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  • This paper discusses the effects of water quality on the hydrological and erosion response of non-saline, non-sodic soils during simulated rain experiments. Two soils, a well-aggregated clay-rich soil developed on marine silty clay deposits
  • simulations are well suited to 1) analyse runoff-infiltration processes and sediment detachment within badlands, and 2) to establish the factors determining the hydrological and erosion response at interrill scale in badland areas. Rainfall simulations
  • and vegetated surfaces. Parent materials properties are discussed with respect to the initiation and development of different badlands processes. In particular, clay dispersivity at different depths in the sample sites is examined as a well-known controlling
  • has a model function both for our understanding as well as perspective on all landscape systems.
  • was applied on selected plots of a plant dataset to distinguish vegetation types and identify the indicator species of each different type. They then evaluated soil erodibility on the eroded biancana surfaces, regosols and well-developed vertisols. The AA. aim