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Par Collection Par Auteur- GOVERS, G. (4)
- VERSTRAETEN, G. (4)
- POESEN, J. (3)
- DE VENTE, J. (1)
- DECKERS, S. (1)
- MOEYERSONS, J. (1)
- NYSSEN, J. (1)
- POESEN, J. (1)
- ROMMENS, T. (1)
- VAN OOST, K. (1)
- VAN OOST, K. (1)
- VAN ROMPAEY, A. (1)
- VANDEKERCKHOVE, L. (1)
- VANWALLEGHEM, T. (1)
- HAREGEWEYN, N. (1)
- PEETERS, I. (1)
- VAN DEN EECKHAUT, M. (1)
- VAN ROMPAEY, A.J.J. (1)
- Analyse de régression ; Analyse multivariée ; Ardenne ; Belgique ; Carte thématique ; Dynamique de versant ; Glissement de terrain ; Prévision ; Versant (1)
- Analyse de régression ; Bassin-versant ; Belgique ; Bilan sédimentaire ; Charge en suspension ; Echelle spatiale ; Erosion des sols ; Leuven ; Modèle ; Taux de sédimentation ; Vlaanderen (1)
- Bassin-versant ; Belgique ; Erosion des sols ; Holocène ; Loess ; Modèle ; Modèle numérique de terrain ; Paléogéographie ; Paléogéomorphologie ; Topographie (1)
- Bassin-versant ; Bilan sédimentaire ; Erosion des sols ; Ethiopie ; Gestion de l'eau ; Lac artificiel ; Modèle ; Sédimentation (1)
- Belgium ; Digital elevation model ; Holocene ; Loess ; Model ; Palaeogeography ; Palaeogeomorphology ; Soil erosion ; Topography ; Watershed (1)
- Belgium ; Flanders ; Leuven ; Model ; Regression analysis ; Sediment budget ; Sedimentation rate ; Soil erosion ; Spatial scale ; Suspended load ; Watershed (1)
- Ethiopia ; Model ; Reservoir ; Sediment budget ; Sedimentation ; Soil erosion ; Water management ; Watershed (1)
- Reconstructing ancient topography through erosion modelling
- Bassin-versant ; Belgique ; Erosion des sols ; Holocène ; Loess ; Modèle ; Modèle numérique de terrain ; Paléogéographie ; Paléogéomorphologie ; Topographie
- Belgium ; Digital elevation model ; Holocene ; Loess ; Model ; Palaeogeography ; Palaeogeomorphology ; Soil erosion ; Topography ; Watershed
- The AA. present a topography based hillslope erosion and deposition model that is based on the WATEM/SEDEM model structure and works on a millennial time scale. Soil erosion, transport and deposition are calculated using slope and unit contributing
- area. The topography is iteratively rejuvenated by taking into account modelled erosion and deposition rates, thereby simulating topographic development backwards in time. The model is spatially evaluated, using detailed estimates for historical soil
- erosion and show that the model can simulate realistic soil redistribution patterns.
- Modelling mean annual sediment yield using a distributed approach
- Analyse de régression ; Bassin-versant ; Belgique ; Bilan sédimentaire ; Charge en suspension ; Echelle spatiale ; Erosion des sols ; Leuven ; Modèle ; Taux de sédimentation ; Vlaanderen
- Belgium ; Flanders ; Leuven ; Model ; Regression analysis ; Sediment budget ; Sedimentation rate ; Soil erosion ; Spatial scale ; Suspended load ; Watershed
- The AA. present a spatially distributed model for the calculation of sediment delivery to river channels (SEDEM : SEdiment DElivery Model) at a catchment scale (100 to 10 000 km2). The model was applied on several catchments in central Belgium
- Specific sediment yield in Tigray-Northern Ethiopia : assessment and semi-quantitative modelling
- Bassin-versant ; Bilan sédimentaire ; Erosion des sols ; Ethiopie ; Gestion de l'eau ; Lac artificiel ; Modèle ; Sédimentation
- Ethiopia ; Model ; Reservoir ; Sediment budget ; Sedimentation ; Soil erosion ; Water management ; Watershed
- Sediment deposition in reservoirs is a serious off-site consequence of soil erosion in Tigray. Field rating of catchment characteristics and the sediment yield data from the reservoir survey were used for calibration and validation of the models
- will have the same causal factors as the landslides initiated in the past. Significant model results were obtained, with pre-landslide hillslope gradient and 3 different clayey lithologies being important predictor variables. Receiver Operating
- Characteristics (ROC) curves and the Kappa index were used to validate the model. The results allow to conclude that the model is capable of predicting hillslope sections prone to landsliding.