The OsO4F-, OsO4F22-, and OsO3F3- anions, their study by vibrational and NMR spectroscopy and density functional theory calculations, and the X-ray crystal structures of [N(CH3)(4)][OsO4F] and [N(CH3)(4)][OsO3F3]
M. Gerken et al., The OsO4F-, OsO4F22-, and OsO3F3- anions, their study by vibrational and NMR spectroscopy and density functional theory calculations, and the X-ray crystal structures of [N(CH3)(4)][OsO4F] and [N(CH3)(4)][OsO3F3], INORG CHEM, 39(19), 2000, pp. 4244-4255
The fluoride ion acceptor properties of OsO4 and OsO3F2 were investigated.
The salts [N(CH3)(4)][OsO4F] and [N(CH3)(4)](2)[OsO4F2] were prepared by th
e reactions of OsO4 with stoichiometric amounts of [N(CH3)(4)][F] in CH3CN
solvent, The salts [N(CH3)(4)][OsO3F3] and [NO][OsO3F3] were prepared by th
e Tractions of OsO3F2 With a stoichiometric amount of [N(CH3)(4)][F] in CH3
CN solvent and with excess NOF, respectively. The OsO4F-anion was fully str
ucturally characterized in the solid state by vibrational spectroscopy and
by a single-crystal X-ray diffraction study of [N(CH3)(4)][OsO4F]: Abm2, a
= 7.017(1) Angstrom, b = 11.401(2) Angstrom, c = 10.925(2) Angstrom, V = 87
4.1(3) Angstrom(3), Z = 4, and R = 0.0282 at -50 degrees C. The cis-OsO4F22
- anion was characterized in the solid state by vibrational spectroscopy, a
nd previous claims regarding the cis-OsO4F22- anion are shown to be erroneo
us. The fac-OsO3F3- anion was fully structurally characterized in CH3CN sol
ution by F-19 NMR spectroscopy and in the solid state by vibrational spectr
oscopy of its N(CH3)(4+) and NO+ salts and by a single-crystal X-ray diffra
ction study of [N(CH3)(4)][OsO3F3]: C2/c, a = 16.347(4) Angstrom, b = 13.47
5(3) Angstrom, c = 11.436(3) Angstrom, beta = 134.128(4)degrees V = 1808.1(
7) Angstrom(3), Z = 8, and R = 0.0614 at -117 DC. The geometrical parameter
s and vibrational frequencies of OsO4F-, Cis-OsO4F22-, monomeric OsO3F2, an
d fac-OsO3F3- and the fluoride affinities of OsO4 and monomeric OsO3F2 were
calculated using density functional theory methods.