CCN activation of pure and coated carbon black particles

被引:104
作者
Dusek, U [1 ]
Reischl, GP [1 ]
Hitzenberger, R [1 ]
机构
[1] Univ Vienna, Inst Phys Expt, A-1090 Vienna, Austria
关键词
D O I
10.1021/es0503478
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The CCN (cloud condensation nucleus) activation of pure and coated carbon black particles was investigated using the University of Vienna cloud condensation nuclei counter Giebl, H.; Berner, A.; Reischl, G.; Puxbaum, H.; KasperGiebl, A.; Hitzenberger, R. J. Aerosol Sci. 2002, 33, 16231634). The particles were produced by nebulizing an aqueous suspension of carbon black in a Collison atomizer. The activation of pure carbon black particles was found to require higher supersaturations than predicted by calculations representing the particles as insoluble, wettable spheres with mobility equivalent diameter. To test whether this effect is an artifact due to heating of the light-absorbing carbon black particles in the laser beam, experiments at different laser powers were conducted. No systematic dependence of the activation of pure carbon black particles on laser power was observed. The observations could be modeled using spherical particles and an effective contact angle of 4-6 degrees of water at their surface. The addition of a small amount of NaCl to the carbon black particles (by adding 5% by mass NaCl to the carbon black suspension) greatly enhanced their CCN efficiency. The measured CCN efficiencies were consistent with Kohler theory for particles consisting of insoluble and hygroscopic material. However, coating the carbon black particles with hexadecanol (a typical film-forming compound with one hydrophobic and one hydrophilic end) efficiently suppressed the CCN activation of the carbon black particles.
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页码:1223 / 1230
页数:8
相关论文
共 37 条
[1]   EFFECT OF SURFACTANT LAYERS ON THE SIZE CHANGES OF AEROSOL-PARTICLES AS A FUNCTION OF RELATIVE-HUMIDITY [J].
ANDREWS, E ;
LARSON, SM .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1993, 27 (05) :857-865
[2]   CCN activation of slightly soluble organics: the importance of small amounts of inorganic salt and particle phase [J].
Bilde, M ;
Svenningsson, B .
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2004, 56 (02) :128-134
[3]   A technology-based global inventory of black and organic carbon emissions from combustion [J].
Bond, TC ;
Streets, DG ;
Yarber, KF ;
Nelson, SM ;
Woo, JH ;
Klimont, Z .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2004, 109 (D14) :D14203
[4]   Air traffic may increase cirrus cloudiness [J].
Boucher, O .
NATURE, 1999, 397 (6714) :30-31
[5]   Partially soluble organics as cloud condensation nuclei: Role of trace soluble and surface active species [J].
Broekhuizen, K ;
Kumar, PP ;
Abbatt, JPD .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (01) :L011071-5
[6]   Black carbon radiative heating effects on cloud microphysics and implications for the aerosol indirect effect - 1. Extended Kohler theory [J].
Conant, WC ;
Nenes, A ;
Seinfeld, JH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2002, 107 (D21)
[7]   Construction of a 1° x 1° fossil fuel emission data set for carbonaceous aerosol and implementation and radiative impact in the ECHAM4 model [J].
Cooke, WF ;
Liousse, C ;
Cachier, H ;
Feichter, J .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D18) :22137-22162
[8]   A global black carbon aerosol model [J].
Cooke, WF ;
Wilson, JJN .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D14) :19395-19409
[9]   The effect of organic coatings on the cloud condensation nuclei activation of inorganic atmospheric aerosol [J].
Cruz, CN ;
Pandis, SN .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D11) :13111-13123
[10]   The susceptibility of ice formation in upper tropospheric clouds to insoluble aerosol components [J].
DeMott, PJ ;
Rogers, DC ;
Kreidenweis, SM .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D16) :19575-19584