On the formation, growth and composition of nucleation mode particles

被引:475
作者
Kulmala, M [1 ]
Dal Maso, M [1 ]
Mäkelä, JM [1 ]
Pirjola, L [1 ]
Väkevä, M [1 ]
Aalto, P [1 ]
Miikkulainen, P [1 ]
Hämeri, K [1 ]
O'Dowd, CD [1 ]
机构
[1] Univ Helsinki, Dept Phys, FIN-00014 Helsinki, Finland
来源
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY | 2001年 / 53卷 / 04期
关键词
D O I
10.1034/j.1600-0889.2001.d01-33.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Taking advantage of only the measured aerosol particles spectral evolution as a function of time, a new analytical tool is developed to derive formation and growth properties of nucleation mode aerosols. This method, when used with hygroscopic growth-factors, can also estimate basic composition properties of these recently-formed particles. From size spectra the diameter growth-rate can be obtained, and aerosol condensation and coagulation sinks can be calculated. Using this growth-rate and condensation sink, the concentration of condensable vapours and their source rate can be estimated. Then, combining the coagulation sink together with measured number concentrations and apparent source rates of 3 run particles, I nm particle nucleation rates and concentration can be estimated. To estimate nucleation rates and vapour concentration source rates producing new particle bursts over the Boreal forest regions, three cases from the BIOFOR project were examined using this analytical tool. In this environment, the nucleation mode growth-rate was observed to be 2-3 nm hour(-1), which required a condensable vapour concentration of 2.5-4 x 10(7) cm(-3) and a source rate of approximately 7.5-11 x 10(4) cm(-3) s(-1) to be sustained. The formation rate of 3 nm particles was approximate to 1 particle cm(-)3 s(-1) in all three cases. The estimated formation rate of 1 nm particles was 10-100 particles cm(-3) s(-1), while their concentration was estimated to be between 10,000 and 100,000 particles cm(-3). Using hygroscopicity data and mass flux expressions, the mass flux of insoluble vapour is estimated to be of the same order of magnitude as that of soluble vapour, with a soluble to insoluble vapour flux ratio ranging from 0.7 to 1.4 during these nucleation events.
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页码:479 / 490
页数:12
相关论文
共 31 条
  • [1] Physical characterization of aerosol particles during nucleation events
    Aalto, P
    Hämeri, K
    Becker, E
    Weber, R
    Salm, J
    Mäkelä, JM
    Hoell, C
    O'Dowd, CD
    Karlsson, H
    Hansson, HC
    Väkevä, M
    Koponen, IK
    Buzorius, G
    Kulmala, M
    [J]. TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2001, 53 (04): : 344 - 358
  • [2] SLIP CORRECTION MEASUREMENTS OF SPHERICAL SOLID AEROSOL-PARTICLES IN AN IMPROVED MILLIKAN APPARATUS
    ALLEN, MD
    RAABE, OG
    [J]. AEROSOL SCIENCE AND TECHNOLOGY, 1985, 4 (03) : 269 - 286
  • [3] Birmili W, 1998, J AEROSOL SCI, V29, pS1015, DOI DOI 10.1016/S0021-8502(98)90690-5
  • [4] OCEANIC PHYTOPLANKTON, ATMOSPHERIC SULFUR, CLOUD ALBEDO AND CLIMATE
    CHARLSON, RJ
    LOVELOCK, JE
    ANDREAE, MO
    WARREN, SG
    [J]. NATURE, 1987, 326 (6114) : 655 - 661
  • [5] Ultrafine (nanometre) particle mediated lung injury
    Donaldson, K
    Li, XY
    MacNee, W
    [J]. JOURNAL OF AEROSOL SCIENCE, 1998, 29 (5-6) : 553 - 560
  • [6] Fuchs N. A., 1971, TOPICS CURRENT AEROS
  • [7] Fuchs N.A., 1964, MECH AEROSOLS
  • [8] Hygroscopic growth of ultrafine ammonium sulphate aerosol measured using an ultrafine tandem differential mobility analyzer
    Hämeri, K
    Väkevä, M
    Hansson, HC
    Laaksonen, A
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D17) : 22231 - 22242
  • [9] Hämeri K, 2001, TELLUS B, V53, P359, DOI 10.1034/j.1600-0889.2001.d01-26.x
  • [10] Formation of atmospheric particles from organic acids produced by forests
    Kavouras, IG
    Mihalopoulos, N
    Stephanou, EG
    [J]. NATURE, 1998, 395 (6703) : 683 - 686