4.6 Article

Examining the Microbial Degradation of Naphthenic Acids Using Stable Isotope Analysis of Carbon and Nitrogen

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

  1. Carbon Dynamics
  2. Food Web Structure & Reclamation Strategies in Athabasca Oil Sands Wetlands project (CFRAW)
  3. Syncrude Canada Ltd.
  4. Suncor Energy Inc
  5. Canadian Natural Resources Limited
  6. Albian Sands,
  7. Total S. A.
  8. Petro-Canada and Imperial Oil Limited
  9. Natural Sciences and Engineering Research Council of Canada and the Canadian Water Network

向作者/读者索取更多资源

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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