Abstract
The crystal structure of deuterated topaz [topaz-OD; Al2SiO4 (OD)2], synthesized at 10 GPa and 800 °C, has been determined using neutron powder diffraction at pressures up to 7.5 GPa. The linear axial compressibilities obtained from regressions of the lattice constants vs. pressure are β a = 1.87(1) × 10-3 GPa-1, βb = 1.7t(1) × 10-3 GPa-1, and βc, = 2.73(1) × 10-3 GPa-1. The occupancy of the D1 site was found to be greater than that of D2, as shown independently using neutron diffraction and infrared spectra at ambient conditions. A bifurcated hydrogen bond involving the D1 site, O4-D1⋯O2 and O4-D1⋯O3, and a trifurcated hydrogen bond involving D2 site, O4-D2⋯O1, O4-D2⋯O2, and O4-D2⋯O4 are proposed for hydrogen-bond donor and acceptor pairs in addition to those reported previously. The observed pressure dependences of the hydrogen-bonding geometry show that these donor and acceptor pairs are classifiable into two types of interaction: (1) those that strengthen as a function of pressure (O4-D1⋯O3, O4-D2⋯O2, and O4-D2⋯O4) and (2) those that weaken (O4-D1⋯O1 and O4-D2⋯O1). These results also demonstrate that the reason for the contrasting behavior of the v(OH) between F-rich natural topaz and topaz-OH are both the cooperative effect, O4-D2⋯O4-D2⋯O3, and the increasing A1-O4 distance.
| Original language | English |
|---|---|
| Pages (from-to) | 217-227 |
| Number of pages | 11 |
| Journal | American Mineralogist |
| Volume | 93 |
| Issue number | 1 |
| DOIs | |
| State | Published - Jan 2008 |
Keywords
- High pressure
- Hydrogen bond
- Neutron powder diffraction
- Topaz-OD
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