Buy article online - an online subscription or single-article purchase is required to access this article.
Recently, there has been substantial interest in the new high-pressure polymorphs of GeO2 synthesized in the laboratory. Previous investigators reported the synthesis of `CaCl2-type', `α-PbO2-type' and `pyrite-type (modified-fluorite-type)' GeO2 at pressures of 30–130 GPa in laser-heated diamond anvil cells. In order to provide definitive information about the new high-pressure polymorphs, we performed Rietveld refinements of the structures. The structure refinements confirm that two of these high-pressure phases do have the α-PbO2-type and pyrite-type (modified-fluorite-type) structures.
Supporting information
| Crystallographic Information File (CIF) https://doi.org/10.1107/S0108768103021761/ws0004sup1.cif Contains datablocks RIETAN_publ, I_phase_1, I_phase_2, II_phase_1, II_phase_2, II_phase_3, III_phase_1, III_phase_2, III_phase_3, I_p_01, II_p_01, III_p_01 |
| Rietveld powder data file (CIF format) https://doi.org/10.1107/S0108768103021761/ws0004Isup2.rtv Contains datablock I |
| Rietveld powder data file (CIF format) https://doi.org/10.1107/S0108768103021761/ws0004IIsup3.rtv Contains datablock II |
| Rietveld powder data file (CIF format) https://doi.org/10.1107/S0108768103021761/ws0004IIIsup4.rtv Contains datablock III |
(I_phase_1) germanium dioxide
top
Crystal data top
GeO2 | b = 4.2024 (7) Å |
Mr = 104.61 | c = 2.8039 (4) Å |
Orthorhombic, Pnnm | V = 50.08 (1) Å3 |
a = 4.2499 (7) Å | Z = 2 |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Ge1 | 0.0 | 0.0 | 0.0 | 0.35* | |
O1 | 0.304 (5) | 0.292 (6) | 0.0 | 0.35* | |
Crystal data top
Pt | a = 3.8072 (6) Å |
Mr = 195.08 | V = 55.19 (2) Å3 |
Cubic, Fm3m | Z = 4 |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Pt1 | 0.0 | 0.0 | 0.0 | 1.0* | |
(II_phase_1) germanium dioxide
top
Crystal data top
GeO2 | b = 5.0269 (6) Å |
Mr = 104.61 | c = 4.5223 (6) Å |
Orthorhombic, Pbcn | V = 92.11 (2) Å3 |
a = 4.0519 (6) Å | Z = 4 |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Ge1 | 0.0 | 0.169 (1) | 0.25 | 2.9 (7)* | |
O1 | 0.211 (5) | 0.895 (3) | 0.400 (2) | 2.9 (7)* | |
(II_phase_2) sodium chloride
top
Crystal data top
ClNa | a = 2.8600 (3) Å |
Mr = 58.44 | V = 23.39 (1) Å3 |
Cubic, Pm3m | Z = 1 |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Na1 | 0.0 | 0.0 | 0.0 | 0.983* | |
Cl1 | 0.5 | 0.5 | 0.5 | 0.983* | |
(II_phase_3) platinum
top
Crystal data top
Pt | a = 3.7381 (4) Å |
Mr = 195.08 | V = 52.23 (1) Å3 |
Cubic, Fm3m | Z = 4 |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Pt1 | 0.0 | 0.0 | 0.0 | 0.983* | |
(III_phase_1) germanium dioxide
top
Crystal data top
GeO2 | a = 4.3365 (15) Å |
Mr = 104.61 | V = 81.55 (5) Å3 |
Cubic, Pa3 | Z = 4 |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Ge1 | 0.0 | 0.0 | 0.0 | 0.446 (9)* | |
O1 | 0.3417 (16) | 0.3417 (16) | 0.3417 (16) | 0.446 (9)* | |
(III_phase_2) rhenium
top
Crystal data top
Re | c = 4.162 (9) Å |
Mr = 186.21 | V = 24.42 (6) Å3 |
Hexagonal, P63/mmc | Z = 2 |
a = 2.6029 (16) Å | |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Re1 | 0.33333 | 0.66667 | 0.25 | 0.446 (9)* | |
(III_phase_3) platinum
top
Crystal data top
Pt | a = 3.647 (1) Å |
Mr = 195.08 | V = 48.51 (2) Å3 |
Cubic, Fm3m | Z = 4 |
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2) top | x | y | z | Biso*/Beq | |
Pt1 | 0.0 | 0.0 | 0.0 | 0.446 (9)* | |
Subscribe to Acta Crystallographica Section B: Structural Science, Crystal Engineering and Materials
The full text of this article is available to subscribers to the journal.
If you have already registered and are using a computer listed in your registration details, please email
support@iucr.org for assistance.