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Decreased atmospheric nitrogen deposition in eastern North America: Predicted responses of forest ecosystems

期刊

ENVIRONMENTAL POLLUTION
卷 244, 期 -, 页码 560-574

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.envpol.2018.09.135

关键词

Decreased nitrogen deposition; Forest ecosystems; Nitrogen biogeochemistry; Eastern deciduous forest; Clean Air Act

资金

  1. National Science Foundation through the Hubbard Brook and Harvard Forest Long-Term Ecological Research Programs [DEB-1637685, DEB-1237491]
  2. U.S. Geological Survey National Water Quality Program
  3. New York State Energy Research and Development Environmental Monitoring, Evaluation and Protection program

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Historical increases in emissions and atmospheric deposition of oxidized and reduced nitrogen (N) provided the impetus for extensive, global-scale research investigating the effects of excess N in terrestrial and aquatic ecosystems, with several regions within the Eastern Deciduous Forest of the United States found to be susceptible to negative effects of excess N. The Clean Air Act and associated rules have led to decreases in emissions and deposition of oxidized N, especially in eastern U.S., representing a research challenge and opportunity for ecosystem ecologists and biogeochemists. The purpose of this paper is to predict changes in the structure and function of North American forest ecosystems in a future of decreased N deposition. Hysteresis is a property of a system wherein output is not a strict function of corresponding input, incorporating lag, delay, or history dependence, particularly when the response to decreasing input is different from the response to increasing input. We suggest a conceptual hysteretic model predicting varying lag times in recovery of soil acidification, plant biodiversity, soil microbial communities, forest carbon (C) and N cycling, and surface water chemistry toward pre-N impact conditions. Nearly all of these can potentially respond strongly to reductions in N deposition. Most responses are expected to show some degree of hysteresis, with the greatest delays in response occurring in processes most tightly linked to slow pools of N in wood and soil organic matter. Because experimental studies of declines in N loads in forests of North America are lacking and because of the expected hysteresis, it is difficult to generalize from experimental results to patterns expected from declining N deposition. These will likely be long-term phenomena, difficult to distinguish from other, concurrent environmental changes, including elevated atmospheric CO2, climate change, reductions in acidity, invasions of new species, and long-term vegetation responses to past disturbance. (C) 2018 Elsevier Ltd. All rights reserved.

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