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Title: Nitrous oxide emission from denitrification in stream and river networks

Journal Article · · Proceedings of the National Academy of Sciences
 [1];  [1];  [2];  [3];  [4];  [5];  [6];  [7];  [5];  [8];  [9];  [10];  [11];  [12];  [13];  [14];  [1];  [15];  [2];  [8] more »;  [16];  [1];  [2];  [3];  [10];  [11];  [6] « less
  1. University of Notre Dame, IN
  2. Michigan State University, East Lansing
  3. University of New Hampshire
  4. University of Wyoming, Laramie
  5. ORNL
  6. Marine Biological Laboratory
  7. Oregon State University, Corvallis
  8. University of New Mexico, Albuquerque
  9. Kansas State University
  10. Arizona State University
  11. Oregon State University
  12. University of Hew Hampshire
  13. Montana State University
  14. Virginia Polytechnic Institute and State University (Virginia Tech)
  15. Ball State University
  16. University of Georgia, Athens, GA

Nitrous oxide (N{sub 2}O) is a potent greenhouse gas that contributes to climate change and stratospheric ozone destruction. Anthropogenic nitrogen (N) loading to river networks is a potentially important source of N{sub 2}O via microbial denitrification that converts N to N{sub 2}O and dinitrogen (N{sub 2}). The fraction of denitrified N that escapes as N{sub 2}O rather than N{sub 2} (i.e., the N{sub 2}O yield) is an important determinant of how much N{sub 2}O is produced by river networks, but little is known about the N{sub 2}O yield in flowing waters. Here, we present the results of whole-stream {sup 15}N-tracer additions conducted in 72 headwater streams draining multiple land-use types across the United States. We found that stream denitrification produces N{sub 2}O at rates that increase with stream water nitrate (NO{sub 3}{sup -}) concentrations, but that <1% of denitrified N is converted to N{sub 2}O. Unlike some previous studies, we found no relationship between the N{sub 2}O yield and stream water NO{sub 3}{sup -}. We suggest that increased stream NO{sub 3}{sup -} loading stimulates denitrification and concomitant N{sub 2}O production, but does not increase the N{sub 2}O yield. In our study, most streams were sources of N{sub 2}O to the atmosphere and the highest emission rates were observed in streams draining urban basins. Using a global river network model, we estimate that microbial N transformations (e.g., denitrification and nitrification) convert at least 0.68 Tg {center_dot} y{sup -1} of anthropogenic N inputs to N{sub 2}O in river networks, equivalent to 10% of the global anthropogenic N{sub 2}O emission rate. This estimate of stream and river N{sub 2}O emissions is three times greater than estimated by the Intergovernmental Panel on Climate Change.

Research Organization:
Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
Sponsoring Organization:
USDOE Office of Science (SC)
DOE Contract Number:
DE-AC05-00OR22725
OSTI ID:
1005200
Journal Information:
Proceedings of the National Academy of Sciences, Vol. 108, Issue 1; ISSN 0027--8424
Country of Publication:
United States
Language:
English