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华北城市雪中有机氮的高分子多样性。

High Molecular Diversity of Organic Nitrogen in Urban Snow in North China.

机构信息

Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China.

State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China.

出版信息

Environ Sci Technol. 2021 Apr 20;55(8):4344-4356. doi: 10.1021/acs.est.0c06851. Epub 2021 Jan 27.

DOI:10.1021/acs.est.0c06851
PMID:33502199
Abstract

Snow serves as a vital scavenging mechanism to gas-phase and particle-phase organic nitrogen substances in the atmosphere, providing a significant link between land-atmosphere flux of nitrogen in the surface-earth system. Here, we used optical instruments (UV-vis and excitation-emission matrix fluorescence) and a Fourier transform ion cyclotron resonance mass spectrometer (FT-ICR MS) to elucidate the molecular composition and potential precursors of snow samples collected simultaneously at four megacities in North China. The elemental O/N ratio (≥3), together with the preference in the negative ionization mode, indicates that the one and two nitrogen atom-containing organics (CHON and CHON) in snow were largely in the oxidized form (as organic nitrates, -ONO). This study assumed that scavenging of particle-phase and gas-phase organic nitrates might be significant sources of CHON in precipitation. A gas-phase oxidation process and a particle-phase hydrolysis process, at a molecular level, were used to trace the potential precursors of CHON. Results show that more than half of the snow CHON molecules may be related to the oxidized and hydrolyzed processes of atmospheric organics. Potential formation processes of atmospheric organics on a molecular level provide a new concept to better understand the sources and scavenging mechanisms of organic nitrogen species in the atmosphere.

摘要

雪作为大气中气相和颗粒相有机氮物质的重要清除机制,为地表-大气系统中氮的陆气通量提供了重要的联系。在这里,我们使用光学仪器(紫外-可见和激发-发射矩阵荧光)和傅里叶变换离子回旋共振质谱仪(FT-ICR MS)来阐明同时在华北四个特大城市采集的雪样本的分子组成和潜在前体。元素 O/N 比(≥3),加上负离子模式的偏好,表明雪中的一氮和两氮原子有机化合物(CHON 和 CHON)主要以氧化形式存在(作为有机硝酸盐,-ONO)。本研究假设颗粒相和气相有机硝酸盐的清除可能是降水 CHON 的重要来源。一个气相氧化过程和一个颗粒相水解过程,在分子水平上,被用来追踪 CHON 的潜在前体。结果表明,超过一半的雪 CHON 分子可能与大气有机物的氧化和水解过程有关。在分子水平上,大气有机物的潜在形成过程为更好地理解大气中有机氮物质的来源和清除机制提供了一个新概念。

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