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Identifying Ammonia Hotspots in China Using a National Observation Network

机译:使用国家观测网络识别中国的氨热点

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摘要

The limited availability of ammonia (NH_(3)) measurements is currently a barrier to understanding the vital role of NH_(3) in secondary aerosol formation during haze pollution events and prevents a full assessment of the atmospheric deposition of reactive nitrogen. The observational gaps motivated us to design this study to investigate the spatial distributions and seasonal variations in atmospheric NH_(3) on a national scale in China. On the basis of a 1-year observational campaign at 53 sites with uniform protocols, we confirm that abundant concentrations of NH_(3) [1 to 23.9 μg m~(–3)] were identified in typical agricultural regions, especially over the North China Plain (NCP). The spatial pattern of the NH_(3) surface concentration was generally similar to those of the satellite column concentrations as well as a bottom-up agriculture NH_(3) emission inventory. However, the observed NH_(3) concentrations at urban and desert sites were comparable with those from agricultural sites and 2–3 times those of mountainous/forest/grassland/waterbody sites. We also found that NH_(3) deposition fluxes at urban sites account for only half of the emissions in the NCP, suggesting the transport of urban NH_(3) emissions to downwind areas. This finding provides policy makers with insights into the potential mitigation of nonagricultural NH_(3) sources in developed regions.
机译:氨(NH_(3))测量的有限可用性目前是了解NH_(3)在霾污染事件期间二次气溶胶形成中的重要作用的障碍,并妨碍了对活性氮在大气中的沉积的全面评估。观测上的差距促使我们设计这项研究,以研究中国全国范围内大气NH_(3)的空间分布和季节变化。根据对53个地点的统一协议进行的为期1年的观测活动,我们确认在典型的农业地区,尤其是北部地区,发现了大量的NH_(3)[1至23.9μgm〜(–3)]中国平原(NCP)。 NH_(3)表面浓度的空间格局通常与卫星列浓度以及自下而上的农业NH_(3)排放清单的格局相似。但是,在城市和沙漠地区观测到的NH_(3)浓度与农业地区相当,是山区/森林/草原/水体场所的2-3倍。我们还发现,城市站点的NH_(3)沉积通量仅占NCP排放的一半,这表明城市NH_(3)排放向下游地区的迁移。这一发现为决策者提供了有关缓解发达地区非农业NH_(3)来源的潜在见解。

著录项

  • 来源
    《Environmental Science & Technology》 |2018年第7期|3926-3934|共9页
  • 作者单位

    State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871, China;

    Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871, China;

    National Climate Center, China Meteorological Administration, Beijing 100081, China;

    State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China;

    State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    Department of Environmental Science, Peking University, Beijing 100871, China;

    Ministry of Education Key Laboratory for Earth System Modeling, Center for Earth System Science, Tsinghua University, Beijing 100084, China;

    State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry (LAPC), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

  • 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);
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  • 正文语种 eng
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  • 入库时间 2022-08-17 13:56:41

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