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Assessing the ammonium nitrate formation regime in the Paris megacity and its representation in the CHIMERE model

机译:评估巴黎大城市的硝酸铵形成状况及其在CHIMERE模型中的表示

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pstrongAbstract./strong Secondary inorganic compounds represent a major fraction of fine aerosol in the Paris megacity. The thermodynamics behind their formation is now relatively well constrained but, due to sparse direct measurements of their precursors (in particular NHsub3/sub and HNOsub3/sub), uncertainties remain on their concentrations and variability as well as the formation regime of ammonium nitrate (in terms of limited species among NHsub3/sub and HNOsub3/sub) in urban environments such as Paris. This study presents the first urban background measurements of both inorganic aerosol compounds and their gaseous precursors during several months within the city of Paris. Intense agriculture-related NHsub3/sub episodes are observed in spring/summer while HNOsub3/sub concentrations remain relatively low, even during summer, which leads to a NHsub3/sub-rich regime in Paris. The local formation of ammonium nitrate within the city appears low, despite high NOsubix/i/sub emissions. The data set also allows evaluating the CHIMERE chemistry-transport model (CTM). Interestingly, the rather good results obtained on ammonium nitrates hide significant errors on gaseous precursors (e.g., mean bias of a??75 and +195span class="thinspace"/span% for NHsub3/sub and HNOsub3/sub, respectively). This leads to a misrepresentation of the nitrate formation regime through a highly underestimated gas ratio metric (introduced by Ansari and Pandis, 1998) and a much higher sensitivity of nitrate concentrations to ammonia changes. Several uncertainty sources are investigated, pointing out the importance of better assessing both NHsub3/sub agricultural emissions and OH concentrations in the future. These results remind us of the caution required when using of CTMs for emission scenario analysis, highlighting the importance of prior diagnostic and dynamic evaluations./p.
机译:> >摘要。次要无机化合物占巴黎特大城市中大部分气溶胶的主要部分。现在,其形成背后的热力学受到了较好的限制,但是由于对其前体(尤其是NH 3 和HNO 3 )的直接测量稀疏,因此其浓度和巴黎等城市环境中硝酸铵的变异性和形成机理(就NH 3 和HNO 3 中的有限物种而言)这项研究提出了巴黎市几个月内对无机气溶胶化合物及其气态前体的首次城市本底测量。在春季/夏季观察到与农业相关的强烈NH 3 事件,而即使在夏季,HNO 3 的浓度仍然相对较低,导致NH 3 x 的排放量很高,但城市中硝酸铵的局部形成仍很低。该数据集还允许评估CHIMERE化学运输模型(CTM)。有趣的是,在硝酸铵上获得的相当不错的结果掩盖了气态前体的显着误差(例如,对于NH 3 75和+195 class =“ thinspace”> %的平均偏差。 sub>和HNO 3 )。由于高度低估了气体比率(由Ansari和Pandis引入,1998年),硝酸盐浓度对氨变化的敏感性更高,这导致对硝酸盐形成机制的误解。调查了一些不确定性来源,指出了将来更好地评估NH 3 农业排放量和OH浓度的重要性。这些结果使我们想起了使用CTM进行排放情景分析时需要谨慎的地方,突出了事先诊断和动态评估的重要性。

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