HR: 0800h
AN: B51A-0186    [Abstracts]
TI: Nitrogen Inputs and Transformations in a Boreal Wetland: Hypotheses and Preliminary Results From the Alaska Peatland Experiment (APEX)
AU: * Millar, N
EM: millarn@msu.edu
AF: Michigan State University, Department of Plant Biology, East Lansing, MI 48824-1312 United States
AU: O'Donnell, J A
EM: ftjao1@uaf.edu
AF: University of Alaska-Fairbanks, Institute of Arctic Biology, Fairbanks, AK 99775-7000 United States
AU: Turetsky, M R
EM: mrt@msu.edu
AF: Michigan State University, Department of Plant Biology, East Lansing, MI 48824-1312 United States
AB: High latitudes are expected to experience some of the most dramatic effects of climate change in the near future. This is already evident from existing permafrost and air temperature records in Alaska. Peatlands are a major component of boreal landscapes and store massive reservoirs of soil organic carbon (C) and nitrogen (N), yet the vulnerability of these organic matter stocks to climate change is poorly understood. While some field studies have focused on N cycling in bogs, little is known about N inputs and transformations within boreal fens. We recently initiated a large scale manipulation of soil temperature and water table in a moderately rich fen situated near the Bonanza Creek LTER site, outside Fairbanks, Alaska (the Alaska Peatland Experiment or APEX; www.apex.msu.edu). As part of this experiment, we hypothesized that water table height regulates microbial reduction - oxidation (redox) reactions in organic soils. This may alter the potential for nitrification and denitrification, and therefore, concentrations of ammonium (NH₄⁺), and nitrate (NO₃^-), and fluxes of nitrous oxide (N₂O) in fen ecosystems. Denitrification however, may be limited by low NO₃^- concentrations in this fen, which is dominated by a mix of herbaceous species, brown mosses, and Sphagnum. We also hypothesized that warming would increase N transformation rates by stimulating heterotrophic microbial activity, leading to variation in N mineralization rates and N availability.

We established three water table plots (control, raised, lowered), each about 120 m² in area. Water table levels at the lowered and raised plots were manipulated using drainage ditches and solar powered pumping techniques, respectively, and were kept at between 5-10 cm below and at 5 cm above the control plot. At 3 of the 6 sub plots within each water table plot, we constructed replicate open top chambers (OTCs) to passively increase surface temperatures by about 1 ° C.

In the first season of measurements at the APEX, our initial results suggest that higher water table levels increase atmospheric N₂O concentrations above the soil surface (400 ± 3 and 380 ± 7 ppbv, at raised and lowered water table level, respectively). We also measured lower dissolved N₂O concentrations in soil water (37 and 4 ppbv at raised and lowered water table level, respectively at 100 cm depth). Here, we will present interactions between thermal and moisture regimes in the experimental fen in relation to N balance, by quantifying concentrations of various N species (e.g., NH₄⁺, NO₃^-, N₂O, TDN, DON, DIN) in the soil, water and atmosphere. This work will help define the role of N availability and N transformations in boreal peatland ecosystems in feedbacks to global climate change.
UR: http://apex.msu.edu
DE: 0426 Biosphere/atmosphere interactions (0315)
DE: 0469 Nitrogen cycling
DE: 0475 Permafrost, cryosphere, and high-latitude processes (0702, 0716)
DE: 0497 Wetlands (1890)
DE: 1615 Biogeochemical cycles, processes, and modeling (0412, 0414, 0793, 4805, 4912)
SC: Biogeosciences [B]
MN: Fall Meeting 2005