Integration of size distributions and size-resolved hygroscopicity measured during the Houston Supersite for compositional categorization of the aerosol

被引:75
作者
Gasparini, R [1 ]
Li, RJ [1 ]
Collins, DR [1 ]
机构
[1] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA
关键词
aerosol; DMA; TDMA; hygroscopic; hygroscopicity; organic; Houston; nucleation;
D O I
10.1016/j.atmosenv.2004.03.019
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Measurements of aerosol size distributions and hygroscopicity were combined to infer the size-resolved composition of the ambient aerosol during the Houston Supersite campaign from June through October, 2001. The 3000+ distributions used in this analysis were measured at the Aldine site north and typically downwind of the greater Houston metropolitan area. Size distributions spanning the diameter range from 0.025 to 0.700 mum, and hygroscopic behavior at eight logarithmically spaced dry diameters from 0.025 to 0.344 mum were analyzed. At smaller dry sizes, the aerosol hygroscopic growth factor distributions were typically monomodal and peaked at or near a growth factor of 1.0, indicating predominantly non-hygroscopic aerosols. Particles larger than similar to0.100 mum exhibited bimodal growth patterns, with increasing importance of the hygroscopic mode with increasing dry particle size. Hygroscopic growth distributions were used to partition the aerosol into pure insoluble, mixed insoluble, mixed soluble, and pure soluble categories. This categorization scheme was used to analyze in detail four multi-day episodes. During two of these episodes new particle formation events were observed daily. The recently formed particles were only sparingly hygroscopic, suggesting they were composed primarily of insoluble material. To contrast these periods during which pronounced diurnal variability was observed, a third period was chosen because the aerosol concentration and composition varied little. The fourth period analyzed spanned the passage of a cold front, which had a pronounced influence on the aerosol distributions. (C) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:3285 / 3303
页数:19
相关论文
共 29 条
[1]  
ALLEN D, 2002, PARTICULATE MATTER C
[2]  
Brechtel FJ, 2000, J ATMOS SCI, V57, P1854, DOI 10.1175/1520-0469(2000)057<1854:PPCSFH>2.0.CO
[3]  
2
[4]   Growth and deposition of hygroscopic particulate matter in the human lungs [J].
Broday, DM ;
Georgopoulos, PG .
AEROSOL SCIENCE AND TECHNOLOGY, 2001, 34 (01) :144-159
[5]   Gas-to-particle conversion in the atmosphere: I. Evidence from empirical atmospheric aerosols [J].
Clement, CF ;
Ford, IJ .
ATMOSPHERIC ENVIRONMENT, 1999, 33 (03) :475-487
[6]   Hygroscopic properties of Pasadena, California aerosol [J].
Cocker, DR ;
Whitlock, NE ;
Flagan, RC ;
Seinfeld, JH .
AEROSOL SCIENCE AND TECHNOLOGY, 2001, 35 (02) :637-647
[7]   Deliquescence and hygroscopic growth of mixed inorganic-organic atmospheric aerosol [J].
Cruz, CN ;
Pandis, SN .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2000, 34 (20) :4313-4319
[8]   REACTION OF N2O5 ON TROPOSPHERIC AEROSOLS - IMPACT ON THE GLOBAL DISTRIBUTIONS OF NOX, O3, AND OH [J].
DENTENER, FJ ;
CRUTZEN, PJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1993, 98 (D4) :7149-7163
[9]   Direct measurements and parameterisation of aerosol flux, concentration and emission velocity above a city [J].
Dorsey, JR ;
Nemitz, E ;
Gallagher, MW ;
Fowler, D ;
Williams, PI ;
Bower, KN ;
Beswick, KM .
ATMOSPHERIC ENVIRONMENT, 2002, 36 (05) :791-800
[10]   GROWTH LAWS FOR ATMOSPHERIC AEROSOL-PARTICLES - AN EXAMINATION OF THE BIMODALITY OF THE ACCUMULATION-MODE [J].
KERMINEN, VM ;
WEXLER, AS .
ATMOSPHERIC ENVIRONMENT, 1995, 29 (22) :3263-3275