Sensitivity and specificity of atmospheric trace gas detection by proton-transfer-reaction mass spectrometry

被引:279
作者
de Gouw, J
Warneke, C
Karl, T
Eerdekens, G
van der Veen, C
Fall, R
机构
[1] NOAA, Aeron Lab, Boulder, CO 80303 USA
[2] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[3] Univ Utrecht, Inst Marine & Atmospher Res, Utrecht, Netherlands
[4] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[5] Univ Colorado, Dept Chem & Biochem, Boulder, CO 80309 USA
基金
奥地利科学基金会; 美国国家科学基金会;
关键词
volatile organic compounds; proton-transfer-reaction mass spectrometry; atmospheric trace gas;
D O I
10.1016/S1387-3806(02)00926-0
中图分类号
O64 [物理化学(理论化学)、化学物理学]; O56 [分子物理学、原子物理学];
学科分类号
070203 ; 070304 ; 081704 ; 1406 ;
摘要
Proton-transfer-reaction mass spectrometry (PTR-MS) has emerged as a useful tool to study the atmospheric chemistry of volatile organic compounds (VOCs), which are implicated in the formation of ozone and aerosols in polluted air. In PTR-MS, ambient air is continuously pumped through a drift-tube reactor and the VOCs in the sample are ionized using proton-transfer reactions with H3O+ ions. The H3O+ and product ions are detected with a quadrupole mass spectrometer. The technique combines a fast response time (I s) with a low detection limit (10-100 parts-per-trillion), and allows atmospheric measurements of many important VOCs and their oxidation products in a variety of field experiments. Here, the sensitivity of PTR-MS with respect to a number of VOCs is characterized. The measured sensitivity, obtained using calibrated mixtures of VOCs in air, is compared with a calculated sensitivity and a reasonable agreement is obtained. It is shown how the sensitivity depends on the pressure in the drift tube and on the humidity of the sample air. In PTR-MS, only the mass of the ionized trace gases is determined, which is a useful but not a unique indicator of the trace gas identity. A combination of gas chromatography and PTR-MS (GC-PTR-MS) has been developed to investigate which compounds contribute to the signal at a certain mass. Air samples collected in the city of Utrecht in The Netherlands and at the remote Sonnblick Observatory in Austria were analyzed by GC-PTR-MS. The results clearly indicate that PTR-MS measurements of VOCs such as methanol, acetonitrile, acetaldehyde, benzene and toluene are free from interference by other compounds. For other VOCs, such as acetone and methyl ethyl ketone, interference cannot always be ruled out entirely. For some masses like 69 amu, a large number of biogenic VOCs produce the same signal, demonstrating the need for GC-PTR-MS methods. It is also shown that PTR-MS measurements can likely be used to determine the sum of the concentration of C-2-benzenes, despite the fact that these compounds cannot be independently measured with PTR-MS. (C) 2002 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:365 / 382
页数:18
相关论文
共 47 条
[11]   Biogenic C5VOCs: release from leaves after freeze-thaw wounding and occurrence in air at a high mountain observatory [J].
Fall, R ;
Karl, T ;
Jordon, A ;
Lindinger, W .
ATMOSPHERIC ENVIRONMENT, 2001, 35 (22) :3905-3916
[12]   Volatile organic compounds emitted after leaf wounding: On-line analysis by proton-transfer-reaction mass spectrometry [J].
Fall, R ;
Karl, T ;
Hansel, A ;
Jordan, A ;
Lindinger, W .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D13) :15963-15974
[13]   Tropospheric air pollution: Ozone, airborne toxics, polycyclic aromatic hydrocarbons, and particles [J].
FinlaysonPitts, BJ ;
Pitts, JN .
SCIENCE, 1997, 276 (5315) :1045-1052
[14]  
FISHER AJ, UNPUB PLANT BIOL
[15]  
GOLDAN PG, COMMUNICATION
[16]   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
[17]   Energy dependencies of the proton transfer reactions H3O++CH2O↔CH2OH++H2O [J].
Hansel, A ;
Singer, W ;
Wisthaler, A ;
Schwarzmann, M ;
Lindinger, W .
INTERNATIONAL JOURNAL OF MASS SPECTROMETRY, 1997, 167 :697-703
[18]  
Hewitt C. N., 1999, REACTIVE HYDROCARBON
[19]   Biomass burning as a source of formaldehyde, acetaldehyde, methanol, acetone, acetonitrile, and hydrogen cyanide [J].
Holzinger, R ;
Warneke, C ;
Hansel, A ;
Jordan, A ;
Lindinger, W ;
Scharffe, DH ;
Schade, G ;
Crutzen, PJ .
GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (08) :1161-1164
[20]   Fast time response measurements of HNO3 in air with a chemical ionization mass spectrometer [J].
Huey, LG ;
Dunlea, EJ ;
Lovejoy, ER ;
Hanson, DR ;
Norton, RB ;
Fehsenfeld, FC ;
Howard, CJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D3) :3355-3360