1872
Can. J. Chem. Vol. 77, 1999
bonded to Sb(V) are observed. In addition, there is a sharp
fluorosulfato-antimonate(V) species can be extracted from
the signals in the F(S) region, and no assignment of reso-
nances in this region will be made.
singlet at ca. –162 ppm, which is attributed to SiF4(solv)
.
Apparently, there is a trace amount of HF that reacts with
SiO2, the main component of glass, to produce SiF4 accord-
ing to
In contrast, the F(Sb) region (d CFCl3 = –80~–150 ppm)
(see Fig. 3) provides a great deal of structural information.
The observed splitting of the signals results from the cou-
pling between non-equivalent fluorines bonded to the same
antimony atom. The complex spectral feature of this region
indicates complicated equilibria of various chemical species
in the system. The overlap of signals is sometimes so severe
that an analysis based solely on traditional 1D 19F NMR
spectra remains ambiguous. Even with the assistance of 2D
NMR methods, the spectral analysis is occasionally incon-
clusive.
[10] 4HF + SiO2 ® 2H2O + SiF4
The other product, H2O, is a strong base in the system and is
protonated to form the oxonium ion H3O+, which is observ-
able using 1H NMR spectroscopy. Its salt with weakly
nucleophilic [Sb2F11]– as the counter anion has been isolated
as discussed (22). The other possible route for the produc-
tion of H2O, dehydration of HSO3F according to
Significant signal broadening begins to be observed in the
[11] 2HSO3F W H2O + S2O5F2
spectra of the HSO3F–SbF5 system with xSbF ³ 0.500. The
5
is unlikely because the signal due to S2O5F2 at 47~48.5 ppm
(23, 24) is not observed in the 19F NMR spectra of all sam-
ples studied by us here. Evidence for reaction [10] also co-
mes from the visual observation of etching of NMR tubes
and capillary tubes after several weeks.
The mechanism for the generation of HF in magic acid is
not obvious. The observation of progressively increasing
spectra in the F(Sb) region of the systems with xSbF = 0.649
5
and 0.795 are dominated by broad peaks. Such signal broad-
ening precludes any detailed analysis in terms of individual
species. Therefore, the assignment of signals discussed in
the following sections will focus on the F(Sb) region in the
spectra of solutions with low SbF5 content (0.000 999 £ xSbF
5
³ 0.342). For the convenience, the following notation system
for the assignable signals in the F(Sb) region is used. The
signals in the F(Sb) region are labeled according to their
multiplicity: S for singlet, D for doublet, T for triplet, Q for
quartet, q for quintet, s for sextet, etc. For signals of the
same multiplicity, a number is attached in the order of their
appearance from low field to high field.
amounts of SiF4 with increasing xSbF in the system suggests
5
that the trace amounts of HF may be introduced as an impu-
rity in SbF5. However, as discussed in the following sec-
tions, partial solvolysis of SbF5 in HSO3F according to
[12] SbF5 + HSO3F W SbF4(SO3F) + HF
The increasing viscosity of the system, as the SbF5 con-
tent increases, may not be the only factor responsible for the
broadness of signals, because a number of relatively sharp
lines are also observed as well in the F(Sb) region. The
oligomeric structures of (SbF5)m and possibly H[SbmF5m(SO3F)]
or H[SbmF5m+1], as well as ligand exchange, may contribute
to the broadness of the signals. The sharp lines are probably
from some relatively small complex anions. Among these
sharp lines, the most intense signals labeled T3 and T6 can
be assigned to cis-[SbF4(SO3F)2]–, S8 to [SbF6]–, and Q1 to
[Sb2F11]–.
[13] SbF4(SO3F) + HSO3F W SbF3(SO3F)2 + HF
is a much more likely source for HF.
This proposal is based on the assumption that SbF5 or
SbF4(SO3F) are more readily solvolyzed by HSO3F than
coordinatively saturated anions like [SbF6]– and [SbF5(SO3F)]–.
Since SiF4 is also observed by 19F NMR spectroscopy for
the neat solvent HSO3F, it is also possible that some HF may
be formed by the self dissociation of HSO3F (K < 3 × 10–7):
[14] HSO3F W SO3 + HF
As reported previously (16–19), the proton exchange be-
tween the Sb(V) species and HSO3F appears to be rapid and
only averaged signals of both complex acids and their conju-
gate anions are observed in the 19F NMR spectra. For conve-
nience, the anionic formulation is used to represent both
forms in the discussion. The assignment of segments
(monomeric Sb(V) moieties), SbFn(SO3F)5–n m-(SO3F), and
m-(SO3F)SbFn(SO3F)4–n m-(SO3F), in the oligomeric species
will be discussed below. To distinguish the segments from
monomeric species (both complex acids and conjugate an-
ions), the segments are formulated as neutral fragments.
(see ref. 25) or may be present as an impurity in HSO3F. It is
not at all uncommon to observe SiF4 as well as BF3 in the
gas phase of freshly distilled HSO3F or introduced with
HSO3F as an impurity.
Figure 2 illustrates the 19F NMR spectra of pure HSO3F
and HSO3F–SbF5 systems with various xSbF values in the
5
F(S) region (d CFCl3 = 40~45 ppm).
In this region, all signals are singlets. For the solvent and
solutions with low SbF5 content, intense signals due to
HSO3F dominate the region. A main peak due to F-32SO3H
and a weak satellite peak due to F-34SO3H can be observed
(26, 27). For example, in the 1D 19F NMR spectrum of
fluorosulfuric acid (see Fig. 2), the very intense peak at
41.98 ppm and a weak satellite peak at 41.94 ppm are ob-
served. The isotope shift is 0.044 ppm, in agreement with
the previous studies (26, 27). For less intense F(S) signals,
the satellite peak (F-34SO3) is not observed. Long-range cou-
plings of the types 19F-S-O-Sb-19F and 19F-S-O-Sb-O-S-19F
are not observed for any samples in this study. Conse-
quently, little information about the structures of the fluoro-
Assignment of monomeric species
In the 19F NMR spectra (F(Sb) region) of the HSO3F–SbF5
system with xSbF = 0.000 999 (see Fig. 3a), there are a num-
5
ber of multiplets in addition to two singlets. Apparently, sev-
eral chemical species are present in the system. The possible
–
monomers of the type [SbFn(SO3F)6–n
Fig. 4.
]
are illustrated in
In these species, antimony(V) is assumed to be octahe-
drally coordinated by fluoro and fluorosulfato ligands.
© 1999 NRC Canada