Publication: Rapid transformation of inorganic to organic and plant available phosphorous in soils of a glacier forefield
Rapid transformation of inorganic to organic and plant available phosphorous in soils of a glacier forefield
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Egli, M., Filip, D., Mavris, C., Fischer, B., Götze, J., Raimondi, S., & Seibert, J. (2012). Rapid transformation of inorganic to organic and plant available phosphorous in soils of a glacier forefield. Geoderma, 189–190, 215–226. https://doi.org/10.1016/j.geoderma.2012.06.033
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Abstract
Chemical weathering of rocks or sediments is extremely important for the generation of soils, for the evolution of landscape, and as a main source of inorganic nutrients for plant growth and therefore for life. Temporal trends in weathering mechanisms, plant succession and nutrients availability in cold environments can be successfully studied in soil chronosequences along a glacier forefield. In the present paper, this was carried out in the pro-glacial area of Morteratsch. Different forms of phosphorous in the soil, stream and sprin
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- Egli, Markus
- Filip, Damien
- Mavris, Christian
- Fischer, Benjamin
- Götze, Jens
- Raimondi, Salvatore
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Egli, M., Filip, D., Mavris, C., Fischer, B., Götze, J., Raimondi, S., & Seibert, J. (2012). Rapid transformation of inorganic to organic and plant available phosphorous in soils of a glacier forefield. Geoderma, 189–190, 215–226. https://doi.org/10.1016/j.geoderma.2012.06.033
