FTIR spectroscopic investigation of the mechanism and kinetics of the heterogeneous reactions of NO2 and HNO3 with soot

被引:152
作者
Kirchner, U [1 ]
Scheer, V [1 ]
Vogt, R [1 ]
机构
[1] Ford Forsch Zentrum Aachen GmbH, D-52072 Aachen, Germany
关键词
D O I
10.1021/jp0005322
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Soot samples from a spark generator, a flame, and a diesel passenger car were either collected on a Teflon filter and transferred to an IR-transparent window or deposited directly from a flame onto the window and investigated by Fourier transform infrared (FTIR) spectroscopy. The soot-covered windows were mounted in a 10 cm vacuum cell connected to a standard flow system with He as carrier gas. Reactive gases, such as NO2 and HNO3, were added to the carrier gas flow at a concentration of (0.016 to 2.5) x 10(14) molecule cm(-3). FTIR spectra of soot samples before and after exposure to HNO3, NO2, and O-3 are presented. Formation of IR absorption bands was analyzed as a function of exposure time. IR bands attributable to soot surface oxidation products and nitrogen containing species, e.g. -C=O, R-NO2, R-ONO2, and R-ONO were observed. The observed time dependence of the absorption bands of the spark generator soot can be fitted by two parallel reactions, a slow and a fast process. Both processes have a reaction order of n approximate to 0.2 (+/-0.3) for the NO2 + soot reaction and n approximate to 0.5 (+/-0.6) for the HNO3 + soot reaction. The number of active sites, N-max = 2.2 x 10(14) molecules cm(-2) soot surface, has been estimated from saturation experiments. Surface reaction probabilities depend on reactant concentration and reaction time and were in the range of gamma approximate to 10(-6) to 10(-8) for the slow, and gamma approximate to 10(-3) to 10(-6) for the fast processes. The reaction probability on diesel engine soot was nearly 1 order of magnitude slower. It is concluded that the reaction of NO2, with soot cannot account for the HONO levels observed in urban air.
引用
收藏
页码:8908 / 8915
页数:8
相关论文
共 32 条
[11]   HNO3/NOx ratio in the remote troposphere during MLOPEX 2: Evidence for nitric acid reduction on carbonaceous aerosols? [J].
Hauglustaine, DA ;
Ridley, BA ;
Solomon, S ;
Hess, PG ;
Madronich, S .
GEOPHYSICAL RESEARCH LETTERS, 1996, 23 (19) :2609-2612
[12]   THE ORIGIN OF INFRARED-ABSORPTION BANDS OF SOOT IN THE REGION 750 TO 900 CM-1 [J].
JASSIM, JA ;
LU, HP ;
CHUGHTAI, AR ;
SMITH, DM .
APPLIED SPECTROSCOPY, 1986, 40 (01) :113-116
[13]   Heterogeneous chemical processing of (NO2)-N-13 by monodisperse carbon aerosols at very low concentrations [J].
Kalberer, M ;
Tabor, K ;
Ammann, M ;
Parrat, Y ;
Weingartner, E ;
Piguet, D ;
Rossler, E ;
Jost, DT ;
Turler, A ;
Gaggeler, HW ;
Baltensperger, U .
JOURNAL OF PHYSICAL CHEMISTRY, 1996, 100 (38) :15487-15493
[14]   The heterogeneous reaction of ozone with soot aerosol [J].
Kamm, S ;
Möhler, O ;
Naumann, KH ;
Saathoff, H ;
Schurath, U .
ATMOSPHERIC ENVIRONMENT, 1999, 33 (28) :4651-4661
[15]  
KAMM S, 1997, PSI P, V97, P29
[16]   Characterization of the particulate phase in the exhaust from a diesel car [J].
Kerminen, VM ;
Makela, TE ;
Ojanen, CH ;
Hillamo, RE ;
Vilhunen, JK ;
Rantanen, L ;
Havers, N ;
VonBohlen, A ;
Klockow, D .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1997, 31 (07) :1883-1889
[17]  
KIRCHNER U, 1999, P EUROTRAC S 98, V1, P666
[18]  
KLEFFMANN J, 1999, P EUROTRAC S 98, V1, P656
[19]   WATER NUCLEATION PROPERTIES OF CARBON-BLACK AND DIESEL SOOT PARTICLES [J].
LAMMEL, G ;
NOVAKOV, T .
ATMOSPHERIC ENVIRONMENT, 1995, 29 (07) :813-823
[20]   Carbon aerosols and atmospheric photochemistry [J].
Lary, DJ ;
Lee, AM ;
Toumi, R ;
Newchurch, MJ ;
Pirre, M ;
Renard, JB .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D3) :3671-3682