Source terms and source strengths of the carbonaceous aerosol in the tropics

Journal of Atmospheric Chemistry - Tập 3 - Trang 469-489 - 1985
Hélène Cachier1, Patrick Buat-Menard1, Michel Fontugne1, Jacques Rancher2
1Laboratoire mixte CNRS-CEA, Centre des Faibles Radioactivités, Gif-sur-Yvette, France
2CEA, Paris Cédex 15, France

Tóm tắt

Atmospheric aerosol samples were collected in the Ivory Coast, primarily at Lamto (6°N, 5°W) between 1979 and 1981. The samples were analysed for total particulate carbon concentration and isotopic composition (13C/12C) by mass spectrometry. Observed concentrations were found high compared to values reported for temperate regions. Fine particulate carbon in the submicrometersize range accounted for 50 to 80% of the reported concentrations. At Lamto, both particulate carbon concentrations and isotopic ratios exhibit a large temporal variability which is shown to reflect the diversity of sources and their seasonal evolution. Natural emissions from the equatorial forest during the wet season, and biomass burning during the dry season, appear to be the major sources. The latter, though active during only a third of the year, is, on an annual basis, the most important source. Based on the data obtained at Lamto, an attempt has been made to estimate the flux of fine particulate carbon emitted from the tropical regions into the global troposphere. This flux, which is of the order of 20×1012 g C/yr, appears to be equivalent to the flux of fine particulate carbon emitted from industrial sources. These results suggest that the tropospheric burden of fine particulate carbon in lowlatitude regions is dominated by the long-range transport of carbonaceous aerosols originating from the Tropics.

Tài liệu tham khảo

Bertrand J., 1976, Visibilité et brume sèche en Afrique, La Metéorologie 6, 201–211.

Court, J. D., Goldsack, R. J., Ferrari, L. M., and Polach, H. A., The use of carbon isotopes in identifying urban air particulate sources, Clean Air, Feb 1981, 6–11.

Cros, B., 1977, Contribution à l'étude des noyaux d'aitken en Afrique équatoriale française, PhD Thesis, Université de Toulouse.

Delmas, R., 1980, Contribution à l'étude des fôrèts équatoriales comme sources naturelles de dérivés soufrés atmosphériques, PhD Thesis, Université de Toulouse.

Domergue, J. L., 1972, Identification et variation des concentrations de quelques éléments constitutifs des aérosols atmosphériques en zone intertropicale, Thèse de spécialité, Toulouse.

Fontugne, M., 1983, Les isotopes stables du carbone organique dans l'océan; application à la paléo-climatologie, PhD Thesis, Université Paris 11.

Fritz P., and Fontes J. C., 1980, Handbook of Environmental Isotope Geochemistry 1, Elsevier, Amsterdam.

Hahn, J., 1980, Organic constituents of natural aerosols, Ann. N.Y. Acad. Sci., 359–376.

Lambert G. Polian G. Sanak J., Ardouin B., Buisson A., Jegou A., Le Roulley J. C., 1982, Cycle du radon et de ses descendants: application à l'étude des échanges troposphère-stratosphère, Ann. Geophys. 4, 497–531.

Lamotte, M., 1983, Structure et fonctionnement d'un écosystème de savane ivoirienne, Courrier du CNRS supp. 52, Paris, 71–79.

Marty J. C., and Saliot A., 1982, Aerosols in equatorial Atlantic air: n-alkanes concentrations and distributions as a function of particle size, Nature 298, 144–147.

Rahn K. A., and McCaffrey R. J., 1980, On the origin and transport of the winter Arctic aerosol, Ann. N.Y. Acad. Sci. 338, 486–503.

Went F. W., 1960, Organic matter in the atmosphere and its possible relation to petroleum formation, Proc. Natl. Acad. Sci. U.S.A. 46, 212–221.