Free radicals and fast photochemistry during BERLIOZ

被引:102
作者
Platt, U [1 ]
Alicke, B
Dubois, R
Geyer, A
Hofzumahaus, A
Holland, F
Martinez, M
Mihelcic, D
Klüpfel, T
Lohrmann, B
Pätz, W
Perner, D
Rohrer, F
Schäfer, J
Stutz, J
机构
[1] Univ Heidelberg, INF 229, Inst Umweltphys, D-69120 Heidelberg, Germany
[2] Forschungszentrum Julich, Julich, Germany
[3] MPI Chem, Mainz, Germany
[4] Inst Tropospharenforsch, Leipzig, Germany
关键词
free radicals; photochemistry; hydroxyl radical; nitrate radical; peroxy radical; spectroscopy; modelling;
D O I
10.1023/A:1015707531660
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The free radicals OH, HO2, RO2, and NO3 are known to be the driving force for most chemical processes in the atmosphere. Since the low concentration of the above radicals makes measurements particularly difficult, only relatively few direct measurements of free radical concentrations have been reported to date. We present a comprehensive set of simultaneous radical measurements performed by Laser Induced Fluorescence (LIF), Matrix Isolation - Electron spin Resonance (MI-ESR), Peroxy Radical Chemical Amplification (PERCA), and Differential Optical Absorption Spectroscopy (DOAS) during the BERLIner OZonexperiment (BERLIOZ) during July and August of 1998 near Berlin, Germany. Most of the above radical species were measured by more than one technique and an intercomparison gave good agreement. This data set offered the possibility to study and quantify the role of each radical at a rural, semi-polluted site in the continental boundary layer and to investigate interconnections and dependencies among these free radicals. In general (box) modelled diurnal profiles of the different radicals reproduced the measurements quite well, however measured absolute levels are frequently lower than model predictions. These discrepancies point to disturbing deficiencies in our understanding of the chemical system in urban air masses. In addition considerable night-time peroxy radical production related to VOC reactions with NO3 and O-3 could be quantified.
引用
收藏
页码:359 / 394
页数:36
相关论文
共 83 条
[1]  
ALICKE B, 2001, UNPUB J GEOPHYS RES
[2]   Observations of the nitrate radical in the marine boundary layer [J].
Allan, BJ ;
Carslaw, N ;
Coe, H ;
Burgess, RA ;
Plane, JMC .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 1999, 33 (02) :129-154
[3]   Chemical ionization mass spectrometer for long-term measurements of atmospheric OH and H2SO4 [J].
Berresheim, H ;
Elste, T ;
Plass-Dülmer, C ;
Eisele, FL ;
Tanner, DJ .
INTERNATIONAL JOURNAL OF MASS SPECTROMETRY, 2000, 202 (1-3) :91-109
[4]   In-situ measurements of tropospheric hydroxyl radicals by folded long-path laser absorption during the field campaign POPCORN [J].
Brandenburger, U ;
Brauers, T ;
Dorn, HP ;
Hausmann, M ;
Ehhalt, DH .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 1998, 31 (1-2) :181-204
[5]   Intercomparison of tropospheric OH radical measurements by multiple folded long-path laser absorption and laser induced fluorescence [J].
Brauers, T ;
Aschmutat, U ;
Brandenburger, U ;
Dorn, HP ;
Hausmann, M ;
Hessling, M ;
Hofzumahaus, A ;
Holland, F ;
PlassDulmer, C ;
Ehhalt, DH .
GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (18) :2545-2548
[6]   INTERHEMISPHERIC ASYMMETRY IN OH ABUNDANCE INFERRED FROM MEASUREMENTS OF ATMOSPHERIC (CO)-C-14 [J].
BRENNINKMEIJER, CAM ;
MANNING, MR ;
LOWE, DC ;
WALLACE, G ;
SPARKS, RJ ;
VOLZTHOMAS, A .
NATURE, 1992, 356 (6364) :50-52
[7]  
BRUNE WH, 1995, J ATMOS SCI, V52, P3328, DOI 10.1175/1520-0469(1995)052<3328:MOAHIT>2.0.CO
[8]  
2
[9]   Airborne in-situ OH and HO2 observations in the cloud-free troposphere and lower stratosphere during SUCCESS [J].
Brune, WH ;
Faloona, IC ;
Tan, D ;
Weinheimer, AJ ;
Campos, T ;
Ridley, BA ;
Vay, SA ;
Collins, JE ;
Sachse, GW ;
Jaegle, L ;
Jacob, DJ .
GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (10) :1701-1704
[10]   CHEMICAL MECHANISMS OF ACID GENERATION IN THE TROPOSPHERE [J].
CALVERT, JG ;
LAZRUS, A ;
KOK, GL ;
HEIKES, BG ;
WALEGA, JG ;
LIND, J ;
CANTRELL, CA .
NATURE, 1985, 317 (6032) :27-35