Influence of relative humidity and temperature on the production of pinonaldehyde and OH radicals from the ozonolysis of α-pinene

被引:58
作者
Tillmann, R. [1 ]
Hallquist, M. [2 ]
Jonsson, A. M. [2 ]
Kiendler-Scharr, A. [1 ]
Saathoff, H. [3 ]
Iinuma, Y. [4 ]
Mentel, Th. F. [1 ]
机构
[1] Forschungszentrum Julich, Inst Chem & Dynam Geosphare 2, D-52425 Julich, Germany
[2] Univ Gothenburg, Dept Chem, S-41296 Gothenburg, Sweden
[3] Forschungszentrum Karlsruhe, Inst Meteorol & Climate Res, D-76344 Eggenstein Leopoldshafen, Germany
[4] Leibnitz Inst Tropospher Res, D-04318 Leipzig, Germany
关键词
SECONDARY ORGANIC AEROSOL; GAS-PHASE REACTIONS; OZONE INITIATED OXIDATION; MASS-SPECTROMETER; BETA-PINENE; AIRBORNE PARTICLES; WATER-VAPOR; MONOTERPENES; DELTA(3)-CARENE; YIELDS;
D O I
10.5194/acp-10-7057-2010
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The ozonolysis of alpha-pinene has been investigated under dry and humid conditions in the temperature range of 243-303 K. The results provided new insight into the role of water and temperature in the degradation mechanism of alpha-pinene and in the formation of secondary organic aerosols (SOA). The SOA yields were higher at humid conditions than at dry conditions. The water induced gain was largest for the lowest temperatures investigated (243 and 253 K). The increase in the SOA yields was dominated by water (and temperature) effects on the organic product distribution, whilst physical uptake of water was negligible. This will be demonstrated for the example of pinon-aldehyde (PA) which was formed as a major product in the humid experiments with total molar yields of 0.30+/-0.06 at 303 K and 0.15+/-0.03 at 243 K. In the dry experiments the molar yields of PA were only 0.07+/-0.02 at 303 K and 0.02+/-0.02 at 253 K. The observed partitioning of PA as a function of the SOA mass present at 303 K limited the effective vapour pressure of pure PA p(PA)(0) to the range of 0.01-0.001 Pa, 3-4 orders of magnitude lower than literature values. The corresponding mass partitioning coefficient was determined to K-PA=0.005+/-0.004 m(3) mu g-1 and the total mass yield alpha(PAtotal)=0.37+/-0.08. At 303 K PA preferably stayed in the gas-phase, whereas at 253 K and 243 K it exclusively partitioned into the particulate phase. PA could thus account at
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页码:7057 / 7072
页数:16
相关论文
共 72 条
[1]   Quantitative sampling using an Aerodyne aerosol mass spectrometer - 1. Techniques of data interpretation and error analysis [J].
Allan, JD ;
Jimenez, JL ;
Williams, PI ;
Alfarra, MR ;
Bower, KN ;
Jayne, JT ;
Coe, H ;
Worsnop, DR .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D3)
[2]   A generalised method for the extraction of chemically resolved mass spectra from aerodyne aerosol mass spectrometer data [J].
Allan, JD ;
Delia, AE ;
Coe, H ;
Bower, KN ;
Alfarra, MR ;
Jimenez, JL ;
Middlebrook, AM ;
Drewnick, F ;
Onasch, TB ;
Canagaratna, MR ;
Jayne, JT ;
Worsnop, DR .
JOURNAL OF AEROSOL SCIENCE, 2004, 35 (07) :909-922
[3]   Products of the gas-phase reactions of O(3P) atoms and O3 with α-pinene and 1,2-dimethyl-1-cyclohexene [J].
Alvarado, A ;
Tuazon, EC ;
Aschmann, SM ;
Atkinson, R ;
Arey, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D19) :25541-25551
[4]  
Anglada JM, 2002, CHEMPHYSCHEM, V3, P215, DOI 10.1002/1439-7641(20020215)3:2<215::AID-CPHC215>3.3.CO
[5]  
2-V
[6]   OH radical formation from the gas-phase reactions of O3 with a series of terpenes [J].
Aschmann, SM ;
Arey, J ;
Atkinson, R .
ATMOSPHERIC ENVIRONMENT, 2002, 36 (27) :4347-4355
[7]   Evaluated kinetic and photochemical data for atmospheric chemistry:: Volume I -: gas phase reactions of Ox, HOx, NOx and SOx species [J].
Atkinson, R ;
Baulch, DL ;
Cox, RA ;
Crowley, JN ;
Hampson, RF ;
Hynes, RG ;
Jenkin, ME ;
Rossi, MJ ;
Troe, J .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2004, 4 :1461-1738
[8]   Gas-phase tropospheric chemistry of biogenic volatile organic compounds: a review [J].
Atkinson, R ;
Arey, J .
ATMOSPHERIC ENVIRONMENT, 2003, 37 :S197-S219
[9]   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
[10]  
Baker J, 2001, INT J CHEM KINET, V34, P73