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Runoff Features for Interrill Erosion at Different Rainfall Intensities, Slope Lengths, and Gradients in an Agricultural Loessial Hillslope

INRA, Science du Sol, Avenue De lab Pomme de Pin, B.P. 20619, Ardon, 45166 Olivet cedex, France

View larger version (20K): [in a new window]   Fig. 1. Histograms of depth of ponded water (cm) for 5-m long plots at 4 and 8% slope angles.

View larger version (23K): [in a new window]   Fig. 2. Directional variograms (0°, parallel to the contour lines; 45°; 90°, up and down slope and; 135°) of the depth of water ponded for experimental plots of 5-m length on 4 and 8% slope gradient positions during a 30-mm h-1 artificial storm.

View larger version (42K): [in a new window]   Fig. 3. Maps of the depth of water ponded performed by ordinary kriging using a data set a the nodes of an 0.2 by 0.5 m grid from a single experimental plot of 5-m length on 4 and 8% slope gradient positions during a 30-mm h-1 artificial storm and under steady-state conditions of runoff.