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Par Collection Par Auteur- DEFORCE, K. (1)
- HAGEDORN, J., (Editeur scientifique) (1)
- MALLANTS, D. (1)
- BEERTEN, K. (1)
- PÖRTGE, K.-H. (1)
- Agua del suelo ; Análisis polínico ; Arena ; Bélgica ; Datación Carbono 14 ; Geocronología ; Granulometría ; Kempen ; Pedogénesis ; Podzolización ; Propiedades del suelo (1)
- Allemagne ; Bassin-versant ; Bilan sédimentaire ; Charge en solution ; Charge solide ; Erosion des sols ; Géomorphométrie ; Hydrologie ; Niedersachsen ; Ruissellement ; Variation spatiale (1)
- Analyse pollinique ; Belgique ; Datation C 14 ; Eau du sol ; Granulométrie ; Géochronologie ; Kempenland ; Luminescence stimulée optiquement ; Podzolisation ; Propriétés du sol ; Pédogenèse ; Pédohydrologie ; Sable (1)
- Belgium ; C 14 dating ; Geochronology ; Grain size distribution ; Kempenland ; Optically stimulated luminescence ; Pedogenesis ; Pedohydrology ; Podsolisation ; Pollen analysis ; Sand ; Soil properties ; Soil water (1)
- Geomorphometry ; Germany ; Hydrology ; Niedersachsen ; Rill wash ; Sediment budget ; Sediment load ; Soil erosion ; Solution load ; Spatial variation ; Watershed (1)
- Landscape evolution and changes in soil hydraulic properties at the decadal, centennial and millennial scale: A case study from the Campine area, northern Belgium (1)
- Late Quaternary and present-day fluvial processes in Central Europe (1)
- Temporal and spatial variation in dissolved and solid load years in partial catchment areas of the upper Leine river (southern Lower Saxony) (1)
- Belgium ; C 14 dating ; Geochronology ; Grain size distribution ; Kempenland ; Optically stimulated luminescence ; Pedogenesis ; Pedohydrology ; Podsolisation ; Pollen analysis ; Sand ; Soil properties ; Soil water
- in which different sandy landscapes and associated soils are preserved was studied with respect to its geomorphological and pedohydrological characteristics. Three stages of soil development corresponding to specific landscapes were observed within a 2-m
- landscape evolution, soil development and hydraulic properties. It is concluded that combination of geomorphological and pedohydrological analyses of sediment-soil archives may provide a unique means to gain insight into the rate and extent of past changes
- patterns as has the respective pedohydrological situation as a time-variant qantity.