Hygroscopic growth of atmospheric and model humic-like substances

被引:108
作者
Dinar, E. [1 ]
Taraniuk, I.
Graber, E. R.
Anttila, T.
Mentel, T. F.
Rudich, Y.
机构
[1] Weizmann Inst Sci, Dept Environm Sci, IL-76100 Rehovot, Israel
[2] Volcani Ctr, Inst Soil Water & Environm Sci, IL-50250 Bet Dagan, Israel
[3] Res Ctr Julich, Inst Tropospher Chem, D-52425 Julich, Germany
关键词
D O I
10.1029/2006JD007442
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The hygroscopic growth (HG) of humic-like substances (HULIS) extracted from smoke and pollution aerosol particles and of Suwannee River fulvic acid (SRFA, bulk and fractions of different molecular weight) was measured by humidity tandem differential mobility analyzer (H-TDMA). By characterizing physical and chemical parameters such as molecular weight, elemental composition, and surface tension, we test the effect of these parameters on particle interactions with water vapor. For molecular weight-fractionated SRFA fractions, the growth factor at 90% relative humidity was generally inversely proportional to the molecular weight. HULIS extracts from ambient particles are more hygroscopic than all the SRFA fractions and exhibit different hygroscopic properties depending on their origin and residence time in the atmosphere. The results point out some dissimilarities between SRFA and aerosol- derived HULIS. The cloud condensation nuclei (CCN) behavior of the studied materials was predicted on the basis of hygroscopic growth using a recently introduced approach of Kreidenweis et al. (2005) and compared to CCN activity measurements on the same samples (Dinar et al., 2006). It is found that the computational approach (Kreidenweis et al., 2005) works reasonably well for SRFA fractions but is limited in use for the HULIS extracts from aerosol particles. The difficulties arise from uncertainties associated with HG measurements at high relative humidity, which leads to large errors in the predicted CCN activity.
引用
收藏
页数:13
相关论文
共 66 条
[1]   Parameterization of the influence of organic surfactants on aerosol activation [J].
Abdul-Razzak, H ;
Ghan, SJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D3)
[2]   Strong present-day aerosol cooling implies a hot future [J].
Andreae, MO ;
Jones, CD ;
Cox, PM .
NATURE, 2005, 435 (7046) :1187-1190
[3]  
Bragatto P, 2002, FRESEN ENVIRON BULL, V11, P182
[4]  
Brechtel FJ, 2000, J ATMOS SCI, V57, P1854, DOI 10.1175/1520-0469(2000)057<1854:PPCSFH>2.0.CO
[5]  
2
[6]  
Brechtel FJ, 2000, J ATMOS SCI, V57, P1872, DOI 10.1175/1520-0469(2000)057<1872:PPCSFH>2.0.CO
[7]  
2
[8]   Water uptake by particles containing humic materials and mixtures of humic materials with ammonium sulfate [J].
Brooks, SD ;
DeMott, PJ ;
Kreidenweis, SM .
ATMOSPHERIC ENVIRONMENT, 2004, 38 (13) :1859-1868
[9]   Molecular characterization of the water-soluble organic compounds in fogwater by ESIMS/MS [J].
Cappiello, A ;
De Simoni, E ;
Fiorucci, C ;
Mangani, F ;
Palma, P ;
Trufelli, H ;
Decesari, S ;
Facchini, MC ;
Fuzzi, S .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2003, 37 (07) :1229-1240
[10]   Mass transfer effects in hygroscopic measurements of aerosol particles [J].
Chan, MN ;
Chan, CK .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2005, 5 :2703-2712