Cation mass-valence sum (CM-VS) approach to assigning OH-bending bands in dioctahedral smectites
Gates, Will 
(Monash University. Department of Civil Engineering)
| Data: |
2008 |
| Resum: |
The assignments of OH-bending bands in the infrared (IR) spectra of dioctahedral smectites (montmorillonites, ferruginous smectites, and nontronites) have been revisited using a cation mass-valence sum (CM-VS) approach to quantify octahedral cation occupancy. The CM-VS approach enabled prediction of OH-bending band positions (in wavenumbers) related to OH-sharing octahedral cation pairs that had valence sums of 4 and 5, and cation masses associated with Fe(II) and Mg. Application of rules for the relationship enabled determination of the location of OH-sharing octahedral cation pairs containing Mg and Fe(II) for which previous assignments have been considered controversial, e. g. Fe(III)Mg-OH and MgMg-OH, or for which assignments have been missing due to lack of spectroscopic evidence, e. g. AlFe(II)-OH, Fe(III)Fe(II)-OH, Fe(II)Mg-OH, and Fe(II)Fe(II)-OH. Examples of these bands from several natural ferruginous smectites and nontronites are discussed. Quantification of IR spectra was used to develop a better understanding of the octahedral cation occupancy of this important class of Fe(III)-enriched smectites. While Fe(II) contents may be somewhat overestimated by the IR technique, those for four of the six ferruginous smectites studied here agree well with data from Mössbauer spectroscopy. |
| Drets: |
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| Llengua: |
Anglès |
| Document: |
Article ; recerca ; Versió publicada |
| Matèria: |
Cation mass ;
Cation pairs ;
Infrared spectroscopy ;
Octahedral ;
Smectite chemistry ;
Valence sum |
| Publicat a: |
Clays and Clay Minerals, Vol. 56, Núm. 1 (2008) , p. 10-22, ISSN 1552-8367 |
DOI: 10.1346/CCMN.2008.0560102
13 p, 1.8 MB
Accés restringit a la UAB
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