The relationship of soil loss by interrill erosion to slope gradient

The influence of slope gradient on erosion rate differs for rill and interr ill conditions. Rill erosion increases substantially more with increasing s lope gradient than interrill erosion. Combining the two erosion processes i nto single data sets led to the development of regression equations (e.g., USLE) that overestimated the effect of slope gradient on erosion rate for l ow slope gradients and short slopes. This study investigated the change in interrill erosion rate with slope gradient and examined its relationship to runoff velocity. A sandy loam (grey brown luvisol) was packed in 100 X 40 X 10 cm(3) soil trays and subjected to simulated rainfall for a period of 7 5 min. Rain-impacted flow erosion and downslope splash were monitored, and runoff velocity measurements were made at three positions within the flume. Downslope splash erosion never accounted for more than 20% of the total er osion. Rain-impacted flow erosion peaked early in the simulation then decre ased to a constant rate: erosion rate was therefore probably detachment-lim ited. For a constant runoff rate, rain-impacted flow erosion increased roug hly with the square root of slope gradient, as did the runoff velocity. Soi l loss was correlated (0.81) with runoff velocity under the experimental co nditions. (C) 1999 Elsevier Science B.V. All rights reserved.