ChemInform Abstract: Pb2Fe2Ge2O9, the Germanate Analogue of the Silicate Mineral Melanotekite.
โ Scribed by J. BARBIER; D. LEVY
- Publisher
- John Wiley and Sons
- Year
- 2010
- Weight
- 32 KB
- Volume
- 29
- Category
- Article
- ISSN
- 0931-7597
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โฆ Synopsis
Pb 2 Fe 2 Ge 2 O 9 , the Germanate Analogue of the Silicate Mineral Melanotekite.
-Single crystals of the title compound are prepared by reaction of MgFe 2 Ge 2 O 8 (prereacted at 1398 K) and GeO 2 in a PbO/B 2 O 3 flux (1323 K, 5 h). The single crystal of composition Pb 2 Fe 1.78 Ge 2.11 Mg 0.11 O 9 crystallizes in the orthorhombic space group Pbcn with Z = 4. The structure exhibits an unsymmetrical splitting of the Pb site and a strong anisotropy of the bridging O atom of the Ge 2 O 7 group, which was also observed in the mineral melanotekite, Pb 2 Fe 2 Si 2 O 9 . These structural features can be associated with the stereoactivity of the Pb 2+ lone pairs, which is more pronounced in the silicate structure. -(BARBIER,
๐ SIMILAR VOLUMES
1997 structure structure (solids and liquids) D 2000 ## 19 -013 Crystal Structures of the Tellurates Pb3Fe2Te2O12 and Pb2CoTeO6. -Single crystals of the title compounds are prepared by reaction of PbO and Fe2O3 or CoO in a TeO2 flux (corundum crucible, air, 730 โข C, 48 h). Pb3Fe2Te2O12 crystalliz