The kinetics of Cr(VI) reduction to Cr(III) by carbonate green rust were st
udied for a range of reactant concentrations and pH values. Carbonate green
rust, [(Fe4Fe2III)-Fe-IIl(OH)(12)][4H(2)O . CO3], was synthesized by induc
ed hydrolysis (i.e., co precipitation) of an Fe(III)/Fe(III) solution held
at a constant pH of 8. An average specific surface area of 47 +/- 7 m(2) g(
-1) was measured for five separate batches of freeze-dried green rust preci
pitate. Heterogeneous reduction by Fe(II) associated with the carbonate gre
en rust appears to be the dominant pathway controlling Cr(VI) loss from sol
ution. The apparent stoichiometry of the reaction between ferrous iron asso
ciated with green rust ([Fe(II)(GR)]) Cr(VI) was slightly higher than the e
xpected 3:1 ratio, possibly due to the presence of other oxidants, such as
oxygen, protons, or interlayer carbonate ions. The rate of Cr(VI) reduction
was proportional to the green rust surface area concentration, and psuedo-
first-order rate coefficients (k(obs)) ranging from 1.2 x 10(-3) to 11.2 x
10(-3) s(-1) were determined. The effect of pH was small with a 5-fold decr
ease in rate with increasing pH (from 5.0 to 9.0). At low COO concentration
s (< 200 muM), the rate of reaction was first order with respect to Cr(VI)
concentration, whereas, at high Cr(VI) concentrations, rates appear to devi
ate from first-order kinetics and approach a constant value. Estimated amou
nts of surface Fe(II) and total Fe(II) suggest that the deviation from firs
t-order kinetics observed at higher COO concentrations and the 50-fold decr
ease in rate observed upon three sequential exposures to Cr(VI) is due to e
xhaustion of available Fe(II).