The Coordination of Aluminum Ions in the Palygorskite Structure
Authors:
- Necip GüvenNGNecip Güven
- Jean-Baptiste D'ESpinose de la CaillerieJean-Baptiste D'ESpinose de la Caillerie
- Jose J. FripiatJFJose J. Fripiat
- 1 August 1992
- journal article
- Published by Cambridge University Press (CUP) in Clays and Clay Minerals
- Vol. 40 (4) , 457-461
Abstract
NMR spectra of PF1-1 Floridan palygorskite strongly suggest that Al 3+ occurs only in octahedral coordination. X-ray microanalysis of the palygorskite fibers indicate a chemical composition defined by the atomic ratios: Mg/Si = 0.34, Al/Si = 0.27, and Fe/Si = 0.04. Considering the NMR and CEC data in this report along with the previously published results of IR and Mössbauer spectroscopic studies, the following structural formula is proposed for PF1-1 palygorskite: $${\rm{(M{g_{2.12}}A{l_{1.68}}F{e^{3 + }}_{0.24}{\square _{0.96}})S{i_8}{O_{20}}{(OH)_2}{(O{H_2})_4}}}$$ where □ represents the vacant Ml octahedral sites in the structure, and Al 3+ and Fe 3+ are all exclusively assigned to the octahedral sites.
Keywords
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