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Published on: February 25, 2021
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Upper Midwest lakes are supersaturated with N2.
Brianna M Loeks1, James B Cotner2
1Department of Ecology Evolution and Behavior, University of Minnesota, St. Paul, MN 55108 loek0003@d.umn.edu.
Summary
Freshwater lakes continuously release nitrogen gas to the atmosphere, challenging the idea that they primarily gain nitrogen. This suggests terrestrial inputs are crucial for balancing lake nitrogen cycles.
Area of Science:
- Environmental Science
- Limnology
- Biogeochemistry
Background:
- Gaseous nitrogen (N2) exchange in freshwater systems is poorly understood.
- N2 cycling is vital for aquatic ecosystems, involving nitrogen fixation and denitrification/anammox.
- Atmospheric N2 exchange influences nutrient availability for aquatic life.
Purpose of the Study:
- To investigate N2 saturation levels in lakes to infer net biological nitrogen processes.
- To understand the role of N2 supersaturation in the nitrogen balance of freshwater systems.
- To evaluate the prevailing paradigm of nitrogen fixation compensating for N-limitation in lakes.
Main Methods:
- Analysis of N2 saturation in 34 lakes across a 5° latitude range.
- Inclusion of lakes with diverse trophic statuses, mixing regimes, and bathymetry.
- Statistical analysis of N2 supersaturation across a large sample size (n=248).
Main Results:
- Nearly all surveyed lakes in the upper Midwest (USA) exhibited N2 supersaturation (>85% of samples).
- This supersaturation indicates a net release of nitrogen from lakes to the atmosphere.
- Observed N2 release suggests denitrification and/or anammox processes dominate over nitrogen fixation.
Conclusions:
- Freshwater lakes are significant sources of atmospheric nitrogen, contrary to some traditional views.
- The continuous loss of nitrogen implies that internal processes are not sufficient to balance the nitrogen cycle.
- Terrestrial nitrogen inputs are likely essential for maintaining nitrogen balance in these lake ecosystems.
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