Raman and Fourier transform infrared spectroscopic study of pyromorphite-vanadinite solid solutions.

Spectrochim Acta A Mol Biomol Spectrosc

AGH - University of Science and Technology, Faculty of Geology, Geophysics and Environment Protection, Department of Mineralogy, Petrography and Geochemistry, Mickiewicza 30 Ave., 30-059 Krakow, Poland.

Published: February 2018

Due to the great range of the application fields for apatites, there is a strong need to complete the data set determining the properties of these minerals. In this study, Raman and Infrared spectra of the phases from pyromorphite Pb(PO)Cl - vanadinite Pb(VO)Cl series were investigated. Totally, 9 samples (2 end-members and 7 solid solutions of the series) were synthesized at 25°C and pH=3.5, and analyzed. In the Raman and Infrared spectra of the studied Pb-apatites, the bands typical for the vibrations in the PO and the VO tetrahedra appeared. The bands attributed to the stretching vibrations (ν, ν) occurred in the 1050-910cm and 830-720cm regions, whereas the bending vibrations (ν, ν) were visible at the 580-540cm, 430-380cm and 370-290cm range. The position of the bands depended on the P/(P+V) ratio in the analyzed solid, since there are differences in the ionic radii and the atomic mass of P and V, which affect the bong lengths, bond forces and the banding energies of the substituting tetrahedra. The analysis allowed observing gradual shifts of the bands caused by the replacement of phosphorous with vanadium in the studied phases. The positions and the intensities of selected bands are proposed to serve as a semi-quantitative estimation of the chemical composition of the phases from the pyromorphite - vanadinite series.

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http://dx.doi.org/10.1016/j.saa.2017.08.061DOI Listing

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