Ozonolysis of α-pinene at atmospherically relevant concentrations:: Temperature dependence of aerosol mass fractions (yields)

被引:157
作者
Pathak, Ravi K. [1 ]
Stanier, Charles O.
Donahue, Neil M.
Pandis, Spyros N.
机构
[1] Carnegie Mellon Univ, Dept Chem Engn, Pittsburgh, PA 15213 USA
[2] Univ Iowa, Dept Engn, Iowa City, IA 52242 USA
[3] Univ Patras, Dept Chem Engn, GR-26000 Patras, Greece
关键词
D O I
10.1029/2006JD007436
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Despite a number of smog chamber studies of the alpha-pinene/O-3 system, the effect of temperature on alpha-pinene secondary organic aerosol (SOA) mass fractions (or yields) remains poorly understood. In this study, the temperature dependence of secondary organic aerosol mass fractions (AMF) during ozonolysis of a- pinene is investigated in a temperature controlled smog chamber. Experiments were performed with and without ammonium sulfate aerosol seeds at RH < 10% and at 0 degrees C, 15 degrees C, 20 degrees C, 30 degrees C and 40 degrees C. The initial alpha-pinene concentration varied from 3.5 to 50 ppb, and an excess of ozone was used. High time resolution secondary organic AMFs were obtained combining continuous gas-phase concentration measurements (using proton transfer reaction mass spectrometry, PTR-MS) with continuous aerosol concentration measurements (using a scanning mobility particle sizer, SMPS). The presence of inert aerosol seeds is often necessary to minimize experimental errors due to loss of semivolatile vapors to the walls of the chamber. The alpha-pinene secondary organic AMFs show a weak dependence on temperature in the 15 degrees to 40 degrees C range and stronger temperature dependence in the 0 degrees and 15 degrees C range.
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页数:8
相关论文
共 32 条
[1]   Atmospheric aerosols: Biogeochemical sources and role in atmospheric chemistry [J].
Andreae, MO ;
Crutzen, PJ .
SCIENCE, 1997, 276 (5315) :1052-1058
[2]   New particle formation during α- and β-pinene oxidation by O3, OH and NO3, and the influence of water vapour:: particle size distribution studies [J].
Bonn, B ;
Moortgat, GK .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2002, 2 :183-196
[3]   The effect of water on gas-particle partitioning of secondary organic aerosol.: Part I:: α-pinene/ozone system [J].
Cocker, DR ;
Clegg, SL ;
Flagan, RC ;
Seinfeld, JH .
ATMOSPHERIC ENVIRONMENT, 2001, 35 (35) :6049-6072
[4]   Contributions of organic peroxides to secondary aerosol formed from reactions of monoterpenes with O3 [J].
Docherty, KS ;
Wu, W ;
Lim, YB ;
Ziemann, PJ .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2005, 39 (11) :4049-4059
[5]   Effect of OH radicals, relative humidity, and time on the composition of the products formed in the ozonolysis of α-pinene [J].
Fick, J ;
Pommer, L ;
Nilsson, C ;
Andersson, B .
ATMOSPHERIC ENVIRONMENT, 2003, 37 (29) :4087-4096
[6]   Experimental and modeling studies of secondary organic aerosol formation and some applications to the marine boundary layer [J].
Gao, S ;
Hegg, DA ;
Frick, G ;
Caffrey, PF ;
Pasternack, L ;
Cantrell, C ;
Sullivan, W ;
Ambrusko, J ;
Albrechcinski, T ;
Kirchstetter, TW .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D21) :27619-27634
[7]   Organic aerosol formation from the oxidation of biogenic hydrocarbons [J].
Griffin, RJ ;
Cocker, DR ;
Flagan, RC ;
Seinfeld, JH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D3) :3555-3567
[8]   Estimate of global atmospheric organic aerosol from oxidation of biogenic hydrocarbons [J].
Griffin, RJ ;
Cocker, DR ;
Seinfeld, JH ;
Dabdub, D .
GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (17) :2721-2724
[9]   A GLOBAL-MODEL OF NATURAL VOLATILE ORGANIC-COMPOUND EMISSIONS [J].
GUENTHER, A ;
HEWITT, CN ;
ERICKSON, D ;
FALL, R ;
GERON, C ;
GRAEDEL, T ;
HARLEY, P ;
KLINGER, L ;
LERDAU, M ;
MCKAY, WA ;
PIERCE, T ;
SCHOLES, B ;
STEINBRECHER, R ;
TALLAMRAJU, R ;
TAYLOR, J ;
ZIMMERMAN, P .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D5) :8873-8892
[10]  
HALL P, 1997, NATIONS NATL, V3, P3