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An important factor in the release of phosphorus by soil erosion, withcorresponding consequences on the quality of surface waters, is theformation of aggregates and their stability. Around the eutrophic LakeHallwil six arable lands were examined in five repetitions regardingaggregate and particle size distribution, P-contents of the differentfractions and aggregate stability. Central to this was the use of thesetting column for fractionation of soil samples. In the case of LakeHallwil the risk of phosphorus discharges by soil erosion seems low sincethe phosphorus is mainly bound in aggregates which are transported overshort distances only. Thus other pathways (runoff from grassland, leachingvia drains) may be more important

Risiko des Eintrags von Phosphor in den Hallwilersee durch Bodenerosion