Rapid Autoxidation Forms Highly Oxidized RO2 Radicals in the Atmosphere

被引:192
作者
Jokinen, Tuija [1 ,2 ]
Sipila, Mikko [2 ]
Richters, Stefanie [1 ]
Kerminen, Veli-Matti [2 ]
Paasonen, Pauli [2 ]
Stratmann, Frank [1 ]
Worsnop, Douglas [2 ,3 ]
Kulmala, Markku [2 ]
Ehn, Mikael [2 ]
Herrmann, Hartmut [1 ]
Berndt, Torsten [1 ]
机构
[1] TROPOS, Leibniz Inst Tropospharenforsch, D-04318 Leipzig, Germany
[2] Univ Helsinki, Dept Phys, FIN-00014 Helsinki, Finland
[3] Aerodyne Res Inc, Billerica, MA 01821 USA
基金
芬兰科学院; 欧洲研究理事会;
关键词
atmospheric chemistry; autoxidation; mass spectrometry; radical reactions; SULFURIC-ACID; AIR; OXIDATION; KINETICS; AEROSOL;
D O I
10.1002/anie.201408566
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Gas-phase oxidation routes of biogenic emissions, mainly isoprene and monoterpenes, in the atmosphere are still the subject of intensive research with special attention being paid to the formation of aerosol constituents. This laboratory study shows that the most abundant monoterpenes (limonene and alpha-pinene) form highly oxidized RO2 radicals with up to 12 O atoms, along with related closed-shell products, within a few seconds after the initial attack of ozone or OH radicals. The overall process, an intramolecular ROO -> QOOH reaction and subsequent O-2 addition generating a next R'OO radical, is similar to the well-known autoxidation processes in the liquid phase (QOOH stands for a hydroperoxyalkyl radical). Field measurements show the relevance of this process to atmospheric chemistry. Thus, the well-known reaction principle of autoxidation is also applicable to the atmospheric gas-phase oxidation of hydrocarbons leading to extremely low-volatility products which contribute to organic aerosol mass and hence influence the aerosol-cloud-climate system.
引用
收藏
页码:14596 / 14600
页数:5
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