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The cycling of organic nitrogen through the atmosphere

机译:有机氮在大气中的循环

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摘要

Atmospheric organic nitrogen (ON) appears to be a ubiquitous but poorly understood component of the atmospheric nitrogen deposition flux. Here, we focus on the (ON) components that dominate deposition and do not consider reactive atmospheric gases containing (ON) such as peroxyacyl nitrates that are important in atmospheric nitrogen transport, but are probably not particularly important in deposition. We first review the approaches to the analysis and characterization of atmospheric (ON). We then briefly summarize the available data on the concentrations of (ON)in both aerosols and rainwater from around the world, and the limited information available on its chemical characterization. This evidence clearly shows that atmospheric aerosol and rainwater (ON)is a complex mixture of material from multiple sources. This synthesis of available information is then used to try and identify some of the important sources of this material, in particular, if it is of predominantly natural or anthropogenic origin. Finally, we suggest that the flux of ON is about 25 per cent of the total nitrogen deposition flux.
机译:大气有机氮(ON)似乎是大气中氮沉积通量的普遍存在但知之甚少的成分。在这里,我们集中于控制沉积的(ON)成分,而不考虑包含(ON)的反应性大气气体,例如过氧酰基硝酸盐,它们在大气氮的运输中很重要,但在沉积中可能并不特别重要。我们首先回顾一下大气(ON)分析和表征的方法。然后,我们简要总结了有关来自世界各地的气溶胶和雨水中的(ON)浓度的可用数据,以及有关其化学表征的有限信息。该证据清楚地表明,大气气溶胶和雨水(ON)是多种来源的物质的复杂混合物。然后,可用信息的这种合成被用来尝试识别这种材料的一些重要来源,特别是如果它主要是天然或人为来源的话。最后,我们建议ON的通量约为总氮沉积通量的25%。

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