HR: 11:00h
AN: NB42F-03    [Abstracts]
TI: Nitrogen Retention in the Riparian Zone of Watersheds Underlain by Discontinuous Permafrost in Interior Alaska
AU: * ODonnell, J A
EM: ftjao1@uaf.edu
AF: Insitute of Arctic Biology,, University of Alaska Fairbanks, Fairbanks, AK 99775 United States
AU: Jones, J B
EM: ffjbj@uaf.edu
AF: Insitute of Arctic Biology,, University of Alaska Fairbanks, Fairbanks, AK 99775 United States
AB: Riparian zones function as important ecotones for reducing nitrate concentration in ground water and inputs into streams. In the boreal forest of interior Alaska, permafrost confines subsurface flow through the riparian zone to shallow organic horizons, where plant uptake of nitrate and denitrification are typically high. Two research questions were addressed in this study: 1) how does riparian zone nitrogen retention vary in watersheds underlain by discontinuous permafrost, 2) what is the contribution of denitrification to riparian zone nitrogen retention? To estimate the contribution of the riparian zone to watershed nitrogen retention, we analyzed groundwater chemistry using an end-member mixing model. To assess the importance of denitrification as a mechanism of nitrogen retention, we conducted field denitrification assays using the acetylene block technique. Nitrogen retention averaged 8.9 and 5.7 mgN m^-2 d^-1 in low and high permafrost watersheds, respectively, over the summer. Compared with the fluvial export of nitrogen, the retention rate of nitrogen in the riparian zone is 10 - 15% of the loss rate in stream flow. Denitrification accounted for a small proportion (3%) of nitrogen retention in the riparian zone. The interaction between permafrost, hydrology, and biological processes appears to enhance riparian nitrate retention in this system.
DE: 1615 Biogeochemical processes (4805)
SC: North American Benthological Society [NB]
MN: 2005 Joint Assembly