|
Biodiversity
Landscape Development
Management of Natural Hazards
Natural Resources
Forest Ecosystems
Research Units
Research Programmes
In focus
Staff
Organization
Mission and Tasks
History
Job opportunities
Contact and maps
Heavy metals in Swiss forest soils
The aim of this project is to obtain an overview of contents, effective mobility and potential ecotoxicity of heavy metals in Swiss forest soils. Collaboration and FrameworkIn this project, the WSL research unit “Soil Sciences” collaborates with the Group of “Solid Materials Analytics” at “EMPA Materials Science and Technology” (Peter Lienemann, Christoph Zwicky), the "Dept. of Applied Environmental Science" of the Stockholm University (Markus Meili), and Alterra, Wageningen (Bert-Jan Groenenberg). The investigations on mercury and lead are carried out in the framework of the UN-ECE "Convention on Long-range Transboundary Air Pollution" (LRTAP). The metal specific background can be found in chapter 5.5. of the current "Mapping Manual". Mobility of Chromium, Nickel, Copper, Zinc and LeadHeavy metal contents at various soil depths were determined for soils at 96 forest sites in Switzerland. The physical and chemical properties of these soils are described in great detail in the three volumes “Waldböden der Schweiz”. The calculation of enrichment factors relative to Zirconium allowed to estimate relative mobilities of the metals and to detect atmospheric input. Potential ecotoxicity was estimated by comparison with the guide levels set by the Swiss Ordinance Relating to Impacts on the Soil (VBBo) and with lowest observation effect concentrations for effects on microorganisms in topsoils recommended by the UN-ECE.
(Lit.: Luster et al. 2006b, c) Mobility of MercuryCurrently, the relative mobility of mercury is determined in a representative subset of the soils. These investigations complement the determination of critical mercury limits for effects on soil organisms. Transferfunctions for Cadmium, Copper, Nickel, Lead and ZincThe relations between water soluble and reactive metal pools were expressed as so-called transferfunctions. The data on a representative set of Swiss forest soils from all regions served to validate transferfunctions derived from Dutch and UK data sets. In particular, the Swiss data set included carbonate containing soils not available in the latter data sets. Publications
|