Identifying the signature of the natural attenuation of MTBE in groundwater using molecular methods and "bug traps"
Abstract (Summary)
Natural attenuation through intrinsic bioremediation is the risk-based
management approach commonly used for gasoline (BTEX) contamination sites.
This approach has not yet been utilized for the fuel oxygenate methyl tertiarybutyl
ether (MTBE). MTBE is more resistant to biodegradation than BTEX.
MTBE is more abundant than benzene in oxygenated gasoline, has a greater
water solubility than BTEX, and sorbs weakly to soil. These properties
complicate developing a risk based management option to be implemented as
easily as for BTEX. The purpose of this project is to contribute to a growing
database containing information on MTBE contaminated sites nationwide with a
variety of environmental conditions. Characterizing a highly monitored MTBE
biodegradation site will determine the possible microbial “signature” of the natural
attenuation of MTBE. To correlate microbial community shifts with changes in
MTBE product patterns, “Bug traps” consisting of Ambersorb® Bio-Sep® beads
and regular Bio-Sep® beads were deployed into the polluted groundwater and
into control wells at a highly monitored service station to concentrate the
microorganisms for analysis. They were retrieved after 30 and 60 days of
deployment. Phospholipid fatty acid and nucleic acid analysis (denaturing
gradient electrophoresis (DGGE) and quantitative PCR) were used to analyze
the microbial community in the groundwater.
The samples from the plume showed a difference from the control samples.
Gram-negative communities in the samples closest to the plume did not show a
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lack of limiting nutrients (i.e. carbon) as did other wells further from the plume
and were in log growth phase. Also the Gram-negative community in the highest
contaminated well showed the highest adaptation to the environmentally stressful
conditions through decreased membrane permeability. The site showed
microbial and geochemical evidence for methanogenesis, which may have been
responsible for the observed degradation of MTBE and BTEX. Sulfate-reduction
was also evident throughout the site and may also have been a responsible
process for the observed biodegradation. Iron-reduction (Pelobacter, Geobacter)
was only evident in wells within the plume and downgradient of the plume and
may have played a role in degradation. In addition notable organisms that were
identified in other studies of MTBE biodegradation included Methylosinus
trichosporium OB3b, and environmental clones associated to the Flexibacter-
Cytophaga-Bacteroides phylum associated with hydrocarbon intrinsic
bioremediation. The results of this study provided evidence for anaerobic
biodegradation of MTBE.
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Bibliographical Information:
Advisor:
School:The University of Tennessee at Chattanooga
School Location:USA - Tennessee
Source Type:Master's Thesis
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