Thermal desorption mass spectrometric analysis of organic aerosol formed from reactions of 1-tetradecene and O3 in the presence of alcohols and carboxylic acids

被引:136
作者
Tobias, HJ
Ziemann, PJ [1 ]
机构
[1] Univ Calif Riverside, Air Pollut Res Ctr, Riverside, CA 92521 USA
[2] Univ Calif Riverside, Dept Environm Sci, Riverside, CA 92521 USA
[3] Univ Calif Riverside, Dept Chem, Riverside, CA 92521 USA
关键词
D O I
10.1021/es9907156
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The chemistry of secondary organic aerosol formation from reactions of 1-tetradecene and O-3 in dry air in the presence of excess alcohols and carboxylic acids was investigated in an environmental chamber using a thermal desorption particle beam mass spectrometer. Temperature-programmed thermal desorption of collected aerosol shows that in each reaction two major aerosol products are formed. The more volatile compounds in each pair of products are alpha-alkoxytridecyl or alpha-acyloxytridecyl hydroperoxides, which were identified by comparison of mass spectra with those of standard compounds generated by the corresponding liquid-phase ozonolysis reactions. The formation of organic hydroperoxides in the gas and liquid phases is consistent with a mechanism involving reactions of the alcohols and carboxylic acids with stabilized Criegee biradicals generated in the alkene-O-3 reaction. The less volatile compounds are alpha-alkoxy-alpha'-hydroxyditridecyl or alpha-acyloxy-alpha'-hydroxyditridecyl peroxides (peroxyhemiacetals) formed by reactions of the hydroperoxides with tridecanal, which is generated along with formaldehyde during biradical formation. The vapor pressures of these compounds estimated from their desorption temperatures are similar to 10(-7)-10(-14) Torr. These types of reactions could play a role in atmospheric aerosol nucleation and growth and provide a mechanism for creating fine-particle organic peroxides, which are currently of interest because of their potential for adversely impacting human health.
引用
收藏
页码:2105 / 2115
页数:11
相关论文
共 62 条
[1]  
ADAMSON AW, 1982, PHYSICAL CHEM SURFAC
[2]   Gas-phase tropospheric chemistry of volatile organic compounds .1. Alkanes and alkenes [J].
Atkinson, R .
JOURNAL OF PHYSICAL AND CHEMICAL REFERENCE DATA, 1997, 26 (02) :215-290
[3]   FORMATION OF OH RADICALS IN THE GAS-PHASE REACTIONS OF O3 WITH A SERIES OF TERPENES [J].
ATKINSON, R ;
ASCHMANN, SM ;
AREY, J ;
SHOREES, B .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D5) :6065-6073
[4]  
Atkinson R., 1994, Journal of Physical and Chemical Reference Data, Monograph, V2, P1
[5]  
Atkinson R., 1989, J. Phys. Chem. Ref. Data, V1, P1
[6]  
Bailey P. S., 1978, OZONATION ORGANIC CH, V1
[7]   MASS SPECTROMETRIC STUDY OF SOME ALKYL HYDROPEROXIDES [J].
BURGESS, AR ;
LANE, RDG ;
SENSHARM.DK .
JOURNAL OF THE CHEMICAL SOCIETY B-PHYSICAL ORGANIC, 1969, (04) :341-&
[8]   CLIMATE FORCING BY ANTHROPOGENIC AEROSOLS [J].
CHARLSON, RJ ;
SCHWARTZ, SE ;
HALES, JM ;
CESS, RD ;
COAKLEY, JA ;
HANSEN, JE ;
HOFMANN, DJ .
SCIENCE, 1992, 255 (5043) :423-430
[9]   OCEANIC PHYTOPLANKTON, ATMOSPHERIC SULFUR, CLOUD ALBEDO AND CLIMATE [J].
CHARLSON, RJ ;
LOVELOCK, JE ;
ANDREAE, MO ;
WARREN, SG .
NATURE, 1987, 326 (6114) :655-661
[10]  
Finlayson-Pitts B. J., 1999, CHEM UPPER LOWER ATM