Jm. Harrington et al., BIOTIC GENERATION OF ARSENIC(III) IN METAL(LOID)-CONTAMINATED FRESH-WATER LAKE-SEDIMENTS, Environmental science & technology, 32(16), 1998, pp. 2425-2430
Sediments of Coeur d'Alene Lake, ID, are heavily contaminated with min
e tailings that contain high levels of arsenic, iron, lead, and other
trace elements. Maximal abundance of redox-active elements such as As
and Fe is generally found close to the sediment-water interface, where
as peak abundance of less redox-active elements such as Pb is found at
>25 cm. The suggestion that As is mobile within reduced sediments led
us to characterize the sediment microbiota with regard to organisms w
hose activities favor As mobilization. Most probable number (MPN) esti
mates reveal that the densities of cultivable sulfate-, iron-, and ars
enate-reducing bacteria approach 10(6), 10(5), and 10(4) cells g(-1) w
et weight sediment, respectively. Because As is considered more mobile
in environments that produce As(lll), we measured aqueous As(lll) gen
eration within As(V)-amended sediment microcosms. In organic acid-stim
ulated microcosms, > 50% of a 10mM As(V) amendment is transformed to A
s(III), compared to 30% and 5% in unstimulated microcosms and abiotic
controls, respectively. in microcosms amended with an inhibitor of SRB
metabolism (molybdate), As(V) reduction was in some cases diminished,
suggesting that SRB may contribute to As(V) reduction. The capacity f
or biotic As(V) reduction clearly exists in CDAL sediments, and the pr
ofile of As abundance may be partly attributed to metal(loid)-transfor
ming bacteria.