Gas-phase products and secondary organic aerosol formation from the ozonolysis and photooxidation of myrcene

被引:24
作者
Boege, Olaf [1 ]
Mutzel, Anke [1 ]
Iinuma, Yoshiteru [1 ]
Yli-Pirila, Pasi [2 ]
Kahnt, Ariane [1 ]
Joutsensaari, Jorma [2 ]
Herrmann, Hartmut [1 ]
机构
[1] Leibniz Inst Tropospharenforsch TROPOS, D-04318 Leipzig, Germany
[2] Univ Eastern Finland, Dept Appl Phys, FI-70211 Kuopio, Finland
基金
芬兰科学院;
关键词
Myrcene; Ozonolysis; OH radical; Chamber experiment; Reaction mechanism; SOA; OXIDATION-PRODUCTS; O-3-INITIATED REACTIONS; INITIATED OXIDATION; ALPHA-PINENE; OH RADICALS; OZONE; MONOTERPENES; SERIES; YIELDS; FORESTS;
D O I
10.1016/j.atmosenv.2013.07.034
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this study, the ozone and OH-radical reactions of myrcene were investigated in an aerosol chamber (at 292-295 K and 50% relative humidity) to examine the gas-phase oxidation products and secondary organic aerosol (SOA) formation. The ozone reaction studies were performed in the presence and absence of CO, which serves as an OH radical scavenger. In the photooxidation experiments OH radicals were generated by photolysis of methyl nitrite. The ozonolysis of myrcene in the presence of CO resulted in a substantial yield of 4-vinyl-4-pentenal (55.3%), measured as m/z 111 plus m/z 93 using proton transfer reaction-mass spectrometry (PTR-MS) and confirmed unambiguously as C7H10O by denuder measurements and HPLC/ESI-TOFNIS analysis of its 2,4-dinitrophenylhydrazine (DNPH) derivative. Additionally, the formation of two different organic dicarbonyls with m/z 113 and a molecular formula of C6H8O2 were observed (2.1%). The yields of these dicarbonyls were higher in the ozonolysis experiments without an OH scavenger (5.4%) and even higher (13.8%) in the myrcene OH radical reaction. The formation of hydroxyacetone as a direct product of the myrcene reaction with ozone with a molar yield of 17.6% was also observed. The particle size distribution and volume concentrations were monitored and facilitated the calculation of SOA yields, which ranged from 0 to 0.01 (ozonolysis in the presence of CO) to 0.39 (myrcene OH radical reaction). Terpenylic acid was found in the SOA samples collected from the ozonolysis of myrcene in the absence of an OH scavenger and the OH radical-initiated reaction of myrcene but not in samples collected from the ozonolysis in the presence of CO as an OH radical scavenger, suggesting that terpenylic acid formation involves the reaction of myrcene with an OH radical. A reaction mechanism describing the formation of terpenylic acid is proposed. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:553 / 560
页数:8
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