Abstract

Enumerating the relative proportions of soil losses due to rill erosion processes during monsoon and post-monsoon sea-son is a significant factor in predicting total soil losses and sediment transport and deposition. Present study evaluated the rill network with simulated experiment of treatments on varying slope and rainfall intensity to find out the rill ero-sion processes and sediment discharge in relation to slope and rainfall intensity. Results showed a significant relation-ship between the rainfall intensity and sediment yield (r = 0.75). Our results illustrated that due to increase in rainfall intensity represent the development of efficient rill network while, no rill was found with a slope of 20 ˚ and a rainfall intensity of 60 mm·h−1. The highest rill length was observed in plot E with 20 ˚ slope and 120 mm·h−1 rainfall intensity at 360 minutes. Positive and strong correlation (R2 = 0.734, P < 0.001) was observed between the cumulative rainfall intensity and sediment discharge. A longitudinal profile was delineated and showed that the depth and numbers of de-pressions amplified with time and were more prominent for escalating rainfall intensity for its steeper slopes. Informa-tion derived from the study could be applied to estimate longer-term erosion stirring over larger areas possessing paral-lel landforms.