On the characteristics and origin of closed depressions in loess-derived soils in Europe—a case study from central Belgium
Authors:
- Katleen GillijnsKGKatleen Gillijns
- Jean PoesenJean Poesen
- Jozef DeckersJDJozef Deckers
Abstract
No abstract availableKeywords
This publication has 8 references indexed in Scilit:
- Cold‐climate origin of the enclosed depressions and wetlands (‘spungs’) of the Pine Barrens, southern New Jersey, USAPermafrost and Periglacial Processes, 2001
- Soil losses due to harvesting of chicory roots and sugar beet: an underrated geomorphic process?CATENA, 2001
- Factors Controlling Sediment and Phosphorus Export from Two Belgian Agricultural CatchmentsJournal of Environmental Quality, 2001
- The mathematical modelling of salinity changes in ice and frozen soil as a result of thermal variationsAnnals of Glaciology, 2000
- Post-Carboniferous pre-Quaternary karstification in IrelandProceedings of the Geologists' Association, 2000
- Soil translocation by water erosion from agricultural cropland into wet depressions (morainic kettle holes)Soil and Tillage Research, 1998
- Genesis and development of a close depression near Toppenstedt south of HamburgZeitschrift für Geomorphologie, 1994
- Erosion‐sedimentation in a Closed Drainage Basin in Northwest IndianaSoil Science Society of America Journal, 1986