New Insight into the Relationships Between Structural and Ftir Spectroscopic Features of Kaolinites
Victor A. Drits, Bella B. Zviagina, B. A. Sakharov, O. V. Dorzhieva, А. Т. Savichev
Abstract
Abstract To resolve the existing ambiguities in the interpretation of the OH-stretching vibrations of kaolinites, relationships were, for the first time, established between the structural and Fourier-transform infrared (FTIR) spectroscopic features for a set of kaolinite samples which differed in terms of their relative amounts of coexisting high- and low-ordered phases. For this purpose, a representative collection of kaolinites differing in origin, particle size, and degree of disorder was studied by powder X-ray diffraction (XRD) and FTIR spectroscopy. Modeling of the experimental XRD patterns based on the orthogonal layer unit cell having a mirror plane showed each sample to be a mixture of nearly defect-free high-ordered (HOK) and low-ordered (LOK) kaolinite phases, with HOK varying from 86 to 4%. The wavenumbers, heights, areas, and full widths at half-maximum (FWHM) were determined for the OH-stretching bands at ~3697 ( ν 1 ), ~3670 ( ν 2 ), ~3652 ( ν 3 ), and 3620 cm –1 ( ν 4 ) by decomposition and fitting of the FTIR spectra. The FWHM(ν 1 )/FWHM(ν 4 ) and FWHM(ν 3 )/FWHM(ν 2 ) values were related linearly to the HOK content, which may be associated with the in-phase and out-of-phase character of the corresponding pairs of vibrations, respectively. A novel interpretation was suggested for the variations in the relative integrated intensities of the OH bands with the amount of the HOK phase. The intensity distribution of the ν 2 and ν 3 bands is controlled by the triclinic structure symmetry in the defect-free kaolinite and the mirror symmetry of the layers in low-ordered structures, in agreement with the observed evolution of the corresponding band intensities. The ν 1 and ν 2 band positions for the low-ordered samples are within the wavenumber range for the high-ordered samples. In contrast, the ν 3 and ν 4 band positions for the low-ordered samples are shifted toward higher wavenumbers, indicating that some of the low-ordered kaolinites should contain dickite-like structural fragments distributed among kaolinite layers.