Abstract
Single-crystal polarized Raman spectra (3,000–4,000 cm−1 at 3 ≤ T ≤ 300 K) were measured for synthetic alkali-free and natural beryl, Be2Al3Si6O18·xH2O, to determine the behavior of H2O molecules of both Type I and Type II in the cavities. At low temperature, the H2O molecules of Type I displace from the center of cavity and give rise to very weak hydrogen bonding with the host lattice. The H2O Type I translational motion is characterized by substantial anharmonicity and looks like a motion of “a particle in the box” with a frequency of 6.3 cm−1. Water Type II is characterized by a free rotation with respect to the C 2 molecule axis, and it makes possible the water nuclear isomers (i.e. ortho- and para-) to be observed at low temperature.
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Notes
The fitting of the observed spectra by Gauss functions results from technical reasons but not Gauss distribution of the oscillators: at low-temperature the bandwidth of the observed modes is less than dimension of a pixel of the CCD-matrix; this circumstance and charge spreading between the neighbor pixels produce “incorrect” contour of the spectral line.
In theory, band width of any vibrational band is defined by a lifetime of the excited state. The latter is governed by dissipation of energy of the excited state (i.e. Born and Huang 1954) or delay of the given phonon into other phonons of lower frequency (i.e. Balkanski et al. 1983). In both cases, a temperature decreasing should result in exponential narrowing of vibrational bands due to freezing-out of low-frequency vibrations.
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Acknowledgments
The author thanks V. Thomas, S. Demin, and Dr. Yu.V. Seryotkin of the United Institute of Geology, Geophysics and Mineralogy, Novosibirsk, Russia, for providing the beryl and analcime crystals. P. L. Chapovsky (Institute of Automation and Electrometry, Russian Academy of Sciences, Novosibirsk) is thanked for helpful discussion. The author thanks Prof. Mauro Prencipe and an anonymous referee for helpful comments that improved the manuscript.
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Kolesov, B. Vibrational states of H2O in beryl: physical aspects. Phys Chem Minerals 35, 271–278 (2008). https://doi.org/10.1007/s00269-008-0220-z
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DOI: https://doi.org/10.1007/s00269-008-0220-z