Nitrate and oxidized organic ions in single particle mass spectra during the 1999 Atlanta Supersite Project

被引:63
作者
Lee, SH
Murphy, DM
Thomson, DS
Middlebrook, AM
机构
[1] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[2] NOAA, Aeron Lab, Boulder, CO 80305 USA
关键词
nitrate aerosol; organic acids; organic aerosol; single particle mass spectrometry; Southern Oxidants Study Atlanta; chemical composition;
D O I
10.1029/2001JD001455
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] We measured the chemical components of 0.35-2.5 mum diameter aerosols with a Particle Analysis by Laser Mass Spectrometry ( PALMS) instrument during the Atlanta Supersite Project in August 1999. This paper presents the results for nitrate and oxidized organics. More than 20% of the negative ion spectra of single particles contained nitrate ion peaks. Nitrate peaks showed a clear maximum during the morning at the time of high ambient relative humidity. Nitrate peaks also had a small local maximum during the afternoon when the gas-phase HNO3 concentrations were high. This afternoon maximum was more significant for the particles containing soot/hydrocarbons or aluminosilicate components than for the typical organic/sulfate particles. About 45% of negative spectra contained ions indicative of the oxidized organics. Oxidized organic peaks showed a diurnal variation similar to the nitrate: a morning time maximum during the relative humidity maximum and a small maximum in the afternoon. However, in contrast to the nitrate peaks, the afternoon local maximum of oxidized organic peaks was apparent on the organic/sulfate particles. Both nitrate and oxidized organic peaks had larger ion fractions in particles with higher scattered light intensities.
引用
收藏
页数:8
相关论文
共 38 条
[1]   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
[2]   Secondary organic aerosol formation in cloud and fog droplets: a literature evaluation of plausibility [J].
Blando, JD ;
Turpin, BJ .
ATMOSPHERIC ENVIRONMENT, 2000, 34 (10) :1623-1632
[3]   KINETICS AND MECHANISM OF THE FORMATION OF HYDROXYMETHANESULFONIC ACID AT LOW PH [J].
BOYCE, SD ;
HOFFMANN, MR .
JOURNAL OF PHYSICAL CHEMISTRY, 1984, 88 (20) :4740-4746
[4]   Carboxylic acids in the troposphere, occurrence, sources, and sinks: A review [J].
Chebbi, A ;
Carlier, P .
ATMOSPHERIC ENVIRONMENT, 1996, 30 (24) :4233-4249
[5]   Thermodynamic model of the system H+-NH4+-SO42--NO3--H2O at tropospheric temperatures [J].
Clegg, SL ;
Brimblecombe, P ;
Wexler, AS .
JOURNAL OF PHYSICAL CHEMISTRY A, 1998, 102 (12) :2137-2154
[6]   Role of mineral aerosol as a reactive surface in the global troposphere [J].
Dentener, FJ ;
Carmichael, GR ;
Zhang, Y ;
Lelieveld, J ;
Crutzen, PJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D17) :22869-22889
[7]   Measurement of hydroxymethanesulfonate in atmospheric aerosols [J].
Dixon, RW ;
Aasen, H .
ATMOSPHERIC ENVIRONMENT, 1999, 33 (13) :2023-2029
[8]   A laboratory study of the heterogeneous reaction of nitric acid on calcium carbonate particles [J].
Goodman, AL ;
Underwood, GM ;
Grassian, VH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D23) :29053-29064
[9]   PARAMETERIZATION OF THE FORMATION POTENTIAL OF SECONDARY ORGANIC AEROSOLS [J].
GROSJEAN, D ;
SEINFELD, JH .
ATMOSPHERIC ENVIRONMENT, 1989, 23 (08) :1733-1747
[10]   Organic atmospheric aerosols: Review and state of the science [J].
Jacobson, MC ;
Hansson, HC ;
Noone, KJ ;
Charlson, RJ .
REVIEWS OF GEOPHYSICS, 2000, 38 (02) :267-294