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Par Collection Par Auteur- POESEN, J. (7)
- VANDEKERCKHOVE, L. (4)
- OOSTWOUD WIJDENES, D. (3)
- DE FIGUEIREDO, T. (2)
- BEUSELINCK, L. (1)
- CASALÍ, J. (1)
- DE LUNA, E. (1)
- DECKERS, J. (1)
- DONDEYNE, S. (1)
- GIRÁDEZ, J.V. (1)
- GOVERS, G. (1)
- GYSSELS, G. (1)
- GYSSELS, G. (1)
- KAFIRITI, E. (1)
- KOSMAS, C. (1)
- LÓPEZ, J.J. (1)
- MUGOCO, S. (1)
- MUYS, B. (1)
- NACHTERGAELE, J. (1)
- NACHTERGAELE, J. (1)
- Analyse de régression ; Bassin-versant ; Domaine aride ; Domaine semi-aride ; Erosion des sols ; Espagne ; Granada ; Lithologie ; Ravinement (1)
- Arid area ; Desertification ; Gully erosion ; Land use ; Mediterranean area ; Rill wash ; Soil erosion ; Spain ; Statistics ; Watershed (1)
- Arid area ; Europe ; Gully erosion ; Land use ; Lithology ; Mediterranean area ; Slope gradient ; Soil ; Soil erosion ; Soil properties ; Watershed (1)
- Arid area ; Granada ; Gully erosion ; Lithology ; Regression analysis ; Semi-arid area ; Soil erosion ; Spain ; Watershed (1)
- Bassin-versant ; Belgique ; Erosion des sols ; Holocène ; Loess ; Modèle ; Modèle numérique de terrain ; Paléogéographie ; Paléogéomorphologie ; Topographie (1)
- Bassin-versant ; Concept ; Domaine méditerranéen ; Erosion des sols ; Espagne ; Murcia ; Pente de versant ; Portugal ; Ravinement ; Ruissellement ; Seuil ; Sol cultivé (1)
- Bassin-versant ; Domaine aride ; Domaine méditerranéen ; Désertification ; Erosion des sols ; Espagne ; Espagne du Sud-Est ; Ravinement ; Ruissellement ; Statistique ; Utilisation du sol (1)
- Bassin-versant ; Domaine aride ; Domaine méditerranéen ; Erosion des sols ; Europe ; Lithologie ; Pente de versant ; Propriétés du sol ; Ravinement ; Sol ; Utilisation du sol (1)
- Bassin-versant ; Erodabilité ; Erosion des sols ; Impact ; Modèle mathématique ; Prévision ; Ravinement ; Topographie (1)
- Belgium ; Digital elevation model ; Holocene ; Loess ; Model ; Palaeogeography ; Palaeogeomorphology ; Soil erosion ; Topography ; Watershed (1)
- Concept ; Cultivated land ; Gully erosion ; Mediterranean area ; Murcia ; Portugal ; Rill wash ; Slope gradient ; Soil erosion ; Spain ; Threshold ; Watershed (1)
- Densité de population ; Distribution spatiale ; Erodabilité ; Erosion des sols ; Occupation du sol ; Plaine ; Plateau ; Propriétés du sol ; Ravinement ; Rugosité ; Seuil ; Tanzanie ; Topographie ; Unité paysagique (1)
- Erodibility ; Forecast ; Gully erosion ; Impact ; Mathematical model ; Soil erosion ; Topography ; Watershed (1)
- Erodibility ; Gully erosion ; Land utilisation ; Landscape unit ; Plain ; Plateau ; Population density ; Roughness ; Soil erosion ; Soil properties ; Spatial distribution ; Tanzania ; Threshold ; Topography (1)
- Characteristics and controlling factors of bank gullies in two semi-arid mediterranean environments (1)
- Exploring the role of topography in small channel erosion (1)
- Gully erosion in South Eastern Tanzania : spatial distribution and topographic thresholds (1)
- Reconstructing ancient topography through erosion modelling (1)
- Short-term bank gully retreat rates in Mediterranean environments (1)
- Thresholds for gully initiation and sedimentation in Mediterranean Europe (1)
- Topographical thresholds for ephemeral gully initiation in intensively cultivated areas of the Mediterranean (1)
- In this paper, 2 topographic indices, closely related to mathematical expressions suggested by different AA. are used to characterize the influence of watershed topography on gully erosion. The AS1 index is defined as the product of watershed area
- the topographic indices and the volume of eroded soil.
- Topographical thresholds for ephemeral gully initiation in intensively cultivated areas of the Mediterranean
- and topographical, lithological, land-use and climatic factors.
- Gully erosion in South Eastern Tanzania : spatial distribution and topographic thresholds
- of a landscape to gully erosion. Two important components of gully erosion studies are the prediction of where gullies begin and where they end. To address some of these issues, topographical thresholds for gully initiation and sedimentation in 6 different
- characteristics, such as topographical parameters, material properties and climate. The ultimate goal is to identify the most important controlling factors of past and present bank gully erosion. 55 active bank gullies formed in different lithologies by various
- 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