Pistorius & Clark (1969
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
), Meisalo & Kalliomäki (1976
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
), Adams
et al. (1983
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
), Lee
et al. (1993
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
) and Grzechnik & Friese (2008
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
) reported previously on the high-pressure behaviour of Tl
2CO
3. A sequence of phase transitions at 2, 4.2 and 6.7 GPa was discovered by Meisalo & Kalliomäki (1976
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
), in which the phases below 6.7 GPa were supposed to be structurally very similar. Adams
et al. (1983
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
) also observed phase transitions near 1.3 and 3.8 GPa using IR and Raman spectroscopic analyses. However, a single-crystal diffraction study demonstrated that thallium carbonate (
C2/
m,
Z = 4) is structurally stable to at least 3.56 GPa (Grzechnik & Friese, 2008
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
). The most likely reason for this discrepancy is that the X-ray and spectroscopic data of Meisalo & Kalliomäki (1976
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
) and Adams
et al. (1983
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
), respectively, were poorly resolved and the pressures were nonhydrostatic. In this study, we continue our work on Tl
2CO
3 using single-crystal X-ray diffraction in a diamond anvil cell to characterize the postulated (Meisalo & Kalliomäki, 1976
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
; Adams
et al., 1983
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
) pressure-induced polymorphs above about 4 and 6.7 GPa.
A crystal of dithallium carbonate was compressed slowly to a pressure of 5.82 GPa. Indexing of the diffraction data, analysis of the reconstructed reciprocal space, and structure solution and refinement clearly showed that the material (
C2/
m,
Z = 4) does not transform to a new polymorph at about 4 GPa. However, on further compression to a pressure of 7.4 GPa, no single-crystal reflections were detected. Instead, weak and very smeared incomplete Debye–Scherrer rings were visible in the diffraction diagrams on the image plate. These observations indicate that Tl
2CO
3 does undergo a pressure-induced phase transition at about 6.7 GPa (Meisalo & Kalliomäki, 1976
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
) that also destroys the single crystal. It is thus the only transformation of those reported in the literature that we observe in our high-pressure single-crystal X-ray diffraction data under hydrostatic conditions.
As observed at ambient pressure (Marchand
et al., 1975
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
) and at 3.56 GPa (Grzechnik & Friese, 2008
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
), all atoms except for one of the O atoms lie on crystallographic mirror planes at 5.82 GPa. Two non-equivalent Tl
+ cations are in asymmetric coordination environments attributable to their electron lone pairs (
E). The Tl1 cation is coordinated to seven O atoms at distances in the range 2.50 (11)–2.9 (2) Å. The coordination around the Tl2 cation includes five O atoms at distances in the range 2.42 (19)–3.4 (3) Å (Table 1). The compression mainly affects the part of the structure where the Tl
+ lone pairs are placed. A comparison with the structural data at lower pressures shows that it is the longest Tl—O distances that diminish the most, while the short distances are relatively incompressible or even increase slightly. The fact that the spread of the Tl—O distances becomes smaller on compression to 5.82 GPa indicates that the coordination environments around the Tl atoms tend to become more uniform, due to the diminished (but nevertheless still existent) stereoactivity of the electron lone pairs.
| Table 1Selected geometric parameters (Å, °) |
When only the Tl—O distances below 3 Å are considered, the crystal structure under ambient conditions can be viewed as a stack of corrugated layers of cations and carbonate groups along the
a axis (Fig. 1). The suppression of the
E pairs results in the structure losing its layered character at 5.82 GPa. This is also reflected in the fact that the Tl

Tl distances between adjacent layers are considerably shortened with increasing pressure. Thus, the interlayer Tl1

Tl2 and Tl2

Tl2 distances are 3.588 (1) and 3.693 (1) Å, respectively, at ambient pressure, 3.50 (1) and 3.338 (8) Å, respectively, at 3.56 GPa, and 3.42 (2) and 3.26 (2) Å, respectively, at 5.82 GPa, indicating increasing Tl

Tl interactions between the layers on compression. These interactions might be responsible for the fact that the axial compressibility along the
a axis (within the estimated standard deviations) changes little between 3.56 and 5.82 GPa.
The other striking aspect of the high-pressure behaviour of Tl
2CO
3 is the rotation of the carbonate groups to accommodate the electron lone pairs (Fig. 1). The pressure-induced lattice contraction and changes in the orientation of the carbonate group in Tl
2CO
3 cause a decrease of the shortest C

C distance from 3.46 Å under ambient conditions (Marchand
et al., 1975
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
) to 2.4 (3) Å at 5.82 GPa. At the intermediate pressure of 3.56 GPa, this distance is 3.09 (16) Å (Grzechnik & Friese, 2008
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
). Since experimental data for the shortest C

C distances in
X
2CO
3 (
X = Li, Na, K, Rb, Cs or Tl) at higher pressures are not available, the result of this study can only be compared with the theoretical work by Cancarevic
et al. (2006
![[triangle]](/corehtml/pmc/pmcents/rtrif.gif)
), in which the C

C distances in high-pressure phases of Li
2CO
3 are expected to be below 2.5 Å.