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Denitrification in suburban lawn soils.
Steve M Raciti1, Amy J Burgin, Peter M Groffman
1Department of Natural Resources, Cornell University, Ithaca, NY, USA. raciti@bu.edu
Journal of Environmental Quality
|October 28, 2011
Summary
Lawn soils remove significant nitrogen (N) via denitrification, especially when saturated and fertilized. However, these processes are highly variable, and lawns may still be a source of nitrous oxide (NO).
Area of Science:
- Environmental Science
- Soil Science
- Ecology
Background:
- Nitrogen (N) is frequently added to urban and suburban lawns, but its fate remains uncertain.
- Understanding N cycling in residential landscapes is crucial for managing nutrient pollution and greenhouse gas emissions.
Purpose of the Study:
- To quantify nitrogen (N) and nitrous oxide (NO) fluxes from lawns.
- To identify key environmental factors controlling denitrification and NO production in lawn soils.
Main Methods:
- Direct flux and in situ chamber methods were used to measure N and NO fluxes.
- Soil oxygen, moisture, and available NO were monitored using sensors.
- Laboratory incubations assessed NO production and consumption under controlled conditions.
Main Results:
- Denitrification rates were high only in saturated, fertilized soils, totaling 14.0 ± 3.6 kg N ha⁻¹ yr⁻¹.
- Over 80% of annual denitrification occurred during just 5% of the growing season.
- In situ NO fluxes were low, but laboratory incubations revealed high initial NO production in saturated, fertilized soils, followed by consumption.
Conclusions:
- Denitrification is an important N removal pathway in lawns but is highly dependent on soil saturation and fertilization.
- Lawns can be a significant source of NO due to a lag between production and consumption, especially after fertilization and saturation.
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