Sources of optically active aerosol particles over the Amazon forest

被引:41
|
作者
Guyon, P
Graham, B
Roberts, GC
Mayol-Bracero, OL
Maenhaut, W
Artaxo, P
Andreae, MO
机构
[1] Max Planck Inst Chem, Dept Biogeochem, D-55020 Mainz, Germany
[2] CSIRO Atmospher Res, Melbourne, Vic 3195, Australia
[3] Univ Puerto Rico, Inst Trop Ecosyst Studies, Rio Piedras, PR 00931 USA
[4] Scripps Inst Oceanog, Ctr Atmospher Res, San Diego, CA USA
[5] State Univ Ghent, Inst Nucl Sci, B-9000 Ghent, Belgium
[6] Univ Sao Paulo, Inst Phys, BR-05315970 Sao Paulo, Brazil
基金
巴西圣保罗研究基金会;
关键词
natural background aerosols; biomass burning; black carbon; aerosol scattering; aerosol absorption; Amazonia;
D O I
10.1016/j.atmosenv.2003.10.051
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Size-fractionated ambient aerosol samples were collected at a pasture site and a primary rainforest site in the Brazilian Amazon Basin during two field campaigns (April-May and September-October 1999), as part of the European contribution to the Large-Scale Biosphere-Atmosphere Experiment in Amazonia (LBA-EUSTACH). The samples were analyzed for up to 19 trace elements by particle-induced X-ray emission analysis (PIXE), for equivalent black carbon (BCe) by a light reflectance technique and for mass concentration by gravimetric analysis. Additionally, we made continuous measurements of absorption and light scattering by aerosol particles. The vertical chemical composition gradients at the forest site have been discussed in a companion article (Journal of Geophysical Research-Atmospheres 108 (1318), 4591 (doi:4510.1029/2003JD003465)). In this article, we present the results of a source identification and quantitative apportionment study of the wet and dry season aerosols, including an apportionment of the measured scattering and absorption properties of the total aerosol in terms of the identified aerosol sources. Source apportionments (obtained from absolute principal component analysis) revealed that the wet and dry season aerosols contained the same three main components, but in different (absolute and relative) amounts: the wet season aerosol consisted mainly of a natural biogenic component, whereas pyrogenic aerosols dominated the dry season aerosol mass. The third component identified was soil dust, which was often internally mixed with the biomass-burning aerosol. All three components contributed significantly to light extinction during both seasons. At the pasture site, up to 47% of the light absorption was attributed to biogenic particles during the wet season, and up to 35% at the tower site during the wet-to-dry transition period. The results from the present study suggest that, in addition to pyrogenic particles, biogenic and soil dust aerosols must be taken into account when modeling the physical and optical properties of aerosols in forested regions such the Amazon Basin. (C) 2003 Published by Elsevier Ltd.
引用
收藏
页码:1039 / 1051
页数:13
相关论文
共 50 条
  • [1] In-canopy gradients, composition, sources, and optical properties of aerosol over the Amazon forest
    Guyon, P
    Graham, B
    Roberts, GC
    Mayol-Bracero, OL
    Maenhaut, W
    Artaxo, P
    Andreae, MO
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D18)
  • [2] Refractive index of aerosol particles over the Amazon tropical forest during LBA-EUSTACH 1999
    Guyon, P
    Boucher, O
    Graham, B
    Beck, J
    Mayol-Bracero, OL
    Roberts, GC
    Maenhaut, W
    Artaxo, P
    Andreae, MO
    [J]. JOURNAL OF AEROSOL SCIENCE, 2003, 34 (07) : 883 - 907
  • [3] Refractive index of aerosol particles over the Amazon tropical forest during LBA-EUSTACH 1999
    [J]. Guyon, P. (guyon@mpch-mainz.mpg.de), 1600, Elsevier Ltd (34):
  • [4] Physical properties and concentration of aerosol particles over the Amazon tropical forest during background and biomass burning conditions
    Guyon, P
    Graham, B
    Beck, J
    Boucher, O
    Gerasopoulos, E
    Mayol-Bracero, OL
    Roberts, GC
    Artaxo, P
    Andreae, MO
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2003, 3 : 951 - 967
  • [5] Aerosol number fluxes over the Amazon rain forest during the wet season
    Ahlm, L.
    Nilsson, E. D.
    Krejci, R.
    Martensson, E. M.
    Vogt, M.
    Artaxo, P.
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (24) : 9381 - 9400
  • [6] Sources of carbonaceous aerosol in the Amazon basin
    Gilardoni, S.
    Vignati, E.
    Marmer, E.
    Cavalli, F.
    Belis, C.
    Gianelle, V.
    Loureiro, A.
    Artaxo, P.
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2011, 11 (06) : 2747 - 2764
  • [7] A comparison of dry and wet season aerosol number fluxes over the Amazon rain forest
    Ahlm, L.
    Nilsson, E. D.
    Krejci, R.
    Martensson, E. M.
    Vogt, M.
    Artaxo, P.
    [J]. ATMOSPHERIC CHEMISTRY AND PHYSICS, 2010, 10 (06) : 3063 - 3079
  • [8] THE SOURCES OF SULFATE, VANADIUM AND MINERAL MATTER IN AEROSOL-PARTICLES OVER BERMUDA
    CHEN, LQ
    DUCE, RA
    [J]. ATMOSPHERIC ENVIRONMENT, 1983, 17 (10) : 2055 - 2064
  • [9] Chemical composition of aerosol collected in the Amazon Forest.
    Vasconcellos, PD
    Artaxo, PE
    Ciccioli, P
    Cecinato, A
    Brancaleoni, E
    Frattoni, M
    [J]. QUIMICA NOVA, 1998, 21 (04): : 385 - 393
  • [10] THE CHEMISTRY OF ATMOSPHERIC AEROSOL-PARTICLES IN THE AMAZON BASIN
    ARTAXO, P
    GERAB, F
    YAMASOE, MA
    MARTINS, JV
    [J]. CHEMISTRY OF THE AMAZON: BIODIVERSITY, NATURAL PRODUCTS, AND ENVIRONMENTAL ISSUES, 1995, 588 : 265 - 280