Chemical elements
  Vanadium
    Isotopes
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    Physical Properties
    Chemical Properties
      Hypovanadous Oxide
      Vanadous Oxide
      Hypovanadic Oxide
      Vanadic Oxide
      Hypovanadous Fluoride
      Vanadous Fluoride
      Vanadium Tetrafluoride
      Vanadium Pentafluoride
      Vanadyl Difluoride
      Vanadium Oxytrifluoride
      Vanadium Dioxyfluoride
      Hypovanadous Chloride
      Vanadous Chloride
      Hypovanadic Chloride
      Divanadyl Chloride
      Vanadium Oxymonochloride
      Vanadyl Dichloride
      Vanadium Oxytrichloride
      Vanadium Oxydichloride
      Vanadous Bromide
      Hypovanadic Bromide
      Vanadium Oxymonobromide
      Vanadyl Dibromide
      Vanadium Oxytribromide
      Hydrated Vanadium Tri-iodide
      Vanadium Suboxide
      Hypovanadous Oxide
      Vanadous Oxide
      Hypovanadic Oxide
      Hypovanadates
      Intermediate Vanadium Oxides
      Vanado-vanadates
      Vanadium Pentoxide
      Orthovanadates
      Sodium Stannovanadates
      Vanadates
      Pyrovanadates
      Metavanadates
      Polyvanadates
      Double Vanadates
      Heteropoly-Acids with Vanadium
      Vanado-phosphates
      Molybdo-vanadophosphates
      Vanado-arsenates
      Molybdo-vanadoarsenates
      Tungsto-vanadoarsenates
      Molybdo-vanadates
      Tungsto-vanadates
      Uranyl-vanadates
      Molybdo-vanadosilicates
      Tungsto-vanadosilicates
      Vanado-selenites
      Vanado-tellurites
      Vanado-iodates
      Vanado-periodates
      Oxalo-vanadates
      Pervanadic Acid
      Pyropervanadates
      Orthopervanadates
      Vanadium Monosulphide
      Vanadium Trisulphide
      Vanadium Pentasulphide
      Vanadium Oxysulphides
      Hypovanadous Sulphate
      Vanadous Sulphate
      Vanadyl Sulphites
      Vanadyl Sulphates
      Vanadic Sulphates
      Vanadyl Dithionate
      Ammonium Orthothiovanadate
      Ammonium Pyroxyhexathiovanadate
      Sodium Orthoxytrithiovanadate
      Sodium Orthoxymonothiovanadate
      Vanadium Selenides
      Vanadyl Selenite
      Vanadyl Selenates
      Vanadium Subnitride
      Vanadium Mononitride
      Vanadium Dinitride
      Alkali Vanadyl Nitrites
      Vanadium Nitrates
      Vanadyl Hypophosphite
      Vanadyl Phosphates
      Vanadous Pyrophosphate
      Vanadyl Arsenates
      Vanadium Carbide
      Vanadyl Cyanide
      Potassium Vanadocyanide
      Potassium Vanadicyanide
      Vanadium Ferrocyanides
      Ammonium Vanadyl Thiocyanate
      Vanadium Subsilicide
      Vanadium Disilicide
      Vanadium Boride
    Detection, Estimation
    PDB 1b8j-2i4e
    PDB 2jhr-6rsa

Heteropoly-Acids with Vanadium






Vanadium possesses the property of entering into the composition of a large number of compounds which contain it as a constituent of a complex anion. Light has been thrown on the nature and constitution of these compounds by investigations into other heteropoly-acids, which are now found to be most satisfactorily formulated by the application of a modification of Werner's co-ordination theory first suggested by Miolati, and extended by Rosenheim and his co-workers. According to this theory the heteropoly-acids are produced by hydration of acids having the general formula H8-n[RnO4], where n represents the valency of the metal R. Thus, for example, in the cases of silicon and phosphorus the following schemes obtain:

H4[SiO4] + 2H2O = H8[SiO6].
H3[PO4] + 2H2O = H7[PO6].

Or, generally,

H8-n[RnO4] + 2H2O = H12-n[RnO6].

It will be observed that the basicity of each of these acids is determined by deducting the valency of the central atom in the complex anion from 12. The greatest number of oxygen atoms or other divalent radicals that can be co-ordinated with the central atom is 6; and this number usually holds good in a true compound, but not always. For example, the co-ordination number of the acid is only 4.

Substitution of the co-ordinated oxygen atoms by divalent radicals yields the various heteropoly-acids. The vanado-phosphates, for instance, axe derivatives of the hypothetical phosphato-acid H7[PO6], in which one or more of the oxygen atoms have been replaced by divalent (V2O6)' radicals. The compound to which the formula 7(NH4)2O.P2O5.12V2O5.26H2O has been ascribed from its analytical data thus becomes (NH4)7[P(V2O6)6].13H2O. If some of the oxygen atoms in the complex anion are replaced by (V2O6)' radicals and others by (Mo2O7)' radicals, the molybdovanado-phospliates are produced, e.g. and . Similarly, substitution by both (V2O6)' and (W2O7)' radicals gives rise to the tungstovanado-phosphates. The heteropolyvanado-arsenates are derived from the hypothetical arseno-acid H7[AsO6]. It has recently been shown that the arsenic in these compounds may undergo partial substitution by phosphorus to give rise to series of mixed crystals which are called heteropolyvanado-arseno phosphates or heteropolyvanado - phosphoarsenates. The heteropolyvanado-silicates are derived from the acid H8[SiO6].

The existence of such associated radicals as (V2O6)', (Mo2O7)', and (W2O7)' has been assumed in order to explain the very frequent occurrence of twelve (½V2O5), MoO3, or WO3 radicals in the complex anions of compounds the co-ordination number of which is six. A greater number than twelve has never been observed. As a rule only four of the oxygen atoms can undergo substitution by these associated radicals; thereafter an isomeric change appears to take place, thus:



Compounds are said to be saturated when all the oxygen atoms of the parent anion are replaced by metallic acid anions; unsaturated compounds contain some replaceable oxygen.

The decision as to which element forms the central atom of the complex anion depends on the fact that in any particular series of compounds the atomic proportions of the metals in the place of the co-ordinated oxygen will show very considerable variation when calculated for one atomic weight of the element which constitutes the central atom. Among the molybdo-vanadophosphates many are known which contain varying amounts of molybdenum and vanadium in combination with one gram-atom of phosphorus. Hydrogen also provides the nuclear atoms in some series, which are best viewed as derivatives of a hypothetical co-ordinated hexa-aquo-acid, H10[H2O6]. The vanado-tungstates (or tungsto-vanadates) are, for instance, represented by the general formula . Compounds of this type contain water of constitution.

It should be noted that vanadium does not as a rule form the central atom of the complex anion in the heteropoly-compounds. The oxalo-vanadates, however, most probably contain the anion , which is obtained by substituting two oxygen atoms in the anion of orthovanadic acid, i.e. the [VO4]'' ion by two (C2O4)' groups. Substitution by (MoO4)' groups gives rise to the oxalo-molybdovanadates of the general formula:

or .

Uranyl-vanadates, which are probably derived from uranyl-vanadic acid, , have also recently been prepared.

The constitution of many of the heteropoly-acids and of their salts may thus be explained, although direct proof of the correctness of some of these formulae is lacking. Some of the heteropoly-compounds of vanadium are, however, very complex, and cannot be represented by application of the foregoing scheme. To take an extreme instance, Rogers prepared a black, crystalline compound to which he ascribed the following formula:

99(NH4)2O.12P2O5.2As2O5.66V2O5.6V2O3.191WO3.522H2O.

The composition of these substances is necessarily a matter of doubt, because of the difficulty of conducting exact analyses of compounds of very high molecular weight; a small difference in the analytical data makes a large difference in the number of molecules. Further, the heteropoly-compounds are characterised by the ease with which they undergo hydrolysis; even the process of recrystallisation frequently produces a different complex.

In many cases the salts of any one series which have been analysed are not true compounds, but consist of isomorphous mixtures of simple chemical compounds; the composition of the mixtures varies with the composition, temperature, and acidity of the media from which they separate. This has been shown to apply to the molybdo-vanadates (or vanado-molybdates), molybdo-vanado phosphates, vanado-selenous acid and the vanado-selenites as well as to telluric acid and its salts. Recently, Canneri has succeeded in preparing a large number of mixed crystals of salts, and in some cases of the free acids, which belong to different series; for example, mixed crystals of tungsto-vanadophosphates and tungsto-vanadoar senates, of tungsto-vanado-phosphates and molybdo-vanadophosphates, of tungsto-vanadoar senates and molybdo-vanado arsenates; and, finally, mixed crystals of members of all the four series mentioned have been obtained. The mixed crystals have the same crystalline habit as that of their components, and complete isomorphism exists between any two series which mix in all proportions to form continuous series of mixed crystals containing four or five different oxygenated acid radicals. The crystallographic data of a number of ammonium tungsto-vanadoar senates have also recently been independently determined, and it has been shown that the crystal form is unaffected when the arsenic is substituted by phosphorus, or when the (W2O7)' radicals are partially substituted by (Mo2O7)'.

It appears probable that adsorption of uncombined radicals by molecules which contain a large number of these radicals, but which are not saturated, takes place, and that the only true chemical individuals are the maximum co-ordinated compounds. It has been shown that vanadium pentoxide forms a colloidal solution, in which state it is readily adsorbed.


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