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Fe, Mg and Al distribution in the octahedral sheet of montmorillonites. An infrared study in the OH-bending region

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Abstract:

Ten montmorillonites of different origins with variable Fe contents were analysed using transmission IR spectroscopy. Special attention was devoted to the OH-bending region to obtain information about the distribution of octahedral cations. For low to medium Fe contents (≤0.56 per Si8 formula unit), a linear relationship between the position of the AlFeOH band and Fe content was observed. Such correlation might be explained by changes in the cis-trans occupancy of Fe in the octahedral sheet. Deconvolution of the OH-bending domain allows us to discriminate three components (AlAlOH, AlMgOH and AlFeOH) which are correlated with cation abundances derived from chemical analysis. The relative area of each band can then be compared with theoretical areas calculated assuming a fully random distribution of cations in the octahedral sheet. Using such treatment, eight of the 10 montmorillonites studied presented a nearly randomized octahedral distribution. The two samples from Wyoming were clearly different as they exhibited a strong ordering tendency.

Keywords: BENTONITE; IR SPECTROSCOPY; MONTMORILLONITE; OCTAHEDRAL CATIONS; OH-BENDING REGION; SMECTITE

Document Type: Research Article

DOI: http://dx.doi.org/10.1180/000985501750539463

Publication date: September 1, 2001

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minsoc/cm/2001/00000036/00000003/art00008
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