Background aerosol composition in the namib desert,South West Africa (Namibia) |
| |
| Affiliation: | 1. Department of Physics, University of Girona, Girona, Spain;2. Instituto Pirenaico de Ecología, Consejo Superior de Investigaciones Científicas (IPE–CSIC), Zaragoza, Spain;3. Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA;4. Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA;1. Instituto Superior de Tecnologías y Ciencias Aplicadas, Ave. Salvador Allende y Luaces, La Habana 10600, Cuba;2. Universidad “Camilo Cienfuegos”, Matanzas, Cuba |
| |
| Abstract: | A remote site in the Namib Desert was selected for sampling background aerosols in southern Africa, as one of a wide network of stations spanning the Southern Hemisphere in a programme designed to measure the background concentrations of trace elements in the atmosphere. A series of samples was collected over a 6-month period using a single-orifice cascade impactor, which fractionated the particles into six size groups. Analysis was performed using particle-induced X-ray emission (PIXE), yielding results for S, Cl, K, Ca, Ti, Mn, Fe, Br and Sr, and occasionally also for V, Cr, Ni, Cu, Zn and Pb. No direct correlations with wind direction were observed excluding strong local or regional sources of particles. K, Ca, Ti, Mn and Fe can be identified with a dust dispersion source. Cl, large particle S and Br, and part of the K and Sr are derived from sea spray. Relative to the soil components small particle K is not enriched as it normally is in regions with less scarce vegetation. Cr, V, Ni, Cu, Zn and Pb concentrations and enrichments in the aerosol are lower than practically all values measured at any other location hitherto. The concentration of the small particle sulphur, 200 ng m−3, is believed to be related to anaerobic conditions and plankton blooms in the ocean upwelling zones off Namibia. |
| |
| Keywords: | |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
