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Título

Atmospheric dry deposition of persistent organic pollutants to the Atlantic and inferences for the global oceans

AutorJurado, Elena; Jaward, Foday M.; Lohmann, Rainer; Jones, Kevin C.; Simó, Rafel ; Dachs, Jordi
Fecha de publicación29-sep-2004
EditorAmerican Chemical Society
CitaciónEnvironmental Science and Technology 38(21): 5505-5513 (2004)
ResumenAtmospheric deposition to the oceans is a key process affecting the global dynamics and sinks of persistent organic pollutants (POPs). A new methodology that combines aerosol remote sensing measurements with measured POP aerosol-phase concentrations is presented to derive dry particulate depositional fluxes of POPs to the oceans. These fluxes are compared with those due to diffusive air−water exchange. For all polychlorinated biphenyl (PCB) congeners and lower chlorinated dibenzo-p-dioxins and furans (PCDD/Fs), air−water exchange dominates the dry deposition mechanism. However, this tendency reverses in some areas, such as in marine aerosol influenced areas and dust outflow regions, consistent with the important variability encountered for the depositional fluxes. Seasonal variability is mainly found in mid-high latitudes, due to the important influence of wind speed enhancing dry deposition fluxes and temperature as a driver of the gas-particle partitioning of POPs. The average dry aerosol deposition flux of ΣPCBs and ΣPCDD/Fs to the Atlantic Ocean is calculated to be in the order of 66 ng m-2 yr-1 and 9 ng m-2 yr-1 respectively. The total dry aerosol deposition of ∑PCBs and ∑PCDD/Fs to the Atlantic Ocean is estimated to be 2200 kg yr-1 and 500 kg yr-1, respectively, while the net air−water exchange is higher, 22000 kg ∑PCBs yr-1 for PCBs and 1300 kg ∑PCDD/Fs yr-1. Furthermore, it is suggested that marine aerosol plays an important role in scavenging atmospheric contaminants.
Descripción9 pages, 6 figures, 1 table.-- PMID: 15575265 [PubMed].-- Printed version published Nov 1, 2004.
Supporting information available: Further details on cruise data and methodology to estimate dry deposition velocities (Annexes I, II, and III) and comparison of gross gaseous absorption and dry aerosol deposition fluxes (Annex IV).-- Available at: http://pubs.acs.org/doi/suppl/10.1021/es049240v
Versión del editorhttp://dx.doi.org/10.1021/es049240v
URIhttp://hdl.handle.net/10261/15353
DOI10.1021/es049240v
ISSN0013-936X
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