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

被引:31
作者
Baker, A. R. [1 ]
Thomas, M. [1 ]
Bange, H. W. [2 ]
Plasencia Sanchez, E. [3 ]
机构
[1] Univ E Anglia, Sch Environm Sci, Ctr Ocean & Atmospher Sci, Norwich NR4 7TJ, Norfolk, England
[2] GEOMAR Helmholtz Zentrum Ozeanforsch Kiel, Marine Biogeochem, Dusternbrooker Weg 20, D-24105 Kiel, Germany
[3] Univ Nacl Ingn, Fac Ingn Geol Minera & Met, SENAMHI, Peru Direcc Gen Invest & Asuntos Ambientales,Serv, Lima, Peru
基金
英国自然环境研究理事会;
关键词
UPWELLING REGIME; ATLANTIC-OCEAN; VOCALS-REX; IRON; DEPOSITION; PHYTOPLANKTON; ATMOSPHERE; SOLUBILITY; CHILE; AIR;
D O I
10.5194/bg-13-817-2016
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
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 NO3- and NH4+) 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 similar to 13 degrees 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 (similar to 15-16 degrees S), elevated concentrations of Fe, Cu, Co, and Ni were observed, and we calculated dry deposition fluxes of soluble Cu approximately an order of magnitude higher than a recent model-based estimate of total Cu deposition to the region. The model did not take account of emissions from the large smelting facilities in the south of Peru and northern Chile, and our results may indicate that these facilities constitute an important source of trace metals to the region. Calculated dry deposition fluxes (3370-17800 and 16-107 nmol m(-2) d(-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.
引用
收藏
页码:817 / 825
页数:9
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