Hygroscopic properties of Amazonian biomass burning and European background HULIS and investigation of their effects on surface tension with two models linking H-TDMA to CCNC data

被引:45
作者
Fors, E. O. [1 ]
Rissler, J. [1 ]
Massling, A. [1 ]
Svenningsson, B. [1 ]
Andreae, M. O. [2 ]
Dusek, U. [2 ]
Frank, G. P. [2 ]
Hoffer, A. [2 ]
Bilde, M. [3 ]
Kiss, G. [4 ]
Janitsek, S. [4 ]
Henning, S. [5 ]
Facchini, M. C. [6 ]
Decesari, S. [6 ]
Swietlicki, E. [1 ]
机构
[1] Lund Univ, Dept Phys, Div Nucl Phys, Lund, Sweden
[2] Max Planck Inst Chem, Dept Biogeochem, D-55128 Mainz, Germany
[3] Univ Copenhagen, Dept Chem, DK-2100 Copenhagen, Denmark
[4] Univ Pannonia, Air Chem Grp, Hungarian Acad Sci, Veszprem, Hungary
[5] Leibniz Inst Tropospher Res, Dept Phys, Leipzig, Germany
[6] CNR, Ist Sci Atmosfera & Clima, I-40126 Bologna, Italy
关键词
SOLUBLE ORGANIC-COMPOUNDS; ATMOSPHERIC AEROSOLS; CHEMICAL-COMPOSITION; HUMIC-LIKE; FINE AEROSOL; BLACK CARBON; GROWTH; ACTIVATION; PARTICLES; CLIMATE;
D O I
10.5194/acp-10-5625-2010
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
HUmic-LIke Substances (HULIS) have been identified as major contributors to the organic carbon in atmospheric aerosol. The term "HULIS" is used to describe the organic material found in aerosol particles that resembles the humic organic material in rivers and sea water and in soils. In this study, two sets of filter samples from atmospheric aerosols were collected at different sites. One set of samples was collected at the K-puszta rural site in Hungary, about 80 km SE of Budapest, and a second was collected at a site in Rondonia, Amazonia, Brazil, during the Large-Scale Biosphere-Atmosphere Experiment in Amazonia - Smoke Aerosols, Clouds, Rainfall and Climate (LBA-SMOCC) biomass burning season experiment. HULIS were extracted from the samples and their hygroscopic properties were studied using a Hygroscopicity Tandem Differential Mobility Analyzer (H-TDMA) at relative humidity (RH) < 100%, and a cloud condensation nucleus counter (CCNC) at RH > 100%. The H-TDMA measurements were carried out at a dry diameter of 100 nm and for RH ranging from 30 to 98%. At 90% RH the HULIS samples showed diameter growth factors between 1.04 and 1.07, reaching values of 1.4 at 98% RH. The cloud nucleating properties of the two sets of aerosol samples were analysed using two types of thermal static cloud condensation nucleus counters. Two different parameterization models were applied to investigate the potential effect of HULIS surface activity, both yielding similar results. For the K-puszta winter HULIS sample, the surface tension at the point of activation was estimated to be lowered by between 34% (47.7 mN/m) and 31% (50.3 mN/m) for dry sizes between 50 and 120 nm in comparison to pure water. A moderate lowering was also observed for the entire water soluble aerosol sample, including both organic and inorganic compounds, where the surface tension was decreased by between 2% (71.2 mN/m) and 13% (63.3 mN/m).
引用
收藏
页码:5625 / 5639
页数:15
相关论文
共 49 条
  • [1] Aerosol-cloud-precipitation interactions. Part 1. The nature and sources of cloud-active aerosols
    Andreae, M. O.
    Rosenfeld, D.
    [J]. EARTH-SCIENCE REVIEWS, 2008, 89 (1-2) : 13 - 41
  • [2] [Anonymous], 2006, ATMOS CHEM PHYS
  • [3] [Anonymous], ATMOS CHEM PHYS DISC
  • [4] CCN activation of slightly soluble organics: the importance of small amounts of inorganic salt and particle phase
    Bilde, M
    Svenningsson, B
    [J]. TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2004, 56 (02): : 128 - 134
  • [5] Atmospheric science - Reshaping the theory of cloud formation
    Charlson, RJ
    Seinfeld, JH
    Nenes, A
    Kulmala, M
    Laaksonen, A
    Facchini, MC
    [J]. SCIENCE, 2001, 292 (5524) : 2025 - 2026
  • [6] Characterization of the organic composition of aerosols from Rondonia, Brazil, during the LBA-SMOCC 2002 experiment and its representation through model compounds
    Decesari, S
    Fuzzi, S
    Facchini, MC
    Mircea, M
    Emblico, L
    Cavalli, F
    Maenhaut, W
    Chi, X
    Schkolnik, G
    Falkovich, A
    Rudich, Y
    Claeys, M
    Pashynska, V
    Vas, G
    Kourtchev, I
    Vermeylen, R
    Hoffer, A
    Andreae, MO
    Tagliavini, E
    Moretti, F
    Artaxo, P
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 : 375 - 402
  • [7] Water soluble organic compounds formed by oxidation of soot
    Decesari, S
    Facchini, MC
    Matta, E
    Mircea, M
    Fuzzi, S
    Chughtai, AR
    Smith, DM
    [J]. ATMOSPHERIC ENVIRONMENT, 2002, 36 (11) : 1827 - 1832
  • [8] Hygroscopic growth of atmospheric and model humic-like substances
    Dinar, E.
    Taraniuk, I.
    Graber, E. R.
    Anttila, T.
    Mentel, T. F.
    Rudich, Y.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2007, 112 (D5)
  • [9] Cloud Condensation Nuclei properties of model and atmospheric HULIS
    Dinar, E.
    Taraniuk, I.
    Graber, E. R.
    Katsman, S.
    Moise, T.
    Anttila, T.
    Mentel, T. F.
    Rudich, Y.
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 : 2465 - 2481
  • [10] Surface tension of atmospheric wet aerosol and cloud/fog droplets in relation to their organic carbon content and chemical composition
    Facchini, MC
    Decesari, S
    Mircea, M
    Fuzzi, S
    Loglio, G
    [J]. ATMOSPHERIC ENVIRONMENT, 2000, 34 (28) : 4853 - 4857