Dependence of CCN activity of less volatile particles on the amount of coating observed in Tokyo

被引:50
作者
Kuwata, M.
Kondo, Y.
Mochida, M.
Takegawa, N.
Kawamura, K.
机构
[1] Univ Tokyo, Adv Sci & Technol Res Ctr, Meguro Ku, Tokyo 1538904, Japan
[2] Hokkaido Univ, Inst Low Temp Sci, Kita Ku, Sapporo, Hokkaido 0600819, Japan
关键词
BLACK CARBON AEROSOL; FOSSIL-FUEL; NONVOLATILE FRACTIONS; ATMOSPHERIC AEROSOLS; CLIMATE RESPONSE; SOOT; SIZE; MOBILITY; HYGROSCOPICITY; SULFATE;
D O I
10.1029/2006JD007758
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] A novel observation system has been developed to measure cloud condensation nuclei (CCN) activity simultaneously with volatility of aerosol particles at 400 degrees C. CCN/ CN ratios were measured using a CCN counter and a condensation particle counter, and volatility was measured with a volatility tandem differential mobility analyzer (VTDMA). This system was connected to a hygroscopicity tandem differential mobility analyzer in tandem to measure these properties of hygroscopicity-selected particles. These instruments were deployed in Tokyo in November 2004. In Tokyo, the dominant fraction of nonvolatile cores at 400 degrees C has been found to be black carbon ( BC). Therefore the number size distribution measured by VTDMA represents the mixing state of black carbon particles. The VTDMA measurement of hygroscopicity-selected particles revealed that most of the less hygroscopic particles were less volatile, while more hygroscopic particles were more volatile. CCN/ CN ratios of less volatile particles [(CCN/CN)(LV)] are estimated from CCN activity and volatility measurements of less hygroscopic particles. (CCN/CN)(LV) at SS = 0.5% is correlated with the decrease of peak diameter due to volatilization (Delta d(m)), and (CCN/CN)(LV) is nearly equal to unity at Delta d(m) = 10 nm. This result suggests that the CCN activity of BC particles significantly depends on the amount of coating.
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页数:9
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