The reactive iron monosulfides including mackinawite are known for their ab
ility to scavenge trace metals. Oxidation and reduction reactions in sedime
nts and the types of metal bonding with mackinawite determine both the stab
ility of the metal bonds and the susceptibility of the material to oxidatio
n. Metal retention is important because it influences the availability of t
oxic metals to aquatic organisms. In this study, Pb and Cd interactions wit
h mackinawite were investigated, and two major retention mechanisms were su
ggested. They are, first, that Pb and Cd displace up to 29% of the Fe from
mackinawite by forming (Pb,Fe)S and (Cd,Fe)S on the surface of the mackinaw
ite and, second, that 0.91 mmol/g of Ph and 2.03 mmol/g of Cd are adsorbed
on the surface of the transformed mackinawite. The mixed ferrous sulfides a
re more insoluble and more stable than the pure mackinawite, while surface
adsorption is a relatively weak and labile retention mechanism. Both reacti
ons contributed toward a drop in pH, although the mackinawite containing Pb
and Cd was stable at this lower pH.