Canadian Journal of Chemistry · 1983 · 117 citations · 1 references
Natural SciencesChemistryMaterials ScienceInorganic ChemistryMaterials ChemistrySpectroscopyCarbonate MineralsCrystal ChemistryInorganic MaterialsInorganic SpectroscopyMineral ChemistryRaman SpectroscopyHexagonal Crystal LatticesHexagonal LatticesHexagonal SymmetryInfrared SpectraPrimitive LatticesRaman SpectraSpectral FeaturesUnit Cell Symmetry
Four basic lead carbonates were prepared and identified by X-ray powder diffractometry. These were hydrocerussite (Pb 3 (OH) 2 (CO 3 ) 2 ), plumbonacrite (Pb 10 O(OH) 6 (CO 3 ) 6 ), and the two adducts MOH•2PbCO 3 (M = Na, K). New diffraction data are presented for the latter two compounds; they both have primitive hexagonal lattices with two formula units per unit cell. The unit cell dimensions of the sodium and potassium compounds are a = 5.273 ± 0.002 Å, c = 13.448 ± 0.005 Å and a = 5.348 ± 0.002 Å, c = 13.990 ± 0.005 Å, respectively. Six possible space groups are discussed.Raman and infrared spectra are reported for all four compounds, and compared with those of cerussite (PbCO 3 ); assignment of the spectral features is discussed. Vibrational spectra of the two MOH adducts indicate that they are isostructural, and that the structure contains a well-defined lead sub-lattice, consistent with the X-ray data. The spectra of hydrocerussite and plumbonacrite indicate that lead is present as oxygen-bridged polymeric moieties in these solids. The carbonate ions occupy two and three independent sites in hydrocerussite and plumbonacrite, respectively.
1