Proof of concept was obtained that Fe(O) can stoichiometrically reduce
nitrate to ammonium and that cathodic hydrogen [produced during anaer
obic Fe(O) corrosion by water] can sustain microbial denitrification t
o reduce nitrate to more innocuous products (i.e., N2O and N-2). Autot
rophic, denitrifying growth on Fe(O) was proven through the use of a d
ual-flask apparatus. Cathodic H-2 from a flask containing Fe(O) was al
lowed to diffuse to another (anoxic) flask containing a pure culture o
f Paracoccus denitrificans, where denitrification and microbial growth
were observed. Nitrate reduction and end product distribution were st
udied in batch reactors amended with either steel wool or Fe(O) powder
. Steel wool, with a smaller specific surface area, was less reactive,
and its corrosion did not significantly increase the pH of the soluti
on. This allowed for a greater participation of denitrifiers in the ni
trate removal process, which increased nitrate removal rates and trans
formed a greater portion of the added nitrate to innocuous gases rathe
r than to ammonium. Combining denitrifiers with the more reactive Fe(O
) powder did not increase removal rates or decrease the proportion of
nitrate reduced to ammonium. This was attributed to a corrosion-induce
d increase in pH above the tolerance range of the bacteria (pH > 10).
Nitrate removal was sustained over 4 months in flow-through columns pa
cked with steel wool and seeded with autotrophic denitrifiers. Increas
ing the hydraulic retention time from 0.67 to 2.33 days increased the
nitrate removal efficiency and decreased the fraction of nitrate reduc
ed to ammonium. The finding that Fe(O) can sustain autotrophic denitri
fication may have practical applications to treat nitrate-contaminated
waters in exsitu or in-situ reactive filters.