The effect of organic coatings on the cloud condensation nuclei activation of inorganic atmospheric aerosol

被引:177
作者
Cruz, CN [1 ]
Pandis, SN [1 ]
机构
[1] Carnegie Mellon Univ, Dept Chem Engn, Pittsburgh, PA 15213 USA
关键词
D O I
10.1029/98JD00979
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Atmospheric aerosols have mixed chemical composition, with a variety of inorganic (e.g., sulfate, nitrate, ammonium, and sodium) and organic species often present in a single particle. In the present study, we investigate experimentally the cloud condensation nuclei (CCN) activation of submicron aerosol consisting of an inorganic core (e.g., ammonium sulfate) coated by an organic film, at typical atmospheric supersaturations. We use two types of organic coatings on the (NH4)(2)SO4 particles. The first is glutaric acid, a CCN active organic found in the atmosphere, and the second species is dioctylphthalate (DOP), a nonhygroscopic organic. The CCN activation of (NH4)(2)SO4-glutaric acid particles was measured at a supersaturation of 0.3%, for different inorganic core sizes and organic film thickness. We found that a coating of glutaric acid increases the CCN activation of an (NH4)(2)SO4 particle and that this behavior can be predicted by Kohler theory. The deviation from Kohler theory for the mixed aerosol was determined by comparing theoretical and experimental CCN activation diameters for the particles and was found to be within experimental error. A thick coating of DOP (at least 70% by mass) did not hinder the activation of (NH4)(2)SO4 particles at supersaturations of 0.5 and 1.0%. The values for the measured activation diameters for the DOP coated (NH4)(2)SO4 particles were within the experimental error determined by the pure inorganic experiments, indicating that DOP was most likely acting as inert mass during activation.
引用
收藏
页码:13111 / 13123
页数:13
相关论文
共 52 条
  • [1] EFFECT OF SURFACTANT LAYERS ON THE SIZE CHANGES OF AEROSOL-PARTICLES AS A FUNCTION OF RELATIVE-HUMIDITY
    ANDREWS, E
    LARSON, SM
    [J]. ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1993, 27 (05) : 857 - 865
  • [2] [Anonymous], 2012, Microphysics of Clouds and Precipitation: Reprinted 1980
  • [3] [Anonymous], 1970, HIGHLY DISPERSED AER
  • [4] Bigg E. K., 1986, Atmospheric Research, V20, P82
  • [5] Bird R.B., 1960, TRANSPORT PHENOMENA, P495
  • [6] TEMPORAL AND SPATIAL VARIATIONS OF PM(2.5) AND PM(10) AEROSOL IN THE SOUTHERN CALIFORNIA AIR-QUALITY STUDY
    CHOW, JC
    WATSON, JG
    FUJITA, EM
    LU, ZQ
    LAWSON, DR
    ASHBAUGH, LL
    [J]. ATMOSPHERIC ENVIRONMENT, 1994, 28 (12) : 2061 - 2080
  • [7] CORRIGAN CE, 1996, 15 ANN C AM ASS AER
  • [8] SURVEY OF MOLECULAR NATURE OF PRIMARY AND SECONDARY COMPONENTS OF PARTICLES IN URBAN AIR BY HIGH-RESOLUTION MASS-SPECTROMETRY
    CRONN, DR
    CHARLSON, RJ
    KNIGHTS, RL
    CRITTENDEN, AL
    APPEL, BR
    [J]. ATMOSPHERIC ENVIRONMENT, 1977, 11 (10) : 929 - 937
  • [9] A study of the ability of pure secondary organic aerosol to act as cloud condensation nuclei
    Cruz, CN
    Pandis, SN
    [J]. ATMOSPHERIC ENVIRONMENT, 1997, 31 (15) : 2205 - 2214
  • [10] FITZGERALD JW, 1973, J ATMOS SCI, V30, P628, DOI 10.1175/1520-0469(1973)030<0628:DOTSSO>2.0.CO