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Methods of Soil Resampling to Monitor Changes in the Chemical Concentrations of Forest Soils
Published on: November 25, 2016
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Spruce-fir forest changes during a 30-year nitrogen saturation experiment.
Steven G McNulty1, Johnny L Boggs1, John D Aber2
1USDA Forest Service, 920 Main Campus Dr. Suite 300, Raleigh, NC 27606, United States.
The Science of the Total Environment
|July 3, 2017
Summary
This 30-year study on red spruce-balsam fir forests found that nitrogen addition initially altered forest floor and tree health. Post-treatment, ecosystem recovery was slow, with climate change and other stressors hindering future regeneration.
Area of Science:
- Ecology
- Forestry
- Environmental Science
Background:
- High elevation red spruce-balsam fir forests face decline.
- The nitrogen (N) saturation hypothesis proposes excessive N causes forest damage.
- Understanding N impacts is crucial for forest management and conservation.
Purpose of the Study:
- To test the nitrogen (N) saturation hypothesis in a red spruce-balsam fir ecosystem.
- To investigate the mechanisms behind forest decline attributed to N deposition.
- To assess the long-term effects of N fertilization and subsequent recovery.
Main Methods:
- Established a field experiment with control, low, and high N addition plots (0, 15.7, 31.4 kg N ha⁻¹ yr⁻¹).
- Applied N treatments annually from 1988 to 2010, with ongoing monitoring.
- Measured forest floor properties (C:N, N mineralization, nitrification), foliar N and Ca content, and tree basal area.
Main Results:
- Increased N addition led to decreased forest floor C:N, N mineralization, and spruce basal area.
- Elevated N addition resulted in increased spruce foliar N% and forest floor nitrification.
- Control plots accumulated N, while N addition plots lost N from the forest floor.
- Post-treatment, tree components normalized, but forest floor processes recovered slowly.
- Forest mortality on N addition plots coincided with drought and freeze injury years.
Conclusions:
- Nitrogen addition significantly altered forest floor dynamics and tree health, supporting aspects of the N saturation hypothesis.
- Ecosystem recovery after N fertilization cessation was slow, with forest floor processes lagging.
- Climate change (warming, drought) and other stressors interact with N deposition, complicating ecosystem response.
- Spruce-fir ecosystem regeneration is unlikely in the next century due to cumulative stressors, despite recent growth increases.
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