1. Anharmonic OH vibrations in brucite: Small pressure-induced redshift in the range 0-22 GPa
- Author
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Mitev, Pavlin D., Gajewski, Grzegorz, and Hermansson, Kersti
- Subjects
Brucite -- Properties ,Materials at high pressures -- Evaluation ,Vibration -- Measurement ,Quantum theory -- Research ,Earth sciences - Abstract
The uncoupled anharmonic OH-stretching vibrational frequency for the layered mineral Mg[(OH).sub.2] (brucite) has been calculated in the pressure range 0-22 GPa. Quantum-mechanical electronic structure (DFT) calculations were performed, followed by quantum-mechanical vibrational energy calculations. The following findings emerged: (1) The calculated dv(OH)/dP slope is -4 [cm.sup.-1]/GPa, in agreement with the experimental literature value [taken as the average between the Raman and IR-measured slopes for Mg[(OH).sub.2]]. (2) The calculated v(OH) vs. R(O***O) correlation is linear and the slope is much smaller than that of traditional H-bond correlation curves in the literature. (3) The main origin of the small dv/dP and dv/dR(O***O) slopes is the small electric field variation as the mineral layers are pressed toward each other. (4) At high pressure, the OH- ions show s[O.sup.m]e tendency to be tilted with respect to the c axis, and a larger tilt angle leads to a larger v(OH) downshift. (5) The pressure variation of the D quadrupole coupling constant is approximately -1 kHz/GPa. Keywords: Brucite, anharmonic OH frequencies, high pressure, electric field, hydrogen bonding, correlation curve, hydrous mineral DOI: 10.2138/am.2009.3188
- Published
- 2009