Zobrazeno 1 - 10
of 27
pro vyhledávání: '"podzolgronden"'
Publikováno v:
Scopus-Elsevier
Geologie & Mijnbouw, 92(2/3), 243-266. Stichting Netherlands Journal of Geosciences
Netherlands journal of geosciences, 92(4), 243-266
Netherlands journal of geosciences 92 (2013) 4
Geologie & Mijnbouw, 92(2/3), 243-266. Stichting Netherlands Journal of Geosciences
Netherlands journal of geosciences, 92(4), 243-266
Netherlands journal of geosciences 92 (2013) 4
A unique complex of multiphased Holocene drift sands and paleosols, with at least two lacustrine phases, was discovered during a major sanitation project in the Laarder Wasmeren area near Hilversum, the Netherlands. The complex could be studied in de
Publikováno v:
Ecosystems, 5, 11-22
Ecosystems 5 (2002)
Ecosystems 5 (2002)
Tunnels in feldspar grains, assumed to be created by fungal hyphae, were first discovered in a boreal podzol. In this paper, we further describe the phenomenon of mineral tunneling by determining the rate of feldspar tunneling across a north Sweden p
Publikováno v:
Geoderma 94 (2000)
Geoderma, 94, 125-148
Geoderma, 94, 125-148
The chemistry, mineralogy and micromorphology of three soil profiles formed on genetically different Quaternary deposits have been studied in relation to the podzolization process. The soil materials showed quite uniform geochemical composition both
Autor:
Erik Karltun, Lars Nyberg, N. van Breemen, A. Nordgren, L. Tau Strand, Hannu Mannerkoski, O. Wahlberg, Roger D. Finlay, Gunnhild Riise, Tommy Magnusson, A.G. Jongmans, Kevin Bishop, Ulla S. Lundström, Jon Petter Gustafsson, Reiner Giesler, Hannu Ilvesniemi, P.A.W. van Hees, A. Bergelin, Mats Olsson, Mike Starr, P.-A. Melkerud, D. C. Bain
Publikováno v:
Geoderma 94 (2000)
Geoderma, 94, 335-353
Geoderma, 94, 335-353
Advances in understanding the podzolisation process resulting from a multidisciplinary study at three coniferous forest soils in the Nordic countries
Publikováno v:
Geoderma, 94, 91-107
Geoderma 94 (2000)
Geoderma 94 (2000)
This paper reviews the major mechanisms proposed to explain podzolization. These include the production of organic acids that form soluble complexes with aluminium/iron thereby enhancing weathering, followed by illuviation by precipitation/adsorption
Publikováno v:
Biogeochemistry, 49, 53-67
Biogeochemistry 49 (2000)
Biogeochemistry 49 (2000)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0f65e398a86d5e98c3dbd3fa3d9e0058
https://research.wur.nl/en/publications/mycorrhizal-weathering-a-true-case-of-mineral-plant-nutrition
https://research.wur.nl/en/publications/mycorrhizal-weathering-a-true-case-of-mineral-plant-nutrition
Autor:
Nierop, K.G.J., Buurman, P.
Publikováno v:
Humic Substances in the Environment, 1(2), 29-37
Humic Substances in the Environment 1 (1999) 2
Humic Substances in the Environment 1 (1999) 2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::e34c69937c28da3e28d1f69305508117
https://research.wur.nl/en/publications/insoluble-organic-matter-fractions-in-incipient-podzol-b-horizons
https://research.wur.nl/en/publications/insoluble-organic-matter-fractions-in-incipient-podzol-b-horizons
Autor:
Peter Buurman, L. P. Van Reeuwijk
Publikováno v:
Journal of soil science 35 (1984)
Journal of soil science, 35, 447-452
Journal of soil science, 35, 447-452
SUMMARY The presence of imogolite or other poorly crystalline aluminosilicates in the lower B horizons of podzols can be explained by neoformation from silica in the percolating soil solution and aluminium species liberated from their organic bond by