Hcb. Hansen et Cb. Koch, REDUCTION OF NITRATE TO AMMONIUM BY SULFATE GREEN RUST - ACTIVATION-ENERGY AND REACTION-MECHANISM, Clay Minerals, 33(1), 1998, pp. 87-101
Iron(II)-containing minerals are potential inorganic nitrate reductant
s in soils and sediments. Specifically, synthetic green rust (Fe4IIFe2
III(OH)(12)SO4 . yH(2)O, GR) reduces nitrate to ammonium. The reaction
of GR with two different nitrate salts, NaNO3 and Ba(NO3)(2), has bee
n compared. The reaction stoichiometry and the reaction order with res
pect to Fe(II) in GR does not change in the examined temperature range
(15-50 degrees C), irrespective of the nitrate salt used. Activation
energies of 83.9 +/- 7.6 kJ mol(-1) and 90.5 +/- 6.9 kJ mol(-1) have b
een determined for the reaction of GR with NaNO3 and Ba(NO3)2, respect
ively. However, for the latter reaction the rate of reaction is increa
sed 40 times. Based on X-ray and Mossbauer investigations, this accele
ration of the reaction rates is attributed to the forced exchange of s
ulphate with nitrate in GR interlayers caused by precipitation of BaSO
4 outside the GR particles, a reaction which does not occur in the pre
sence of NaNO3. This difference in anion exchange behaviour is confirm
ed by anion exchange experiments with the redox-inactive GR-analogue,
pyroaurite. A reaction model initiated by nitrate electrostatically bo
und at positively charged sites of GR is proposed.