Shorafa and Seppelt
are passivated with elemental fluorine for several hours, filled with
dry argon, and then transferred to a drybox for use. The drybox of
the M. Braun Co., Germany, has water and O2 contents of less
than 1 ppm.
then attached to a metal vacuum line to remove traces of volatiles.
The autoclave was transferred to the drybox, opened there, and a
green material was scraped off the lid and stored in PFA containers.
Os2O3F7: 600 mg (2 mmol) of OsO4 and 900 mg (2.5 mmol)
and OsF6 are reacted as described above, except at 170 °C for 24
h. Green, crystalline material, mp 121.3°. IR (Nujol, cm-1): 997.9
m, 954.3 s, 668.0 s, 638.1 s, 527 s. Raman spectrum (cryst., cm-1):
997(15), 966(100), 711(30), 694(10), 652(10), 625(5), 606(3), 488-
(5,br), 374(60), 311(2), 276(5), 266(5), 230(2), 215(2), 119(20).
OsOF5: 377 mg (1.5 mol) of OsO4 mg and 1039 mg (4.2 mmol)
of OsF6 are reacted as described above at 230 °C for 24 h. All
volatile materials were removed between -20 and -30 °C within
10-15 min. Pure OsOF5 is obtained by sublimation at room
temperature into a PFA trap at -196 °C.
Attempts to prepare OsF7: 1000 mg (5.26 mmol) of osmium
metal powder was heated at 620 °C with 10 mL of fluorine in an
80 mL monel autoclave. The product was pumped directly at 600
°C through a 4 mm PFA tube that was cooled to -196 °C while
excess F2 was pumped away immediately. The tube was sealed off
at both ends, and the Raman spectrum was taken from the yellow
sublimate (OsF6). The pressure of F2 in the autoclave was calculated
assuming ideal gas behavior to be about 400 bar. To check this
value by an experiment, the autoclave has been equipped with a
pressure gauge and filled with the same molar amount (10 mL) of
Ar. The physical properties of Ar and F2 are very similar (bp, critical
data, mol wt), and indeed the measured pressure of 420 bar Ar is
very close to the calculated pressure of F2.
Single crystals were grown from dry HF by slow cooling from
0 to -78 °C over a period of 2-3 days. Crystals have also been
obtained by sublimation. Crystals were handled under nitrogen
cooling to approximately -140 °C in a special device,17 and with
this mounted on a Bruker SMART CCD 1000 TU diffractometer,
using Mo KR irradiation, a graphite monochromator, a scan width
of 0.3° in ω, and a measuring time of 10 or 20 s per frame. Each
compound was measured up to 2θ ) 61° by 1800 frames (OsOF5
up to 2θ ) 86° and 3600 frames), covering a full sphere.
Semiempirical absorption corrections (SADABS) were used by
equalizing symmetry-equivalent reflections. Because the refractive
power of the compound was high, very small crystals (0.02 mm)
were chosen, to minimize absorption effects. The structures were
solved and refined with the SHELX programs.18
Calculations. The program package GAUSSIAN 03 has been
used.14 Basis sets: Os, Re: Electron core potentials for 60 core
electrons from Institut fu¨r Theoretische Chemie, Universita¨t Stut-
tgart, and scalar relativistically corrected basis sets 8s7p6d for
valence electrons. F, O: 6-31+G(d,p) and aug-cc-pVTZ basis sets,
as implemented in the GAUSSIAN program. B3LYP-DFT cal-
culations according to Becke20 in the version of Lee, Yang, and
Parr,21 and coupled cluster calculations, CCSD(T), all as imple-
mented in the GAUSSIAN Program.
Raman spectra were recorded on a Bruker RFS 100 FT-Raman
spectrometer.
Results and Discussion
OsO3F. The osmium(VII) oxide fluoride with the highest
oxygen content would be OsO3F. There is only one report
about its possible existence.9 A colorless crystalline material
has been obtained from OsF6 by reaction with glass and has
considerable volatility. The single-crystal structure determi-
nations could not distinguish between OsO3F and OsO2F2.
It has existed in two crystallographic modifications, mono-
clinic, C2/c, and cubic, P4h3n. In the meantime, the crystal
structures of OsO4 and RuO4 have been (re)investigated,22-24
and the data for OsO4 are identical to those of the claimed
OsO3F/OsO2F2, see Table 1, including all positional param-
eters. Also, the colorless nature and volatility of the
compound in question point to OsO4. We have often
observed that OsF6 and the oxide fluorides convert eventually
to OsO4 in the case of slow hydrolysis. According to our
calculations, molecular OsO3F is a minimum on the potential
hypersurface. Its structure is quite distorted from ideal C3V
symmetry; it has only Cs symmetry, see Figure 1. This is
further evidence that the material obtained in 1974 was not
OsO3F.
OsO4 has been purchased from Chempur, Karlsruhe, Germany,
and used without further purification. OsF6 is prepared from osmium
powder and excess elemental fluorine in an 80 mL monel autoclave
at 250 °C. HF was redistilled in a metal vacuum line and stored
over BiF5.
OsO2F3: OsO4 (140 mg, 0.59 mmol) was loaded into an 80 mL
stainless steel autoclave in the drybox. OsF6 (169.5 mg, 0.56 mmol)
is condensed onto the OsO4 at -196 °C with the help of a metal
vacuum line. The autoclave was allowed to warm to room
temperature and then heated for 16-20 h at 150 °C. At the end of
the reaction, the autoclave was cooled to room temperature and
(17) Kottge, T.; Stalke, G. J. Appl. Crystallogr. 1996, 29, 465-468.
(18) Sheldrick, G. H. SHELXS-93, Program for Crystal Structure Solution;
Universita¨t Go¨ttingen: Go¨ttingen, Germany, 1986 and 1993.
(19) Frisch, M. J.; Trucks, G. W.; Schlegel, H. B.; Scuseria, G. E.; Robb,
M. A.; Cheeseman, J. R.; Montgomery, J. A., Jr.; Vreven, T.; Kudin,
K. N.; Burant, J. C.; Millam, J. M.; Iyengar, S. S.; Tomasi, J.; Barone,
V.; Mennucci, B.; Cossi, M.; Scalmani, G.; Rega, N.; Petersson, G.
A.; Nakatsuji, H.; Hada, M.; Ehara, M.; Toyota, K.; Fukuda, R.;
Hasegawa, J.; Ishida, M.; Nakajima, T.; Honda, Y.; Kitao, O.; Nakai,
H.; Klene, M.; Li, X.; Knox, J. E.; Hratchian, H. P.; Cross, J. B.;
Adamo, C.; Jaramillo, J.; Gomperts, R.; Stratmann, R. E.; Yazyev,
O.; Austin, A. J.; Cammi, R.; Pomelli, C.; Ochterski, J. W.; Ayala, P.
Y.; Morokuma, K.; Voth, G. A.; Salvador, P.; Dannenberg, J. J.;
Zakrzewski, V. G.; Dapprich, S.; Daniels, A. D.; Strain, M. C.; Farkas,
O.; Malick, D. K.; Rabuck, A. D.; Raghavachari, K.; Foresman, J.
B.; Ortiz, J. V.; Cui, Q.; Baboul, A. G.; Clifford, S.; Cioslowski, J.;
Stefanov, B. B.; Liu, G.; Liashenko, A.; Piskorz, P.; Komaromi, I.;
Martin, R. L.; Fox, D. J.; Keith, T.; Al-Laham, M. A.; Peng, C. Y.;
Nanayakkara, A.; Challacombe, M.; Gill, P. M. W.; Johnson, B.; Chen,
W.; Wong, M. W.; Gonzalez, C.; Pople, J. A. Gaussian 03, revision
B.04; Gaussian, Inc.: Pittsburgh, PA, 2003.
Table 1. Crystallographic Data of Claimed OsO3F or OsO2F2,3 in
17,19
18
Comparison to OsO4
and RuO4
modification
OsO3F/OsO2F2
OsO4
RuO4
a (pm)
b (pm)
c (pm)
â (deg)
a (pm)
C2/c
942
449.1
860
117.5
859.5
937.4(4)
451.5(2)
863.0(3)
116.58(4)
856.8(1)
930.2(4)
439.6(1)
845.4(4)
116.82(3)
850.9(1)
(20) Becke, A. D. J. Chem. Phys. 1993, 98, 5648.
P4h3n
(21) Lee, C.; Yang, W.; Parr, R. G. Phys. ReV. B 1988, 37, 785.
(22) Krebs, B.; Hasse, K. Acta Crystallogr., Sect. B 1976, 32, 1334-1337.
(23) Play, M.; Wickleder, M. S. J. Solid State Chem. 2005, 178, 3206-
3209.
(24) Play, M., Wickleder, M. S.; Shorafa, H.; Seppelt, K. Unpublished
results.
OsO2F3. OsO2F3 is a green sublimable material, first
prepared in 1975. No conclusive structure has been presented,
even in the most detailed description,11 although elemental
7930 Inorganic Chemistry, Vol. 45, No. 19, 2006