Soluble trace metals in aerosols over the tropical south east Pacific offshore of Peru

Descripción del Articulo

Bulk aerosol samples collected during cruise M91 of FS Meteor off the coast of Peru in December 2012 were analysed for their soluble trace metal (Fe, Al, Mn, Ti, Zn, V, Ni, Cu, Co, Cd, Pb, Th) and major ion (including NO−3 and NH+4) content. These data are among the first recorded for trace metals i...

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Detalles Bibliográficos
Autores: Baker, A.R., Thomas, M., Bange, H.W., Plasencia Sanchez, E.
Formato: objeto de conferencia
Fecha de Publicación:2015
Institución:Servicio Nacional de Meteorología e Hidrología del Perú
Repositorio:SENAMHI-Institucional
Lenguaje:español
OAI Identifier:oai:repositorio.senamhi.gob.pe:20.500.12542/992
Enlace del recurso:https://hdl.handle.net/20.500.12542/992
https://doi:10.5194/bgd-12-17219-2015
Nivel de acceso:acceso abierto
Materia:Contaminantes Atmosféricos
Elementos Químicos
Aerosol Atmosférico
Metales Pesados
https://purl.org/pe-repo/ocde/ford#1.05.08
https://purl.org/pe-repo/ocde/ford#1.05.09
contaminacion del aire - Aire y Atmósfera
Descripción
Sumario:Bulk aerosol samples collected during cruise M91 of FS Meteor off the coast of Peru in December 2012 were analysed for their soluble trace metal (Fe, Al, Mn, Ti, Zn, V, Ni, Cu, Co, Cd, Pb, Th) and major ion (including NO−3 and NH+4) content. These data are among the first recorded for trace metals in this relatively poorly studied region of the global marine atmosphere. To the north of ∼ 13◦ S, the concentrations of several elements (Fe, Ti, Zn, V, Ni, Pb) appear to be related to distance from the coast. At the south of the transect (∼ 15–16◦ S), elevated concentrations of Fe, Cu, Co and Ni were observed. These may be related to the activities of the large smelting facilities in the south of Peru or northern Chile. Calculated dry deposition fluxes (3370–17 800 and 16–107 nmolm−2d−1 for inorganic nitrogen and soluble Fe respectively) indicated that atmospheric input to the waters of the Peru upwelling system contains an excess of Fe over N, with respect to phytoplankton requirements. This may be significant as primary production in these waters has been reported to be limited by Fe availability, but atmospheric deposition is unlikely to be the dominant source of Fe to the system.
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