A microbial community stimulated for in situ bioremediation of uranium-contaminated groundwater at the Old Rifle site in Rifle, Colorado. This aquifer community demonstrates sequential reduction processes following acetate biostimulation at 1-3 mM concentrations. The community transitions through distinct metabolic phases: Phase I (days 0-50) dominated by Geobacter species (up to 89% of community) performing Fe(III) reduction coupled to U(VI) reduction, achieving 70% uranium removal within 50 days and reducing concentrations below the EPA treatment goal of 0.18 μM in some wells. Phase II (>50 days) shifts to sulfate-reducing bacteria including Desulfobacteraceae (45% by day 80), Desulfosporosinus, and Desulfotomaculum acetoxidans as Fe(III) becomes depleted. Geobacter metallireducens and Anaeromyxobacter dehalogenans reduce soluble U(VI) to insoluble U(IV), forming biogenic uraninite nanoparticles that immobilize uranium. Desulfovibrio species contribute to uranium reduction through enzymatic pathways while generating hydrogen sulfide that can chemically reduce uranium. This represents the first successful field demonstration of uranium bioremediation via stimulating subsurface Geobacter populations, providing an alternative to pump-and-treat remediation. Groundwater flow rate is 0.82 m/day, creating dynamic conditions where microbial metabolism must outpace uranium advection.
Taxonomy
| Taxon | Ontology ID | Functional Roles | Abundance |
|---|---|---|---|
| Geobacter species | NCBITaxon:28232 |
PRIMARY_DEGRADER
SYNTROPHIC_PARTNER
|
DOMINANT |
| Anaeromyxobacter dehalogenans | NCBITaxon:161493 |
SYNTROPHIC_PARTNER
|
COMMON |
| Desulfovibrio vulgaris | NCBITaxon:881 |
SECONDARY_FERMENTER
SYNTROPHIC_PARTNER
|
COMMON |
| Desulfosporosinus species | NCBITaxon:79206 |
SECONDARY_FERMENTER
|
COMMON |
| Desulfobacteraceae family | NCBITaxon:213118 |
PRIMARY_DEGRADER
|
DOMINANT |
Ecological Interactions
Acetate Oxidation Coupled to Fe(III) and U(VI) Reduction
CROSS_FEEDINGSource Taxon: Geobacter species
Metabolites: acetate (CHEBI:30089), uranium(VI) (CHEBI:37119), uranium(IV) (CHEBI:33395), Fe(III) (CHEBI:29034), Fe(II) (CHEBI:29033)
Biological Processes:
- oxidation-reduction process (GO:0055114)
- acetate catabolic process (GO:0045733)
Evidence
-
PMID:14532040 - SUPPORT (IN_VIVO)"As the acetate injection continued over 50 days there was a loss of sulfate from the groundwater and an accumulation of sulfide and the composition of the microbial community changed"
-
PMID:14532040 - SUPPORT (IN_VIVO)"Within 50 days uranium had declined below the prescribed treatment level"
-
PMID:14532040 - SUPPORT (IN_VIVO)"At 17 days after the start of the acetate injection Geobacteraceae accounted for 89% of the groundwater microbial community"
Uranium Immobilization via Uraninite Formation
MUTUALISMMetabolites: uranium(IV) (CHEBI:33395)
Biological Processes:
- oxidation-reduction process (GO:0055114)
Evidence
-
PMID:14532040 - SUPPORT (IN_VIVO)"Analysis of 16S ribosomal DNA (rDNA) sequences and phospholipid fatty acid profiles demonstrated that the initial loss of uranium from the groundwater was associated with an enrichment of Geobacter species in the treatment zone"
Hydrogen-Mediated U(VI) Reduction by Anaeromyxobacter
SYNTROPHYSource Taxon: Anaeromyxobacter dehalogenans
Metabolites: dihydrogen (CHEBI:18276), uranium(VI) (CHEBI:37119), uranium(IV) (CHEBI:33395)
Biological Processes:
- oxidation-reduction process (GO:0055114)
Evidence
-
PMID:18843300 - SUPPORT (IN_VITRO)"Thirty-four c-type cytochrome genes were upregulated in the sediment-grown cells, including several genes that are homologous to cytochromes that are required for optimal Fe(III) and U(VI) reduction by G"
Sulfate Reduction and Chemical U(VI) Reduction
CROSS_FEEDINGSource Taxon: Desulfobacteraceae family
Metabolites: sulfate (CHEBI:16189), hydrogen sulfide (CHEBI:16136), uranium(VI) (CHEBI:37119), uranium(IV) (CHEBI:33395)
Biological Processes:
- sulfate reduction (GO:0019419)
- oxidation-reduction process (GO:0055114)
Evidence
-
PMID:14532040 - SUPPORT (IN_VIVO)"Organisms with 16S rDNA sequences most closely related to those of sulfate reducers became predominant, and Geobacter species became a minor component of the community"
Community Succession from Metal to Sulfate Reduction
COMPETITIONMetabolites: Fe(III) (CHEBI:29034), sulfate (CHEBI:16189)
Biological Processes:
- oxidation-reduction process (GO:0055114)
Evidence
-
PMID:14532040 - SUPPORT (IN_VIVO)"As the acetate injection continued over 50 days there was a loss of sulfate from the groundwater and an accumulation of sulfide and the composition of the microbial community changed"
-
PMID:14532040 - SUPPORT (IN_VIVO)"Fe(III) is depleted, sulfate is reduced, and sulfate-reducing bacteria predominate"
Environmental Factors
| Factor | Value | Unit |
|---|---|---|
| pH | ~7 | pH units |
| Oxygen Availability | Anaerobic after acetate amendment | qualitative |
| Acetate Concentration | 1-3 | mM |
| Groundwater Flow Rate | 0.82 | m/day |
| Initial Uranium Concentration | 0.4-1.4 | μM |
| Time to Uranium Removal | 9-50 | days |