to quantify variations in splash mass flux, splash SOC (soil organic carbon) concentration and splash SOC flux on an individual aggregate size basis and to examine their relationship with EFD and AMC. These data will be used to determine whether splash
Laboratory rainfall simulation experiments were conducted on a clay-rich kaolinitic oxisol from Hawai'i. The objectives of this study were: 1) to quantify wet-sieved aggregate ER-values for splash and wash transported sediment from a tropical oxisol
; 2) to assess temporal variations in aggregate ER-values for splash and wash under controlled rainfall conditions; 3) to determine the influence of slope angle on splash and wash ER-values.
Couverture végétale ; Erosion des sols ; France ; Infiltration ; Parcelle expérimentale ; Pluie torrentielle ; Propriétés du sol ; Provence-Alpes-Côte d'Azur ; Ruissellement ; Splash ; Topographie ; Transport sédimentaire ; Vaucluse ; Versant
Experiment plot ; France ; Heavy rain ; Infiltration ; Plant cover ; Provence-Alpes-Côte d'Azur ; Rill wash ; Sediment transport ; Slope ; Soil erosion ; Soil properties ; Splash ; Topography ; Vaucluse ; Vinegrowing area
simulation experiments. The infiltration rate is calculated as the difference between rainfall and runoff rates, the flow depths are measured to allow the flow hydraulics to be calculated and thirdly, sediment transport, both by splash and overland flow
Badland ; Drôme ; Erosion des sols ; France ; France du Sud ; Infiltration ; Midi-Pyrénées ; Orage ; Propriétés du sol ; Précipitation ; Rhône-Alpes ; Ruissellement ; Simulation de pluie ; Splash ; Tarn ; Transport sédimentaire ; Versant
Badland ; Drôme ; France ; Infiltration ; Midi-Pyrénées ; Precipitation ; Rainfall simulation ; Rainstorm ; Rhône-Alpes ; Rill wash ; Sediment transport ; Slope ; Soil erosion ; Soil properties ; Southern France ; Splash ; Tarn