2026-07-24T20:53:49Zhttps://docta.ucm.es/rest/oai/requestoai:docta.ucm.es:20.500.14352/497412023-08-27T12:15:36Zcom_20.500.14352_14col_20.500.14352_15
Docta Complutense
author
Súarez Barrios, Mercedes
author
García Romero, Emilia
2023-06-20T09:30:08Z
2023-06-20T09:30:08Z
2006
0169-1317
10.1016/j.clay.2005.10.005
https://hdl.handle.net/20.500.14352/49741
http://www.elsevier.com/locate/clay
The influence of chemical composition to position and intensity of the absorption bands observed in the FTIR spectra of
palygorskite has been studied by a detailed comparative study of six samples. Palygorskites studied have high purity and different
chemical composition. At one extreme, there are two samples that correspond to Mg-rich palygorskites, at the other extreme a
sample with a composition very close to the theoretical formula of this mineral, and there are three further samples whose structural
formulae lie between these extremes. The position of the bands identified in the FTIR spectra of the palygorskites studied is similar
for all samples, but there are some differences in their intensity, which are significant. Analysing these intensities, valuable
information about the distribution of cations along the octahedral sheet has been obtained. Isomorphic substitution in octahedral
sheet occurs only in M2 position. Al, and Fe may occupy M2 position whereas Mg can occupy all possible sites: M1, M2 and M3.
eng
FTIR spectroscopic study of palygorskite: Influence of the
composition of the octahedral sheet
journal article
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https://docta.ucm.es/bitstreams/02757073-468b-4a32-8f5d-299e609b3251/download
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397534
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2006_FTIR_Palygorskite_1.pdf
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38743
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2006_FTIR_Palygorskite_1.pdf.txt