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in the field. Test results of the PWRS are very satisfactory. The analysis presented in this study suggests in particular very good reproducibility of wind and rain conditions. The PWRS should therefore be a useful device for comparative in situ soil erosion
measurements in the field and support the gathering of quantitative data on the relative importance of soil detachment rates between wind and water erosion, as well as windless and wind-driven rainfall.

The aims of this study are to identify variables as well as thresholds controlling different obstacle mark morphometries and to incorporate these into a simple statistical model. To achieve this, available field and laboratory studies on that topic
are reviewed first. Secondly, the results of laboratory flume experiments are analysed and compared with other available laboratory and field data. The results of this work have shown a significant relationship between the morphometry of fluvial obstacle marks

Sand-filled splash cups were used to study the erosivity of rainfall and throughfall in the humid subtropics of southeast China. The results showed that the splash cup measurements yielded precise and reproducible results both under open field
show that the erosive power of throughfall drops is 2.59 times higher compared to the open field. Moreover, the results show that the erosion potential under forest is related to the forest structure, especially height and canopy cover, and is species

Field experiments for understanding and quantification of rill erosion processes

and deposition model EROSION 2D/3D under field conditions. Based on the model parameters “skinfactor, soil resistance to erosion and surface roughness” the experimental approach is described exemplarily. The experimental results show that results from large-scale

One goal of this study was to assess the suitability of a novel field hybrid rainfall simulator (FH simulator) that combines characteristics of a spray nozzle and a drop former rain simulator (DF) for erosion research. Two soils with different

size distributions were used in the calibration trials performed by the same field worker. The collected runoff is stored in cubic tanks equipped with ten taps for sampling the suspension. When an erosive event occurs, the plot runoff volume is measured

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