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Four years of active sampling and measurement of atmospheric polycyclic aromatic hydrocarbons and oxygenated polycyclic aromatic hydrocarbons in Dronning Maud Land, East Antarctica
Van Overmeiren, P.; Demeestere, K.; De Wispelaere, P.; Gili, S.; Mangold, A.; De Causmaecker, K.; Mattielli, N.; Delcloo, A.; Van Langenhove, H.; Walgraeve, C. (2024). Four years of active sampling and measurement of atmospheric polycyclic aromatic hydrocarbons and oxygenated polycyclic aromatic hydrocarbons in Dronning Maud Land, East Antarctica. Environ. Sci. Technol. 58(3): 1577-1588. https://dx.doi.org/10.1021/acs.est.3c06425
In: Environmental Science and Technology. American Chemical Society: Easton. ISSN 0013-936X; e-ISSN 1520-5851, meer
Peer reviewed article  

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Trefwoord
    Marien/Kust
Author keywords
    polycyclic aromatic hydrocarbons; long-range atmospheric transport; oxygenated PAHs; gas-particle partitioning; Antarctica; volcanic sources

Auteurs  Top 
  • Van Overmeiren, P., meer
  • Demeestere, K., meer
  • De Wispelaere, P., meer
  • Gili, S.
  • Mangold, A., meer
  • De Causmaecker, K., meer
  • Mattielli, N., meer
  • Delcloo, A., meer
  • Van Langenhove, H., meer
  • Walgraeve, C., meer

Abstract
    Antarctica, protected by its strong polar vortex and sheer distance from anthropogenic activity, was always thought of as pristine. However, as more data on the occurrence of persistent organic pollutants on Antarctica emerge, the question arises of how fast the long-range atmospheric transport takes place. Therefore, polycyclic aromatic hydrocarbons (PAHs) and oxygenated (oxy-)PAHs were sampled from the atmosphere and measured during 4 austral summers from 2017 to 2021 at the Princess Elisabeth station in East Antarctica. The location is suited for this research as it is isolated from other stations and activities, and the local pollution of the station itself is limited. A high-volume sampler was used to collect the gas and particle phase (PM10) separately. Fifteen PAHs and 12 oxy-PAHs were quantified, and concentrations ranging between 6.34 and 131 pg m(3) (Sigma(15)PAHs-excluding naphthalene) and between 18.8 and 114 pg m(3) (Sigma(13)oxy-PAHs) were found. Phenanthrene, pyrene, and fluoranthene were the most abundant PAHs. The gas-particle partitioning coefficient log(K-p) was determined for 6 compounds and was found to lie between 0.5 and -2.5. Positive matrix factorization modeling was applied to the data set to determine the contribution of different sources to the observed concentrations. A 6-factor model proved a good fit to the data set and showed strong variations in the contribution of different air masses. During the sampling campaign, a number of volcanic eruptions occurred in the southern hemisphere from which the emission plume was detected. The FLEXPART dispersion model was used to confirm that the recorded signal is indeed influenced by volcanic eruptions. The data was used to derive a transport time of between 11 and 33 days from release to arrival at the measurement site on Antarctica.

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