Irangu et al.
to measure directly the Cu(II/I) self-exchange rate in AN.
ylferrocene (Alfa Inorganics) were used as supplied. Ferrocene
9
(
Strem Chemicals) was purified by sublimation. The copper content
of the various products was determined by iodimetry.
Tetraaquacopper(II) triflate [Cu(OH (F CSO ] (I) was pre-
In fact, Manahan reported in 1967 that radiochemical tracer
-
1
methods gave a self-exchange rate constant of g0.3 M
s
-1
2
)
4
3
3 2
)
in AN. This value seems anomalously large as compared
pared typically by adding 5.0 mL (26.5 mmol) of 5.3 M triflic acid
to a slurry of 1.04 g (13.0 mmol) of cupric oxide in 25 mL of
water. The mixture was heated at ∼60 °C until the solid had
dissolved, and then filtered and evaporated to dryness on a steam
bath. The blue, crystalline product was redissolved in a minimum
volume of water on the steam bath and recrystallized by cooling.
This product was dissolved in acetonitrile (∼10 mL) and precipi-
tated with ether, filtered, and washed with ether and dried in air.
to more recent estimates in water, and this was confirmed
in our preliminary experiments which failed to detect any
Cu(I) NMR line broadening in the presence of Cu(II).
However, before attempting any direct measurements, it
obviously would be helpful to have some idea of the
magnitude of the rate of Cu(II/I) exchange to choose the
appropriate experimental method and time scale.
6
3
The present work describes experiments to estimate the
Cu(II/I) electron exchange rate in AN by applying the Marcus
cross-relationship to the reduction of Cu(II) with ferrocene
2 6 8 10 2
Anal. Calcd for CuC F H O S : Cu, 14.65; C, 5.54; H, 1.86.
Found: Cu, 14.50; C, 5.20; H, 1.67.
1
Anhydrous Cu(II) triflate, Cu(F CSO ) (II), was obtained as a
3
3 2
fine, white hygroscopic powder by heating the tetrahydrate salt in
(Fc) and 1,1′-dimethylferrocene (Dmfc) in AN/water mix-
air at ∼100 °C. This solid was stored in a vial with a plastic cap
tures. Reactions of ferrocenes are generally thought to be
outer-sphere, and necessary background information is
in a desiccator. Anal. Calcd for CuC
Found: Cu, 17.6; C, 6.30.
2 6 6 2
F O S : Cu, 17.5; C, 6.64.
+
available from studies of the Cu(II) and ferrocinium ion (Fc )
3 4 3 3
Tetraacetonitrilecopper(I) triflate [Cu(NCCH ) ](F CSO ) (III)
reduction potentials in AN/water mixtures by Cox and co-
17
was prepared by a modification of the methods by Ogura and
workers10 and the electron self-exchange studies in AN of
18
Jenkins and Kochi. A mixture containing 50 mL of acetonitrile,
+
11-13
+ 11
the Fc/Fc
and Dmfc/Dmfc
couples. In the present
1.0 g (2.3 mmol) of I, and 0.3 g (4.7 mmol) of copper foil was
stirred in a capped parafilm-sealed Erlenmeyer flask until the
solution turned colorless. Filtration on a 4-8 µ sintered glass frit
gave a clear solution. Addition of anhydrous ether produced a white
powder, which was collected by filtration under argon. Argon was
sucked through the product until it looked reasonably dry, and then
study, the driving force for the reaction is varied by changing
the reductant, but primarily by changing the AN/water
composition, and the variation of the rate will be analyzed
in terms of Marcus theory to obtain an estimate of the Cu-
(II/I) self-exchange rate constant.
it was sealed under argon. Anal. Calcd for CuC
9 3 12 4 3
F H N O S: Cu,
The speciation of solvated Cu(II) ions in AN/water solu-
16.86; N, 14.87; C, 28.69; H, 3.21. Found: Cu, 17.10; N, 14.18;
tions was studied by Funahashi and co-workers14 for [H
O]
between 0 and 0.84 M (98.5% AN), and they reported for-
2
C, 27.64; H, 2.98.
The Cu(II) solvates, [Cu(H O) (NCCH ) ](F CSO ) (IV) and
2 2 3 2 3 3 2
2
+
mation of [Cu(OH
2
)
n
+
(NCCH
3
)
6-n
]
(n ) 0-3) with
3 4 3 3 2
[Cu(NCCH ) (F CSO ) ] (V), were obtained as blue crystals by
[
Cu(OH
2
)
2
(NCCH
3
)
4
]2 as the dominant species for [H
2
O]
slow evaporation of acetonitrile solutions of the tetrahydrate (I)
and the anhydrous (II) Cu(II) triflates, respectively. The crystals
from the solution of the tetrahydrate were obtained in an air
atmosphere, whereas those from the solution of the anhydrous salt
were obtained under an argon atmosphere. Single crystals for the
structure determination were selected from the solution-crystal
mixture in the X-ray crystallography laboratory.
The AN/water solvent was made by transferring an appropriate
volume of doubly distilled water, and sometimes standardized aque-
ous perchloric or triflic acid, to a 500 mL or 1.00 L volumetric flask
and diluting to volume with AN (99.7% or 99.5%). Therefore, the
as low as 0.5 M (∼99% AN). For Cu(I), the formation
15
constants determined by Kamau and Jordan suggest that
+
Cu(OH
2
)(NCCH
3
)
3
is the dominant species for >50% AN,
+
but the point at which this converts to Cu(NCCH
)
3 4
is uncer-
16
63
tain. Our study of Cu(I) NMR line widths in AN revealed
that there is significant line broadening for >0.5 M H
gesting the formation of at least some Cu(OH
2
O, sug-
)(NCCH )
3 3
+
2
at this point, and that the latter is the dominant species for
the 50-97.5% AN of this study. The electrochemical studies
of Cox and co-workers10 show that the Cu(II/I) reduction
potential increases smoothly with increasing % AN (50-
%
AN refers to volume percentage. The acid added was prepared by
diluting the concentrated acid with doubly distilled water and analy-
zed by titration with 0.100 M NaOH. The mixed solvents were
stored in volumetric flasks and used within 2 days. The densities
and molarities as a function of volume % AN are given in the
Supporting Information.
100%) and do not suggest any abrupt change in species.
Experimental Section
Materials. Acetonitrile (Caledon, Fisher or BDH), perchloric
acid (Fisher), trifluoromethanesulfonic acid (triflic acid, Aldrich),
copper(II) nitrate trihydrate (Allied Chemicals), and l,1′-dimeth-
For kinetic studies, stock solutions of Cu(II) were prepared by
dissolving ∼1.0 g (∼2.3 mmol) of (I) or ∼0.6 g (∼2.5 mmol) of
Cu(NO
3
)
2
2
‚3H O in 50.0 mL of the appropriate solvent. The Cu(II)
(
8) Ahrland, S.; Nilsson, K.; Tagesson, B. Acta Chem. Scand. 1983, 37A,
93.
9) Manahan, S. E. Can. J. Chem. 1967, 45, 2451.
1
content was determined by standard iodimetry. Aliquots from these
solutions were diluted to 25.0 mL with the solvent and used for
the kinetic runs.
(
(
10) Cox, B. G.; Jedral, W.; Palou, J. J. Chem. Soc., Dalton Trans. 1988,
733.
Solutions of Fc and Dmfc were prepared by dissolving weighed
amounts of Fc (∼10 mg) or Dmfc (∼11 mg) in the appropriate
solvent in 25.0 mL volumetric flasks. Next, 10.0 mL aliquots of
these solutions were diluted in 50.0 mL with the same solvent to
give stock solutions for the kinetic runs.
(
(
11) Yang, E. S.; Chan, M.-S.; Wahl, A. C. J. Phys. Chem. 1980, 84, 3094.
12) Kirchner, K.; Dang, S.-Q.; Stebler, M.; Dodgen, H. W.; Wherland,
S.; Hunt, J. P. Inorg. Chem. 1989, 28, 3604.
(13) McManis, G. E.; Nielson, R. M.; Gochev, A.; Weaver, M. J. J. Am.
Chem. Soc. 1989, 111, 5533 and references there in.
(14) Inamo, M.; Kamiya, N.; Inada, Y.; Nomura, M.; Funahashi, S. Inorg.
Chem. 2001, 40, 5636.
(
(
15) Kamau, P.; Jordan, R. B. Inorg. Chem. 2001, 40, 3879.
16) Irangu, J.; Jordan, R. B. Inorg. Chem. 2003, 42, 3934.
(17) Ogura, T. Transition Met. Chem. 1976, 1, 179.
(18) Jenkins, C. L.; Kochi, J. K. J. Am. Chem. Soc. 1972, 94, 843.
1620 Inorganic Chemistry, Vol. 44, No. 5, 2005