Per citar aquest document: http://ddd.uab.cat/record/131569
Variation of soluble and insoluble calcium in red rains related to dust sources and transport patterns from North Africa to northeastern Spain
Àvila i Castells, Anna (Centre de Recerca Ecològica i Aplicacions Forestals)
Alarcón Jordán, Marta, 1958- (Universitat Politècnica de Catalunya. Departament de Física i Enginyeria Nuclear)
Castillo, S. (Institut de Ciències de la Terra Jaume Almera)
Escudero, M. (Centre de Recerca Ecològica i Aplicacions Forestals)
Garcia i Orellana, Jordi (Universitat Autònoma de Barcelona. Institut de Ciència i Tecnologia Ambientals)
Masqué Barri, Pere (Universitat Autònoma de Barcelona.. Institut de Ciència i Tecnologia Ambientals)
Querol Carceller, Xavier (Institut de Ciències de la Terra Jaume Almera)

Data: 2007
Resum: We use the chemical composition of African dust delivered by red rains at a rural site in northeastern Spain (Montseny, 41460 N, 2210 E) to describe its relationship with the possible provenance areas and the processes occurring during transport. To this end, we obtained the red rain insoluble composition for the major elements (Al, Fe, Ca, Mg, K, P, Ti, and Na) in 30 filters, the 210Pb concentration in 23 filters, and the soluble cation concentrations (Na, K, Ca, and Mg) in 28 coincident red rain samples. These samples comprised most major events occurring at the site from 1983 to 2002. On the basis of back trajectories and satellite images, a distinction has been made between an eastern and western air mass flux with respect to 0 Greenwich for the analyzed samples. Principal component and ANOVA analyses between the two provenance groups have shown striking differences in the insoluble phase, with eastern samples being significantly richer in insoluble Ca, Mg, and Sr compared to western samples. Conversely, western samples had significantly higher concentrations of insoluble Al, Fe, K, V, and 210Pb than eastern samples. Therefore, in the insoluble phase, the ratios of various elements to Ca were significantly higher in western provenances. However, these differences disappeared when considering bulk Ca ratios (bulk Ca = insoluble + soluble Ca). Neither of the ratios Fe/Al and Ti/Fe showed significant differences. This lack of differences is interpreted in view of a similar carbonated lithology broadly underlying both areas. The difference in insoluble Ca with respect to total Ca between provenances (Cainsoluble/Catotal = 0. 10 and 0. 70 for western and eastern trajectories, respectively) is interpreted as a difference in calcite dissolution during transport. Evidence from 210Pb data and from the length of the back trajectories indicates that western trajectories covered a longer distance than the eastern ones; their higher soluble Ca could be due to (1) higher calcite dissolution due to longer contact with wet fronts from the Atlantic and (2) particle segregation during transport, with finer (carbonate) particles more prone to dissolution due to a higher surface to volume ratio.
Nota: Número d'acord de subvenció MCYT/REN2001-0659/CLI
Nota: Número d'acord de subvenció MEC/CGL2004-05984/CLI
Nota: Número d'acord de subvenció MEC/CGL2005-07543/CLI
Drets: Tots els drets reservats
Llengua: Anglès
Document: article ; recerca ; publishedVersion
Matèria: Calcium ; Red rain ; Spain ; North Africa
Publicat a: Journal of geophysical research : atmospheres, Vol. 112, Issue D5 (March 2007) , p D05210, ISSN 2169-897X

DOI: 10.1029/2006JD007153


14 p, 580.6 KB

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Documents de recerca > Documents dels grups de recerca de la UAB > Centres i grups de recerca (producció científica) > Ciències > CREAF (Centre de Recerca Ecològica i d'Aplicacions Forestals)
Documents de recerca > Documents dels grups de recerca de la UAB > Centres i grups de recerca (producció científica) > Ciències > Institut de Ciència i Tecnologia Ambientals (ICTA)
Articles > Articles de recerca
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 Registre creat el 2015-04-14, darrera modificació el 2016-06-04



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