The reduction of Cr(VI) to Cr(III) decreases the toxicity and mobility
of chromium contaminants in soils and water. In addition, the formati
on of a highly insoluble Cr(III) product would decrease the likelihood
of future Cr(III) re-oxidation. Amorphous iron sulfide minerals like
mackinawite (FeS1-x) have the potential to reduce large quantities of
Cr(VI) and in the process form very stable [Cr, Fe](OH)(3) solids. In
this study, we examine the effectiveness of amorphous FeS as a reducta
nt of Gr(VI) by identifying the solution and solid-phase products of t
he reaction between FeS suspensions and chromate. Iron sulfide suspens
ions at pH 5.0, 7.0, and 8.0 were reacted with a range of Cr(VI) solut
ions from 50 to 5000 mu M in a N-2 atmosphere glovebox for 3 d. Soluti
ons were analyzed using ICP-AES, IC, and colorimetric methods; solids
were analyzed using XRD, TEM, EDS, and XANES spectroscopy. Iron sulfid
e removed all of the added Cr(VI) from solution for the reaction condi
tions studied and reduced between 85% and 100% of the Cr(VI) to Cr(III
). Chromate reduction occurred dominantly at the FeS surface and resul
ted in [Cr-0.75,Fe-0.25](OH)3; while less extensive, reduction of Cr(V
I) by Fe(II) (ag) was noted and produced a solid with the opposite Cr:
Fe ratio, [Cr-0.25,Fe-0.75](OH)(3).