Abstract
The structures of deuterated pyrochroite, Mn(OD)2 and β-Co(OD)2 have been refined using the Rietveld method and neutron powder diffraction data collected in an opposed-anvil high pressure (Paris-Edinburgh) cell from room pressure to 9 GPa. The equation of state for Mn(OD)2 was determined (K=41(3) GPa for fixed K'=4.7) and found to be consistent with previous studies of the isostructural brucite, Mg(OD)2. The compressibility of β-Co(OD)2 on the other hand is apparently anomalous. The c-axis initially decreases at 3 times the rate of decrease of the a-axis; the ratio decreases to about 1.5 at an estimated 6 GPa before increasing again beyond this pressure. There is no obvious corresponding anomaly in the details of the atomic structure. In both materials there is an increase in the D-site disorder with pressure. A split-site model for the D-positions best fits the data at pressures above 8 GPa. There is no statistically significant increase in the O-D interatomic distance at increased pressure while the hydrogen bonding interaction D...O appears to increase as this distance decreases and the O-D...O angle increases. The intramolecular O-D bond valences, determined indirectly from the intermolecular D...O distances, decrease steadily for both materials as pressure is increased.
| Original language | English |
|---|---|
| Pages (from-to) | 130-137 |
| Number of pages | 8 |
| Journal | Physics and Chemistry of Minerals |
| Volume | 25 |
| Issue number | 2 |
| DOIs | |
| State | Published - Jan 1998 |
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