Vanadate mineral

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Vanadate minerals are mineral species which contain both vanadium and oxygen. They usually also contain other cations, and may also contain other anions: however the mineral forms of the vanadium oxides navajoite (V2O5·3H2O), vanoxite (V6O13·8H2O) and lenoblite (V2O4·2H2O) are also classed as vanadate minerals.

Vanadium(V) is rather too large for tetrahedral coordination but rather small for octahedral coordination,[1][2] and vanadate minerals show a wide range of structural types, often of considerable complexity.

Vanadate minerals are unique among anion types in being divided between two primary classes in the Strunz classification. Minerals containing four-coordinate vanadium(V) are grouped with phosphate and arsenate minerals in class 08, while minerals containing five- and six-coordinate vanadium, which includes all minerals with vanadium(IV) or mixed oxidation states, are grouped as oxide minerals in class 04.

References

  1. Greenwood, Norman N.; Earnshaw, A. Chemistry of the Elements; Pergamon: Oxford, 1984; p 1144. ISBN 0-08-022057-6.
  2. Orgel, L. E. Ferroelectricity and the structure of transition-metal oxides. Faraday Soc. Dis. 1958, 26, 138–44.
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