Fig. 4. Specific erosion (Es in g m−2) as a function of maximal discharge over a 1-min period (Q1max in L s−1) for the 18 events analyzed for the NT field (non-tilled field, top); the T field (tilled field, middle) and the catchment scales (down).
Fig. 4. Specific erosion (Es in g m−2) as a function of maximal discharge over a 1-min period (Q1max in L s−1) for the 18 events analyzed for the NT field (non-tilled field, top); the T field (tilled field, middle) and the catchment scales (down).