compounds have already been studied by Raman spectroscopy, but there are some disagreements in the reported data. Here, Raman micr...

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Bibliographic Details
Published in:Journal of Raman spectroscopy Vol. 28; no. 11; pp. 873 - 878
Main Authors: de Faria, D. L. A., Venâncio Silva, S., de Oliveira, M. T.
Format: Journal Article
Language:English
Published: Chichester, UK John Wiley & Sons, Ltd 01-11-1997
Online Access:Get full text
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Summary:Hematite (α‐Fe2O3), magnetite (Fe3O4), wüstite (FeO), maghemite (γ‐Fe2O3), goethite (α‐FeOOH), lepidocrocite (γ‐FeOOH) and δ‐FeOOH were studied by Raman microscopy. Such compounds have already been studied by Raman spectroscopy, but there are some disagreements in the reported data. Here, Raman microscopy was employed to investigate the laser power dependence of the spectra of these oxides and oxyhydroxides. Low laser power was used for the reference spectra in order to minimize the risks of spectral changes due to sample degradation. The results obtained show that increasing laser power causes the characteristic bands of hematite to show up in the spectra of most of the compounds studied whereas the hematite spectrum undergoes band broadening and band shifts. © 1997 John Wiley & Sons, Ltd.
Bibliography:FAPESP
istex:2C6A41D7F3A59374B30ECA6CC097E8029214B8E2
CNPq
ark:/67375/WNG-QDTPTZ48-B
ArticleID:JRS177
ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:0377-0486
1097-4555
DOI:10.1002/(SICI)1097-4555(199711)28:11<873::AID-JRS177>3.0.CO;2-B