Measurement of atmospheric sesquiterpenes by proton transfer reaction-mass spectrometry (PTR-MS)

被引:101
作者
Kim, S. [1 ,2 ]
Karl, T. [2 ]
Helmig, D. [3 ]
Daly, R. [3 ]
Rasmussen, R. [4 ]
Guenther, A. [2 ]
机构
[1] Natl Ctr Atmospher Res, Adv Study Program, POB 3000, Boulder, CO 80307 USA
[2] Natl Ctr Atmospher Res, Div Atmospher Chem, Boulder, CO 80307 USA
[3] Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA
[4] Oregon Grad Inst, Beaverton, OR 97006 USA
基金
美国国家科学基金会;
关键词
VOLATILE ORGANIC-COMPOUNDS; AIR; HYDROCARBONS; EMISSIONS; PRODUCTS; FOREST; FLUX; CALIBRATION; VEGETATION; MOUNTAINS;
D O I
10.5194/amt-2-99-2009
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The ability to measure sesquiterpenes (SQT; C15H24) by a Proton-Transfer-Reaction Mass Spectrometer (PTR-MS) was investigated. SQT calibration standards were prepared by a capillary diffusion method and the PTR-MS-estimated mixing ratios were derived from the counts of product ions and proton transfer reaction constants. These values were compared with mixing ratios determined by a calibrated Gas Chromatograph (GC) coupled to a Flame Ionization Detector (GC-FID). Product ion distributions from soft-ionization occurring in a selected ion drift tube via proton transfer were measured as a function of collision energies. Results after the consideration of the mass discrimination of the PTR-MS system suggest that quantitative SQT measurements within 20% accuracy can be achieved with PTR-MS if two major product ions (m/z 149(+) and 205(+)), out of seven major product ions (m/z 81(+), 95(+), 109(+), 123(+), 135(+), 149(+) and 205(+)), are accounted for. Considerable fragmentation of bicyclic sesquiterpenes, i.e. beta-caryophyllene and alpha-humulene, cause the accuracy to be reduced to 50% if only the parent ion (m/z 205(+)) is considered. These findings were applied to a field dataset collected above a deciduous forest at the PROPHET (Program for Research on Oxidants: Photochemistry, Emissions, and Transport) research station in 2005. Inferred average daytime ecosystem scale mixing ratios (fluxes) of isoprene, sum of monoterpenes (MT), and sum of SQT exhibited values of 15 mu g m(-3) (4.5 mg m(-2) h(-1)), 1.2 mu g m(-3) (0.21 mg m(-2) h(-1)), and 0.0016 mu g m(-3) (0.10 mg m(-2) h(-1)), respectively. A range of MT and SQT reactivities with respect to the OH radical was calculated and compared to an earlier study inferring significantly underestimated OH reactivities due to unknown terpenes above this deciduous forest. The results indicate that incorporating these MT and SQT results can resolve similar to 30% of missing OH reactivity reported for this site.
引用
收藏
页码:99 / 112
页数:14
相关论文
共 50 条
[21]   ORGANIC-CHEMICALS IN THE AIR AT WHITAKER FOREST SIERRA-NEVADA MOUNTAINS, CALIFORNIA [J].
HELMIG, D ;
AREY, J .
SCIENCE OF THE TOTAL ENVIRONMENT, 1992, 112 (2-3) :233-250
[22]   Sesquiterpene emissions from pine trees - Identifications, emission rates and flux estimates for the contiguous United States [J].
Helmig, Detlev ;
Ortega, John ;
Duhl, Tiffany ;
Tanner, David ;
Guenther, Alex ;
Harley, Peter ;
Wiedinmyer, Christine ;
Milford, Jana ;
Sakulyanontvittaya, Tanarit .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2007, 41 (05) :1545-1553
[23]   The application of proton transfer reaction-mass spectrometry (PTR-MS) to the monitoring and analysis of volatile organic compounds in the atmosphere [J].
Hewitt, CN ;
Hayward, S ;
Tani, A .
JOURNAL OF ENVIRONMENTAL MONITORING, 2003, 5 (01) :1-7
[24]   Formation of organic aerosols from the oxidation of biogenic hydrocarbons [J].
Hoffmann, T ;
Odum, JR ;
Bowman, F ;
Collins, D ;
Klockow, D ;
Flagan, RC ;
Seinfeld, JH .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 1997, 26 (02) :189-222
[25]  
HOFFMANN T, 1995, FRESEN J ANAL CHEM, V351, P41
[26]   Observations of oxidation products above a forest imply biogenic emissions of very reactive compounds [J].
Holzinger, R ;
Lee, A ;
Paw, KT ;
Goldstein, AH .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2005, 5 :67-75
[27]   Gas and particle products distribution from the reaction of β-caryophyllene with ozone [J].
Jaoui, M ;
Leungsakul, S ;
Kamens, RM .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 2003, 45 (03) :261-287
[28]   Exchange processes of volatile organic compounds above a tropical rain forest: Implications for modeling tropospheric chemistry above dense vegetation [J].
Karl, T ;
Potosnak, M ;
Guenther, A ;
Clark, D ;
Walker, J ;
Herrick, JD ;
Geron, C .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D18) :D183061-19
[29]   The bi-directional exchange of oxygenated VOCs between a loblolly pine (Pinus taeda) plantation and the atmosphere [J].
Karl, T ;
Harley, P ;
Guenther, A ;
Rasmussen, R ;
Baker, B ;
Jardine, K ;
Nemitz, E .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2005, 5 :3015-3031
[30]   Eddy covariance measurements of oxygenated volatile organic compound fluxes from crop harvesting using a redesigned proton-transfer-reaction mass spectrometer [J].
Karl, T ;
Guenther, A ;
Lindinger, C ;
Jordan, A ;
Fall, R ;
Lindinger, W .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D20) :24157-24167