Catalyzed Reduction of Nitrite by Dithionite and Sulfoxylate
tant from the copper cofactor. Comparison of this structure
with a refined nitrite-bound crystal structure indicates how
coordination can change between copper-oxygen and
copper-nitrogen during catalysis.
Despite the significant progress in the understanding of
the mechanisms of catalytic nitrite reductions, several
problems remain unresolved. One of them is how the type
of reductant influences the rate of the overall reduction of
nitrite and the composition of the products. In continuation
of our studies on the reactions catalyzed by metallophtha-
locyanines, here we report kinetic data and their mechanistic
interpretation for the reaction between sodium nitrite and
sodium dithionite or sulfoxylate in the presence of iron(III)
phthalocyanine. Thiourea dioxide (TDO) served as a precur-
sor of sulfoxylate.16 The reported data demonstrate the
distinctive differences in the reactivity of sulfoxylate and
dithionite and enable a comparison of the role of iron and
cobalt phthalocyanines in the catalytic reduction of nitrite.
Figure 1. UV-vis spectra of FeIII(TSPc)3- (8.6 × 10-6 M, solid line),
FeII(TSPc)4- (8.6 × 10-6 M, dashed line), FeI(TSPc)5- (6.2 × 10-6 M,
dotted line), and FeI(TSPc•)6- (4.3 × 10-6 M, thick solid line) at pH 13
(0.1 M KOH).
Experimental Section
recorded were limited by the dead time of the stopped-flow
instrument at higher dithionite concentrations and tempera-
tures), i.e.,
Materials. Sodium nitrite, sodium dithionite (85% grade), and
thiourea dioxide (TDO) were obtained from Aldrich and used as
received. Iron(III) phthalocyanine was prepared and purified using
a literature method.17 BIS-TRIS, TRISINE, and CHES buffers were
used to control the pH. Na15NO2 (95% 15N grade) was used for
15N NMR analysis. Oxygen-free nitrogen was used to deoxygenate
solutions. Ultrapure water was used in all measurements.
Kinetic Measurements and Instrumentation. Conventional
kinetic experiments were performed on a Cary 1 or Cary 5 UV-
vis spectrophotometer under anaerobic conditions. No salt was
added to control the ionic strength. The data were analyzed using
Origin 6.1 and SPECFIT software. A thermostated ((0.1 °C)
Applied Photophysics SX 18MV stopped-flow spectrophotometer
with an optical path length of 1.0 cm was used to follow the faster
reactions. High-pressure stopped-flow experiments were performed
at pressures up to 130 MPa on a custom-built instrument described
previously18 and analyzed with the OLIS KINFIT (Bogart, GA,
1989) set of programs. 15N NMR measurements were performed
using a Bruker Avance DRX 400 WB spectrometer equipped with
a superconducting BS-94789 magnet system at 40.56 MHz. 15N
chemical shifts were referenced externally to neat nitromethane.
D2O (99%) was used as a solvent for all NMR measurements.
2-
kobsd1 ) k1[S2O4
]
(1)
The value of k1 at pH 8.06 and 25 °C is (2.63 ( 0.09) ×
10-3 M-1 s-1. The first-order dependence on dithionite
2-
concentration indicates that direct reduction of - by S2O4
-
occurs and does not involve the monomeric species SO2
formed in reaction 2. Further mechanistic information can
-
S2O42- a 2SO2
(2)
be obtained from the thermal activation parameters which
were determined from the Eyring plot over the temperature
range 5-30 °C. The values of ∆H* and ∆S* were found to
be 46 ( 3 kJ mol-1 and +23 ( 11 J K-1 mol-1, respectively.
2-
-
It is known that both S2O4 and SO2 , in general, act as
outer-sphere reductants.19,20 Our data do not contradict this
2-
conclusion. Although such a reduction by S2O4 is not
common21 (more frequently, the actual reductant is the sulfur
-
dioxide anion radical SO2 ), it occurs, for example, in
Results and Discussion
3- 23
ferricytochrome c,22 Fe(CN)6
,
and some CoIII com-
plexes.19
Reaction of Sodium Dithionite with Iron Tetrasulfo-
phthalocyanine. The reaction of an excess of sodium
dithionite with iron tetrasulfophthalocyanine, FeIII(TSPc)3-,
is accompanied by two consecutive color changes. The first
is a very fast change from green to blue. An intense
absorption maximum appears at 671 nm (Figure 1). This
spectrum is essentially identical to that reported11 for
FeII(TSPc)4-. The rate of reduction of the FeIII complex was
found to show a linear dependence on the dithionite
concentration (Supporting Information Figure S1; the data
The second reduction step is accompanied by a color
change of the solution from blue to brown and is much
slower than the first. Absorbance maxima at 480 and 712
nm appear with simultaneous disappearance of the maximum
at 671 nm (Figure 1). This spectrum is very close to that
reported for FeI tetrasulfophthalocyanine.11 The rate of
reduction of the FeII complex determined from the increase
2- 0.5
in the absorbance at 480 nm depends linearly on [S2O4
]
( Supporting Information Figure S2). This observation shows
(16) Makarov, S. V.; Kudrik, E. V.; van Eldik, R.; Naidenko, E. V. J. Chem.
Soc., Dalton Trans. 2002, 4074.
(17) Weber, J. N.; Busch, D. H. Inorg. Chem. 1965, 4, 469.
(18) (a) van Eldik, R.; Palmer, D. A.; Schmidt, R.; Kelm, H. Inorg. Chim.
Acta 1981, 50, 131. (b) van Eldik, R.; Gaede, W.; Wieland, S.; Kraft,
J.; Spitzer, M.; Palmer, D. A. ReV. Sci. Instrum. 1993, 64, 1355.
(19) Mehrotra, R. N.; Wilkins, R. G. Inorg. Chem. 1980, 19, 2177.
(20) Tobe, M. L.; Burgess, J. Inorganic Reaction Mechanisms; Longman
Inc.: New York, 1999; p 475.
(21) Tsukahara, K.; Wilkins, R. G. J. Am. Chem. Soc. 1985, 107, 2632.
(22) Lambeth, D. O.; Palmer, G. J. Biol. Chem. 1973, 248, 6095.
(23) Scaife, C. W. J.; Wilkins, R. G. Inorg. Chem. 1980, 19, 3244.
Inorganic Chemistry, Vol. 44, No. 18, 2005 6471