Field measurements of interrill erosion under different slopes and plot sizes

Despite numerous studies, the effect of slope on interrill erosion is not c learly established. Several interactions exist between erosion parameters t hat are not taken into account under experimental laboratory measurements a nd results need to be validated in the field. The influence of slope steepn ess (2 to 8 per cent) on soil loss for a crusted interrill area and the det achment and transport processes involved in the interaction between slope, rain characteristics and plot size were investigated. Sediment discharge an d runoff rates were measured in bounded plots (1 m(2) and 10 m(2)) under na tural and simulated rainfall, allowing the analysis of a combination of det achment and transport processes at various scales in the field. Runoff rate increased from 20 to 90 per cent with increasing slope and rain intensity for both plot sizes, whereas sediment concentration increased from 2 to 6 g l(-1) with increasing slope only for the 10 m(2) plots. At the 1 m(2) scal e, erosion was transport-limited due to the reduced rain-impacted flow. Int eractions between slope angle and rain intensity were observed for detachme nt and transport processes in interrill erosion. Results show the importanc e of an adapted experimental set-up to get reference data for interrill ero sion model development and validation. Copyright (C) 2000 John Wiley & Sons , Ltd.