A Raman spectroscopic study of bukovskýite Fe2(AsO4)(SO4)(OH)· 7H2O, a mineral phase with a significant role in arsenic migration
Version of Record online: 23 FEB 2011
Copyright © 2011 John Wiley & Sons, Ltd.
Journal of Raman Spectroscopy
Volume 42, Issue 7, pages 1596–1600, July 2011
How to Cite
Loun, J., Čejka, J., Sejkora, J., Plášil, J., Novák, M., Frost, R. L., Palmer, S. J. and Keeffe, E. C. (2011), A Raman spectroscopic study of bukovskýite Fe2(AsO4)(SO4)(OH)· 7H2O, a mineral phase with a significant role in arsenic migration. J. Raman Spectrosc., 42: 1596–1600. doi: 10.1002/jrs.2900
- Issue online: 6 JUL 2011
- Version of Record online: 23 FEB 2011
- Manuscript Accepted: 27 DEC 2010
- Manuscript Received: 29 SEP 2010
- Ministry of Culture of the Czech Republic. Grant Number: MK00002327201
- Raman spectroscopy;
- hydroxyl ions;
- molecular water
The Raman spectrum of bukovskýite [Fe3+2(OH)(SO4)(AsO4)· 7H2O] has been studied and compared with that of an amorphous gel containing specifically Fe, As and S, which is understood to be an intermediate product in the formation of bukovskýite. The observed bands are assigned to the stretching and bending vibrations of (SO4)2− and (AsO4)3− units, stretching and bending vibrations and vibrational modes of hydrogen-bonded water molecules, stretching and bending vibrations of hydrogen-bonded (OH)− ions and Fe3+(O,OH) units. The approximate range of OH···O hydrogen bond lengths was inferred from the Raman spectra. Raman spectra of crystalline bukovskýite and of the amorphous gel differ in that the bukovskýite spectrum is more complex, the observed bands are sharp and the degenerate bands of (SO4)2− and (AsO4)3− are split and more intense. Lower wavenumbers of δ H2O bending vibrations in the spectrum of the amorphous gel may indicate the presence of weaker hydrogen bonds compared to those in bukovskýite. Copyright © 2011 John Wiley & Sons, Ltd.