Different roles of water in secondary organic aerosol formation from toluene and isoprene

被引:59
|
作者
Jia, Long [1 ,2 ]
Xu, YongFu [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China
[2] Univ Chinese Acad Sci, Dept Atmospher Chem & Environm Sci, Coll Earth Sci, Beijing 100049, Peoples R China
基金
国家重点研发计划; 中国国家自然科学基金;
关键词
VAPOR WALL LOSS; RESOLUTION MASS-SPECTROMETRY; RELATIVE-HUMIDITY; SOA FORMATION; CRIEGEE INTERMEDIATE; REACTIVE UPTAKE; M-XYLENE; LABORATORY CHAMBERS; PARTITIONING MODEL; PARTICLE FORMATION;
D O I
10.5194/acp-18-8137-2018
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Roles of water in the formation of secondary organic aerosol (SOA) from the irradiations of toluene-NO2 and isoprene-NO2 were investigated in a smog chamber. Experimental results show that the yield of SOA from toluene almost doubled as relative humidity increased from 5 to 85 %, whereas the yield of SOA from isoprene under humid conditions decreased by 2.6 times as compared to that under dry conditions. The distinct difference of RH effects on SOA formation from toluene and isoprene is well explained with our experiments and model simulations. The increased SOA from humid toluene-NO2 irradiations is mainly contributed by O-H-containing products such as polyalcohols formed from aqueous reactions. The major chemical components of SOA in isoprene-NO2 irradiations are oligomers formed from the gas phase. SOA formation from isoprene-NO2 irradiations is controlled by stable Criegee intermediates (SCIs) that are greatly influenced by water. As a result, high RH can obstruct the oligomerization reaction of SCIs to form SOA.
引用
收藏
页码:8137 / 8154
页数:18
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