R.W. de Waal
- Soil and humus development in drift sands
- Book title
- Inland drift sand landscapes
- Number of pages
- Zeist: KNNV Publishing
- Document type
- Faculty of Science (FNWI)
- Institute for Biodiversity and Ecosystem Dynamics (IBED)
In drift sand, incipient mineral soils with a very thin endorganic horizon develop towards highly acid soils with a thick, differentiated, mor to moder type ectorganic horizon and incipient podzolisation, within a period of about 100 years. This is due slow litter decomposition and associated soil acidification, brought about by the adverse site conditions. Initially being dependent on atmospheric inputs, soil stocks of macrometals (Fe, Al, Ca, Mg, K, Na) strongly increase during succession, largely through efficient biogeochemical cycling. Differences in site conditions and management within drift sand areas lead to differences in rates of soil and humus form development, being clearly visible in the humus form.
If you believe that digital publication of certain material infringes any of your rights or (privacy) interests, please let the Library know, stating your reasons. In case of a legitimate complaint, the Library will make the material inaccessible and/or remove it from the website. Please Ask the Library, or send a letter to: Library of the University of Amsterdam, Secretariat, Singel 425, 1012 WP Amsterdam, The Netherlands. You will be contacted as soon as possible.