globalchange  > 气候减缓与适应
DOI: 10.1016/j.envpol.2018.09.135
WOS记录号: WOS:000452940700061
论文题名:
Decreased atmospheric nitrogen deposition in eastern North America: Predicted responses of forest ecosystems
作者: Gilliam, Frank S.1; Burns, Douglas A.2; Driscoll, Charles T.3; Frey, Serita D.4; Lovett, Gary M.5; Watmough, Shaun A.6
通讯作者: Gilliam, Frank S.
刊名: ENVIRONMENTAL POLLUTION
ISSN: 0269-7491
EISSN: 1873-6424
出版年: 2019
卷: 244, 页码:560-574
语种: 英语
英文关键词: Decreased nitrogen deposition ; Forest ecosystems ; Nitrogen biogeochemistry ; Eastern deciduous forest ; Clean Air Act
WOS关键词: LONG-TERM CHANGES ; SOIL MICROBIAL COMMUNITIES ; NORTHEASTERN UNITED-STATES ; FUNGAL COMMUNITY ; HARVARD FOREST ; N DEPOSITION ; ACIDIC DEPOSITION ; HERBACEOUS LAYER ; HARDWOOD FOREST ; CARBON STORAGE
WOS学科分类: Environmental Sciences
WOS研究方向: Environmental Sciences & Ecology
英文摘要:

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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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/125904
Appears in Collections:气候减缓与适应

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作者单位: 1.Univ West Florida, Dept Biol, Pensacola, FL 32514 USA
2.US Geol Survey, New York Water Sci Ctr, 425 Jordan Rd, Troy, NY 12180 USA
3.Syracuse Univ, Dept Civil & Environm Engn, Syracuse, NY 13244 USA
4.Univ New Hampshire, Dept Nat Resources & Environm, Durham, NH 03824 USA
5.Cary Inst Ecosyst Studies, POB AB, Millbrook, NY 12545 USA
6.Trent Univ, Sch Environm, 1600 West Bank Dr, Peterborough, ON K9L 0G2, Canada

Recommended Citation:
Gilliam, Frank S.,Burns, Douglas A.,Driscoll, Charles T.,et al. Decreased atmospheric nitrogen deposition in eastern North America: Predicted responses of forest ecosystems[J]. ENVIRONMENTAL POLLUTION,2019-01-01,244:560-574
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