6533b833fe1ef96bd129b9b8
RESEARCH PRODUCT
The sea–air exchange of mercury (Hg) in the marine boundary layer of the Augusta basin (southern Italy): Concentrations and evasion flux
M. SproveriElvira OliveriFrancesco ParelloV. Di StefanoMarco BarraSergio CalabreseEmanuela Rita BagnatoMarcello BitettoS. MazzolaMaria Bonsignoresubject
Mediterranean climatePollutionBiogeochemical cycleEnvironmental EngineeringMercury evasion flux Atmospheric mercury concentrations Gaseous elemental mercury Sea–air evasion Marine boundary layer Augusta basinHealth Toxicology and Mutagenesismedia_common.quotation_subjectchemistry.chemical_elementStructural basinFlux (metallurgy)Sea airEnvironmental ChemistrySeawatermedia_commonAir PollutantsAtmospherePublic Health Environmental and Occupational HealthMercuryGeneral MedicineGeneral ChemistryPollutionMercury (element)OceanographyItalychemistryEnvironmental scienceSeasonsBayWater Pollutants ChemicalEnvironmental Monitoringdescription
Abstract The first attempt to systematically investigate the atmospheric mercury (Hg) in the MBL of the Augusta basin (SE Sicily, Italy) has been undertaken. In the past the basin was the receptor for Hg from an intense industrial activity which contaminated the bottom sediments of the Bay, making this area a potential source of pollution for the surrounding Mediterranean. Three oceanographic cruises have been thus performed in the basin during the winter and summer 2011/2012, where we estimated averaged Hg atm concentrations of about 1.5 ± 0.4 (range 0.9–3.1) and 2.1 ± 0.98 (range 1.1–3.1) ng m −3 for the two seasons, respectively. These data are somewhat higher than the background Hg atm value measured over the land (range 1.1 ± 0.3 ng m −3 ) at downtown Augusta, while are similar to those detected in other polluted regions elsewhere. Hg evasion fluxes estimated at the sea/air interface over the Bay range from 3.6 ± 0.3 (unpolluted site) to 72 ± 0.1 (polluted site of the basin) ng m −2 h −1 . By extending these measurements to the entire area of the Augusta basin (∼23.5 km 2 ), we calculated a total sea–air Hg evasion flux of about 9.7 ± 0.1 g d −1 (∼0.004 t yr −1 ), accounting for ∼0.0002% of the global Hg oceanic evasion (2000 t yr −1 ). The new proposed data set offers a unique and original study on the potential outflow of Hg from the sea–air interface at the basin, and it represents an important step for a better comprehension of the processes occurring in the marine biogeochemical cycle of this element.
year | journal | country | edition | language |
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2013-11-01 | Chemosphere |