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Sources and Processes Contributing to Nitrogen Deposition: An Adjoint Model Analysis Applied to Biodiversity Hotspots Worldwide

机译:氮沉积的来源和过程:适用于全球生物多样性热点的伴随模型分析

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摘要

Anthropogenic enrichment of reactive nitrogen (Nr) deposition is an ecological concern. We use the adjoint of a global 3-D chemical transport model (GEOS-Chem) to identify the sources and processes that control Nr deposition to an ensemble of biodiversity hotspots worldwide and two U.S. national parks (Cuyahoga and Rocky Mountain). We find that anthropogenic sources dominate deposition at all continental sites and are mainly regional (less than 1000 km) in origin. In Hawaii, Nr supply is controlled by oceanic emissions of ammonia (50%) and anthropogenic sources (50%), with important contributions from Asia and North America. Nr deposition is also sensitive in complicated ways to emissions of SO_2, which affect Nr gas-aerosol partitioning, and of volatile organic compounds (VOCs), which affect oxidant concentrations and produce organic nitrate reservoirs. For example, VOC emissions generally inhibit deposition of locally emitted NO_x but significantly increase Nr deposition downwind. However, in polluted boreal regions, anthropogenic VOC emissions can promote Nr deposition in winter. Uncertainties in chemical rate constants for OH + NO_2 and NO_2 hydrolysis also complicate the determination of source-receptor relationships for polluted sites in winter. Application of our adjoint sensitivities to the representative concentration pathways (RCPs) scenarios for 2010- 2050 indicates that future decreases in Nr deposition due to NO_x emission controls will be offset by concurrent increases in ammonia emissions from agriculture.
机译:人为反应性氮(Nr)沉积物的富集是生态问题。我们使用全球3-D化学迁移模型(GEOS-Chem)的伴随物,来识别控制Nr沉积到全球生物多样性热点和两个美国国家公园(Cuyahoga和Rocky Mountain)的来源和过程。我们发现,在所有大陆站点的沉积过程中,人为来源均占主导地位,其起源主要是区域性的(小于1000 km)。在夏威夷,Nr的供应受海洋排放的氨(50%)和人为来源(50%)的控制,其中亚洲和北美的贡献很大。 Nr沉积对复杂的方式对排放会影响Nr气溶胶分配的SO_2和对影响氧化剂浓度并产生有机硝酸盐储层的挥发性有机化合物(VOC)的排放也很敏感。例如,VOC排放通常会抑制局部排放的NO_x的沉积,但会显着增加顺风向Nr的沉积。但是,在受污染的北方地区,人为的VOC排放会促进冬季的Nr沉积。 OH + NO_2和NO_2水解的化学速率常数的不确定性也使冬季受污染地点的源-受体关系的确定变得复杂。将我们的伴随敏感性应用到2010-2050年的代表性浓度路径(RCP)情景中,表明由于NO_x排放控制而导致的未来Nr沉积减少将被农业氨气的同时排放所抵消。

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  • 来源
    《Environmental Science & Technology》 |2013年第7期|3226-3233|共8页
  • 作者单位

    School of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts 02138, United States;

    School of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts 02138, United States;

    Department of Mechanical Engineering, University of Colorado, Boulder, Colorado 80309, United States;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-17 14:02:03

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