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Crystal Chemical Aspects of Vanadium: Polyhedral Geometries, Characteristic Bond Valences, and Polymerization of (VO<i><sub>n</sub></i>) Polyhedra
245
Citations
36
References
2000
Year
Materials ScienceInorganic ChemistryEngineeringCharacteristic Bond ValencesChemical BondPhysical ChemistryOrganic ChemistryPolyhedral GeometriesCrystal Chemical AspectsBond LengthsChemistryVanadyl BondCoordination PolymerOrganometallic PolymerCrystallographyCrystal Structure DesignBinary LinkagesLinear Chain Compound
The distribution of bond lengths in (V3+O6) polyhedra shows a maximum between 1.98 and 2.04 Å, and limits of 1.88 and 2.16 Å, respectively. The bond lengths in (V4+On) and (V5+On) (n = 5, 6) polyhedra show distinct populations which allow us to define the following types of bonds: (1a) vanadyl bonds in (V4+On) polyhedra, shorter than 1.74 Å; (1b) vanadyl bonds in (V5+O5) polyhedra, shorter than 1.76 Å; (1c) vanadyl bonds in (V5+O6) polyhedra, shorter than 1.74 Å; (2a) equatorial bonds in (V4+On) polyhedra, in the range 1.90 to 2.12 Å; (2b) equatorial bonds in (V5+O5) polyhedra, longer than 1.76 Å; (2c) equatorial bonds in (V5+O6) polyhedra with one vanadyl bond, in the range 1.74 to 2.10 Å; (2d) equatorial bonds in (V5+O6) polyhedra with two vanadyl bonds, in the range 1.80 to 2.00 Å; (3a) trans bonds in (V4+O6) polyhedra, longer than 2.10 Å; (3b) trans bonds in (V5+O6) polyhedra with one vanadyl bond, longer than 2.15 Å; (3c) trans bonds in (V5+O6) polyhedra with two vanadyl bonds, longer than 2.025 Å. The average equatorial bond length in (V4+On) and (V5+On) polyhedra can be used to calculate the mean valence state of V in mixed-valent structures. We define characteristic bond valences for vanadyl, equatorial, and trans bonds in different coordinations and examine which binary linkages are possible and which linkages occur in minerals and synthetic compounds. Here, V5+−O−V5+, V5+−O−V4+, and V4+−O−V4+ linkages between vanadyl−trans and equatorial−equatorial bonds occur often in synthetic compounds, whereas the corresponding V4+−O−V4+ linkages are rare in minerals.
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