B.M. Gray et al. / Polyhedron 29 (2010) 1630–1638
1637
identified as a cationic vanadyl (VIV) complex of the diphosphine
4. Conclusions
dioxide [VO(H2O){o-C6H4(P(O)Me2)2}2]Cl2ꢀ3H2O, formed through
a sequence of hydrolysis and oxidation reactions. The vanadium
is six-coordinate, bonded to one V@O (1.601(3) Å), two chelating
diphosphine dioxides (V–O = 1.992(2)–2.119(3) Å) which are dis-
posed cis with chelate angles (87.3(1) and 81.8(1)°). The coordina-
tion sphere is completed by a water molecule (the H’s were readily
identified in the electron density map) with V–OH2 = 2.045(3) Å.
The V@O is slightly longer than that in the square pyramidal [VO-
Cl2(OPPh3)2] (1.584(5) Å) [44]. The IR spectrum shows a strong
V@O stretch at 995 cmꢁ1 and several PO stretches, while the UV–
Vis spectrum shows weak d–d transitions in the visible region
and the onset of charge transfer bands > ꢂ25 000 cmꢁ1, typical of
vanadyl complexes containing oxygen donor ligands [38].
The formation of tertiary arsine adducts of VCl4 has been con-
firmed, contrasting with the discredited reports of phosphine ana-
logues. Adducts of VCl3 have also been prepared as reduction
products of the same reactions, including the first structurally
authenticated VIII arsine [V2Cl6{o-C6H4(AsMe2)2}2]. Hydrolysis of
the VIV complexes proceeds via vanadyl–arsine complexes, which
can be obtained pure by reaction of [VOCl2(thf)2(H2O)] with the li-
gands. In contrast, the very strongly coordinating diphosphine, o-
C6H4(PMe2)2, instantly reduces VCl4 even at low temperatures.
The different behaviour of the phosphine and arsine ligands re-
flects the stronger reducing power of the former. However, the
vanadyl diphosphine complex [VOCl2{o-C6H4(PMe2)2}], is readily
obtained showing the stability conferred upon the VIV centre by
the V@O linkage. The VIV complexes undergo complex decomposi-
tion in thf solution exposed to air, the final products being identi-
fied in the case of the diphosphine as a vanadyl diphosphine
dioxide, [VO(H2O){o-C6H4(P(O)Me2)2}2]Cl2, whereas [VCl4{o-
C6H4(AsMe2)2}x] decompose with chlorination of the arsenic ligand
3.5. Hydrolysis of VIV arsine complexes
Comparison of the IR and UV–Vis spectra of [VOCl2{j
2-MeC-
(CH2AsMe2)3}(H2O)] (above), with those obtained from the green
solids made by reacting VCl4 and MeC(CH2AsMe2)3 in ‘‘laboratory
grade” CCl4 without taking any precautions to exclude moisture,
to the cation [o-C6H4(AsMe2Cl)(l
-O)(AsMe2)]+, and cis-[VOCl2-
(H2O)3] is also produced.
and also by exposing solid [VCl4{j
2-MeC(CH2AsMe2)3}] briefly to
air, exhibit similar features, showing that [VOCl2{MeC(CH2As-
Me2)3}(H2O)] is a significant component of the products. However,
the products are not obtained in a pure state by hydrolysis, and
prolonged exposure to air resulted in blue oils. The [VCl4{o-
C6H4(AsMe2)2}n] (n = 1 or 2) also become green in moist air and
eventually blue oils result. When either [VCl4{o-C6H4(AsMe2)2}n]
(n = 1 or 2) are stirred in thf solution exposed to air, the initial
brown solutions turn green and then blue, and removal of the sol-
vent, followed by washing the sticky blue residues with diethyl
ether affords blue powders which are, on the basis of their IR spec-
tra, assigned as VOCl2 with water or thf as co-ligands, and do not
contain any arsenic ligands. Blue crystals have been obtained on
several occasions from the reaction solutions, but mostly gave very
weak diffraction patterns. In one case the structure of a deep blue
crystal (Fig. 6) showed it to contain co-crystallised oxidised/halo-
Acknowledgements
We thank RCUK and EPSRC for support, STFC for access to the
GEM diffractometer at ISIS through the GEM Express service
(XB990042), and Dr R. I. Smith for collecting the PND data.
Appendix A. Supplementary material
CCDC 757918, 757919, 757920, 757921, and 757922 contain
the supplementary crystallographic data for compounds. These
Data Centre, 12 Union Road, Cambridge CB2 1EZ, UK; fax: (+44)
1223-336-033; or e-mail: deposit@ccdc.cam.ac.uk. Supplementary
data associated with this article can be found, in the online version,
genated diarsine cation [o-C6H4(AsMe2Cl)(l
-O)(AsMe2)]+ and cis-
[VOCl2(H2O)3]. The latter is a distorted octahedral molecule with
cis chlorines, a short V@O (1.588(2) Å) and three facially bound
water molecules with the longest V–OH2 trans to the vanadyl unit.
Although [VOCl2ꢀxH2O] (x usually unspecified) is a well known
starting material [1] and there are several structurally authenti-
cated adducts of [VOCl2(H2O)2], this seems to be the first structural
characterisation of the tris(aquo) species The bond lengths are all
slightly longer than in the five-coordinate [VOCl2(H2O)2]ꢀ2Et2O
(which also has trans Cl’s) [30] or [VOCl2(H2O)2ꢀL] (L = 15-crown-
5 or 18-crown-6) [45,46], and the nearest analogue is mer-cis-
[VOCl2(MeOH)3] [30]. The previously unknown organoarsenic(V)
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1
[o-C6H4(AsMe2Cl)(l-O)(AsMe2)]2[VOCl4]. C20H32As4Cl6O3V, RMM = 883.78,
monoclinic, space group P21/n, Z = 2, T = 120 K. Cell dimensions: a = 8.2495(10),
b = 8.6904(10), c = 22.132(4) Å, b = 98.254(10)°, U = 1570.3(4) Å3. k = 0.71073 Å,
18 278 reflections measured, 3 596 unique reflections, Rint = 0.033. R1
[Io > 2r(Io)] = 0.030, wR2 (all data) = 0.065.