Acid-volatile sulfide (AVS) has been shown to be the dominant phase re
acting with metals in anoxic sediments. The AVS in sediment decreases
upon resuspension due to storms and dredging, and in winter when the r
ate of aeration processes exceeds that of the formation of sulfide. We
conducted a series of lab aeration experiments in batch reactors to i
nvestigate the effects of aeration of sediment on the sulfide content
of sediment and on the partitioning of cadmium, a model toxic metal, t
o the sediment. Aeration of sediment results in rapid decrease of the
AVS. We studied the sediment characteristics for aeration periods of a
pproximately a month. During this time, the concentrations of dissolve
d metals increased by 200 to 400% or more, relative to the concentrati
ons present at the beginning of the test. The concentration of metal a
ssociated with AVS and with pyrite decreased. During the aeration, the
re are increases in the concentrations of hydrous iron and manganese o
xides, and these materials become increasingly more important in the b
inding of cadmium. Following the aeration, >50% of the cadmium was ass
ociated with the extractable iron and manganese components of the sedi
ment. Overall, the binding capacity of the sediments for cadmium decre
ased after aeration.