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PORTAIL D'INFORMATION GÉOGRAPHIQUE

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  • was used. Soil texture and aggregate stability were more important than overland flow in modifying the temporal PSD. Transport capacity appears to be diminished due to soil cover, making all predictions based on settling velocity ineffective. High kinetic
  • particles release was continuous and independent of soil texture. It is highlighted that : Temporal iron enrichment of clay/silt-sized particles depends on water submergence; Iron extreme values depend on new sources of iron inside soil aggregates; Soil