期刊
WATER AIR AND SOIL POLLUTION
卷 197, 期 1-4, 页码 107-119出版社
SPRINGER INTERNATIONAL PUBLISHING AG
DOI: 10.1007/s11270-008-9794-9
关键词
Carbon stable isotopes; Dissolved inorganic carbon; Dissolved organic carbon; Naphthenic acids biodegradation; Nitrogen stable isotopes; Oil sands reclamation
资金
- Carbon Dynamics
- Food Web Structure & Reclamation Strategies in Athabasca Oil Sands Wetlands project (CFRAW)
- Syncrude Canada Ltd.
- Suncor Energy Inc
- Canadian Natural Resources Limited
- Albian Sands,
- Total S. A.
- Petro-Canada and Imperial Oil Limited
- Natural Sciences and Engineering Research Council of Canada and the Canadian Water Network
Naphthenic acids (NAs) are a complex group of naturally occurring oil sands constituents that constitute a significant portion of the dissolved organic carbon (DOC) pool available for microbial degradation in the process-related waste water associated with oil sands mine sites. One approach to understanding the biological fate of oil sands process-derived carbon and nitrogen in aquatic reclamation of the mine sites involves the use of stable isotope analyses. However, for stable isotope analyses to be useful in such field-based assessments, there is a need to determine how microbial degradation of a complex mixture of NAs might change the stable isotope values (delta C-13, delta N-15). In batch cultures and semi-continuous laboratory microcosms, utilization of a commercial mixture of NAs by oil sands-derived microbial cultures resulted in microbial biomass that was similar or slightly C-13 enriched (1.4aEuro degrees to 3.0aEuro degrees) relative to the DOC source, depending on the length of incubation. Utilization of a NA-containing extract of oil sands processed water resulted in greater C-13 enrichment of microbial biomass (8.5aEuro degrees) relative to the DOC source. Overall, the delta C-13 of the DOC comprised of complex mixtures of NAs showed minimal change (-0.5aEuro degrees to -0.1aEuro degrees) during the incubation period whereas the delta C-13 of the dissolved inorganic carbon (DIC) was more variable (-5.0aEuro degrees to +5.4aEuro degrees). In tests where the concentration of available nitrogen was increased, the final biomass values were N-15 enriched (3.8aEuro degrees to 8.4aEuro degrees) relative to the initial biomass. The isotope trends established in this study should enhance our ability to interpret field-based data from sites with hydrocarbon contamination, particularly in terms of carbon source utilization and N-15 enrichment.
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