Soil Erosion on Abandoned Land in Andalusia: A Comparison of Interrill- and Rill Erosion Rates
Figure 2
Results of the rill experiments: sediment concentrations of the 6 runs of the 3 rill experiments with an inflow intensity of 9 L min−1 (a), sediment concentrations of the 8 runs of the 4 rill experiments with an inflow intensity higher than 250 L min−1 (b), runoff coefficients of all rill experiments (c), relative measurements errors of the sediment concentrations (separated in experiments with an inflow intensity of 9 L min−1 and an inflow intensity higher than 250 L min−1), and the runoff coefficients (d).