HR: 0800h
AN: B11C-0624    [Abstracts]
TI: Influence of Electron Donor Type and Concentration on Microbial Population Structure During Uranium Reduction and Remobilization
AU: * Daly, R A
EM: rdaly@berkeley.edu
AF: Department of Plant and Microbial Biology, University of California, Berkeley, CA 94720,
AU: Brodie, E L
EM: elbrodie@lbl.gov
AF: Earth Sciences Division, Lawrence Berkeley National Lab, Berkeley, CA 94720,
AU: Kim, Y
EM: ymkim@lbl.gov
AF: Earth Sciences Division, Lawrence Berkeley National Lab, Berkeley, CA 94720,
AU: Wan, J
EM: jmwan@lbl.gov
AF: Earth Sciences Division, Lawrence Berkeley National Lab, Berkeley, CA 94720,
AU: Tokunaga, T
EM: tktokunaga@lbl.gov
AF: Earth Sciences Division, Lawrence Berkeley National Lab, Berkeley, CA 94720,
AU: DeSantis, T Z
EM: tzdesantis@lbl.gov
AF: Earth Sciences Division, Lawrence Berkeley National Lab, Berkeley, CA 94720,
AU: Andersen, G L
EM: glandersen@lbl.gov
AF: Earth Sciences Division, Lawrence Berkeley National Lab, Berkeley, CA 94720,
AU: Hazen, T C
EM: tchazen@lbl.gov
AF: Earth Sciences Division, Lawrence Berkeley National Lab, Berkeley, CA 94720,
AU: Firestone, M K
EM: mkfstone@nature.berkeley.edu
AF: Department of Environmental Science, Policy and Management, University of California, Berkeley, CA 94720,
AB: Enhanced reductive precipitation of U(VI) through stimulation of indigenous microorganisms is an attractive, low- cost strategy for in-situ remediation of contaminated groundwaters and sediments. The rate of organic carbon (OC) supply determines not only the amount of electron donor available for bioreduction of U(VI), but also affects the resulting concentration of aqueous (bi)carbonate generated by microbial respiration. Increased (bi)carbonate concentrations drive aqueous U(VI) concentrations to higher levels and make U(IV) oxidation under reducing conditions favorable. We designed a long-term column study to investigate the effects of different OC forms and supply rates on the stability of bioreduced U and on the structure and dynamics of the microbial communities. OC was supplied as acetate or lactate at four different concentrations and columns were sampled at three time points. In the columns receiving high OC supply the time points correspond to a phases of net U-reduction, U(IV) reoxidation and U(VI) remobilization, and stable levels of U mobilization. DNA was extracted from column sediments, 16S rRNA genes were amplified and the communities analyzed using a high-density phylogenetic microarray (PhyloChip). Lactate and acetate supplied at equivalent rates had a similar impact on uranium mobility with higher OC resulting in re-oxidation of U(IV) after an initial period of U(VI) reduction. Similarly, organic carbon (OC) supply rate, not OC form, had the largest impact on microbial community structure. The diversity (richness) of bacterial and archaeal communities increased over time with those receiving lactate having higher initial richness. Known U-reducing bacteria were present in all columns and time points, however the dynamics of these organisms varied with both organic carbon supply rate and form. This data demonstrates that the initial rate of electron donor supply during heavy metal remediation strongly impacts microbial community development. Uranium re-mobilization occurred irrespective of electron donor form, and this occurred despite the presence of multiple species of U-reducing bacteria.
DE: 0418 Bioremediation
DE: 0448 Geomicrobiology
DE: 0465 Microbiology: ecology, physiology and genomics (4840)
SC: Biogeosciences [B]
MN: 2007 Fall Meeting