OH formation by HONO photolysis during the BERLIOZ experiment -: art. no. 8247

被引:239
作者
Alicke, B [1 ]
Geyer, A
Hofzumahaus, A
Holland, F
Konrad, S
Pätz, HW
Schäfer, J
Stutz, J
Volz-Thomas, A
Platt, U
机构
[1] Heidelberg Univ, Inst Umweltphys, INF 229, D-69120 Heidelberg, Germany
[2] Forschungszentrum Julich, Stettiner Staatsforst, D-52425 Julich, Germany
[3] Univ Calif Los Angeles, Dept Atmospher Sci, Los Angeles, CA 90095 USA
关键词
HONO; photochemistry; OH; photolysis; HCHO; ozone;
D O I
10.1029/2001JD000579
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] The photolysis of nitrous acid (HONO) in the early morning hours is an important source of OH radicals, the most important daytime oxidizing species. Although the importance of this mechanism has been recognized for many years, no accurate quantification of this OH source is available, and the role of HONO photolysis is often underestimated. We present measurements of HONO and its precursor NO2 by Differential Optical Absorption Spectroscopy (DOAS) during the Berliner Ozonexperiment (BERLIOZ) field campaign in July/August 1998 at Pabstthum near Berlin, Germany. HONO concentrations, formation rates, and simultaneously measured HONO photolysis frequencies are used to calculate the total amount of OH formed by HONO photolysis during a full diurnal cycle. A comparison with the OH formation by photolysis of O-3 and HCHO and by the reaction of alkenes with ozone shows that HONO photolysis contributed up to 20% of the total OH formed in a 24 hour period during this campaign. In the morning hours, HONO photolysis was by far the most important OH source during BERLIOZ.
引用
收藏
页数:17
相关论文
共 82 条
[1]   Impact of nitrous acid photolysis on the total hydroxyl radical budget during the Limitation of Oxidant Production/Pianura Padana Produzione di Ozono study in Milan [J].
Alicke, B ;
Platt, U ;
Stutz, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D22)
[2]  
ALLEGRINI I, 1995, ANN CHIM-ROME, V85, P471
[3]   Heterogeneous production of nitrous acid on soot in polluted air masses [J].
Ammann, M ;
Kalberer, M ;
Jost, DT ;
Tobler, L ;
Rössler, E ;
Piguet, D ;
Gäggeler, HW ;
Baltensperger, U .
NATURE, 1998, 395 (6698) :157-160
[4]   Gas-phase tropospheric chemistry of volatile organic compounds .1. Alkanes and alkenes [J].
Atkinson, R .
JOURNAL OF PHYSICAL AND CHEMICAL REFERENCE DATA, 1997, 26 (02) :215-290
[5]   OH RADICAL PRODUCTION FROM THE GAS-PHASE REACTIONS OF O-3 WITH A SERIES OF ALKENES UNDER ATMOSPHERIC CONDITIONS [J].
ATKINSON, R ;
ASCHMANN, SM .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1993, 27 (07) :1357-1363
[6]   A modeling study of the nighttime radical chemistry in the lower continental troposphere 2.: Origin and evolution of HOx [J].
Bey, I ;
Aumont, B ;
Toupance, G .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D9) :9991-10001
[7]   IMPROVEMENT OF DIFFERENTIAL OPTICAL-ABSORPTION SPECTROSCOPY WITH A MULTICHANNEL SCANNING TECHNIQUE [J].
BRAUERS, T ;
HAUSMANN, M ;
BRANDENBURGER, U ;
DORN, HP .
APPLIED OPTICS, 1995, 34 (21) :4472-4479
[8]   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
[9]   AN EVALUATION OF THE MECHANISM OF NITROUS-ACID FORMATION IN THE URBAN ATMOSPHERE [J].
CALVERT, JG ;
YARWOOD, G ;
DUNKER, AM .
RESEARCH ON CHEMICAL INTERMEDIATES, 1994, 20 (3-5) :463-502
[10]   KINETIC STUDY OF HONO FORMATION AND DECAY REACTIONS IN GASEOUS MIXTURES OF HONO, NO, NO2, H2O, AND N2 [J].
CHAN, WH ;
NORDSTROM, RJ ;
CALVERT, JG ;
SHAW, JH .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1976, 10 (07) :674-682