This study is our first effort to obtain more information on the effec
ts of microbial activities on the mobilization/immobilization of radio
nuclides in geological environments. We used aerobic and anaerobic str
ains of bacteria to quantify interactions with U(VI). The quantificati
on of bioaccumulation by two strains of Thiobacillus ferrooxidans has
shown a slightly higher capability to accumulate U for T. ferrooxidans
ATCC 33020, isolated from a uranium mine, than for the type strain T.
ferrooxidans ATCC 23270(T), recovered from a coal mine. The amount of
accumulated uranium increased for both strains when the pH was increa
sed from 1.5 to 4.0. Extraction studies with EDTA showed that only a s
mall part of the accumulated uranium is adsorbed on the surface of the
cell walls whereas the main part is probably taken up by the cells. W
e also examined the U(VI) reduction of a sulfate-reducing bacterial st
rain (Desulfovibrio desulfuricans DSM 642(T)). In addition, we have st
udied one sulfate-reducing culture from a uranium mining waste pile (J
G 1). Kinetic studies with D. desulfuricans have shown that most of U(
VI) is reduced during the first 24 h. The yield of this microbial redu
ction depends strongly on the pH and increases from 10.3 to 99.2% when
the pH is increased from 3.1 to 6.2. In nature D. desulfuricans strai
ns occur in places where the pH is near neutral. (C) 1998 Elsevier Sci
ence S.A.