Abstract
Cerussite (PbCO3) has been investigated by high-pressure and high-temperature Raman spectroscopy up to pressures of 17.2 GPa and temperatures of 723 K. Two pressure induced phase transitions were observed at about 8.0(2) and 16.0(2) GPa, respectively. The post-aragonite transition (PbCO3-II) at 8.0(2) GPa is accompanied by softening of the v2-out-of-plane mode of the CO32- group and disappearance of the B1g (v4-in-plane band of the CO32- group) mode. Stronger shifts of the carbonate group modes after the phase transition suggest that the new structure is more compressible. The formation of a second high-pressure polymorph begins at about 10 GPa. It is accompanied by the occurrence of three new bands at different pressures and splitting of the v1-symmetric C-O stretching mode of the CO32- group. The transitions are reversible on pressure release. A semi-quantitative phase diagram for PbCO3 as a function of pressure and temperature is proposed.
| Original language | English |
|---|---|
| Pages (from-to) | 45-56 |
| Number of pages | 12 |
| Journal | Physics and Chemistry of Minerals |
| Volume | 37 |
| Issue number | 1 |
| DOIs | |
| State | Published - 2010 |
Keywords
- Cerussite
- High pressure
- High temperature
- Phase transition
- Raman spectroscopy
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