沉积(地质)
氮氧化物
氮气
环境科学
环境化学
化学
地质学
古生物学
有机化学
沉积物
燃烧
作者
Zhang Wen,Wen Xu,Qi Li,Mengjuan Han,Aohan Tang,Ying Zhang,Xiaosheng Luo,Jianlin Shen,Wei Wang,Kaihui Li,Yuepeng Pan,Lin Zhang,Wenqing Li,Jeffery L. Collett,Buqing Zhong,Xuemei Wang,K. W. T. Goulding,Fusuo Zhang,Xuejun Liu
标识
DOI:10.1016/j.envint.2020.106022
摘要
China has experienced a dramatic change in atmospheric reactive nitrogen (Nr) emissions over the past four decades. However, it remains unclear how nitrogen (N) deposition has responded to increases and/or decreases in Nr emissions. This study quantitatively assesses temporal and spatial variations in measurements of bulk and calculated dry N deposition in China from 1980 to 2018. A long-term database (1980–2018) shows that bulk N deposition peaked in around 2000, and had declined by 45% by 2016–2018. Recent bulk and dry N deposition (based on monitoring from 2011 to 2018) decreased from 2011 to 2018, with current average values of 19.4 ± 0.8 and 20.6 ± 0.4 kg N ha−1 yr−1, respectively. Oxidized N deposition, especially dry deposition, decreased after 2010 due to NOx emission controls. In contrast, reduced N deposition was approximately constant, with reductions in bulk NH4+-N deposition offset by a continuous increase in dry NH3 deposition. Elevated NH3 concentrations were found at nationwide monitoring sites even at urban sites, suggesting a strong influence of both agricultural and non-agricultural sources. Current emission controls are reducing Nr emissions and deposition but further mitigation measures are needed, especially of NH3, built on broader regional emission control strategies.
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