Ea. Betterton, ON THE PH-DEPENDENT FORMATION-CONSTANTS OF IRON(III) SULFUR(IV) TRANSIENT COMPLEXES, Journal of atmospheric chemistry, 17(4), 1993, pp. 307-324
An experimental study is described of Fe(III)-S(IV) formation constant
s measured as a function of pH (1-3), ionic strength (0.2-0.5 M) and [
Fe(III)]T (2.5-5.0 x 10(-4) M) using a continuous-flow spectrophotomet
ric technique to make observations 160 ms after mixing. Preliminary ex
periments using pulse-accelerated-flow (PAF) spectrophotometry to meas
ure rate constants on a microsecond timescale are also described. The
conditional formation constant at 25-degrees-C can be modeled with the
following equation: K(app) = alpha1alpha4K7 + alpha0alpha4K8, where a
lpha0 = [Fe3+]/[Fe(III)]T, alpha1 = [FeOH2+]/[Fe(III)]T, alpha4 = [HSO
3-]/[S(IV)T], K7 = 8.5 x 10(2) M-1, and K8 = 5.5 x 10(1) M-1. K7 and K
8 can be interpreted as intrinsic constants for the coordination of HS
O -3 by FeOH2+ and Fe3+, respectively, but until further evidence is o
btained they should be regarded as fitting constants. PAF spectrophoto
metry showed that the initial reaction of Fe(III) with S(IV) (pH 2.0)
is characterized by a second-order rate constant of almost-equal-to 4
x 10(6) M-1 s-1 which is comparable to rate of reaction of FeOH2+ with
SO42-. However, the PAF results should be regarded as preliminary sin
ce unexpected features in the initial data indicate that the reaction
may be more complex than expected.