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D. T. Favis-Mortlock, J. Boardman, A. J. Parsons and B. Lascelles, “Emergence and Erosion: A Model for Rill Initiation and Development,” Hydrological Processes, Vol. 14, No. 11-12, 2000, pp. 2173-2205. doi:10.1002/1099-1085(20000815/30)14:11/12<2173::AID-HYP61>3.0.CO;2-6

has been cited by the following article:

• TITLE: Developments of Rill Networks: An Experimental Plot Scale Study

  AUTHORS: Pravat Kumar Shit, Gouri Sankar Bhunia, Ramkrishna Maiti

  KEYWORDS: Rill Network; Slope Gradient; Rainfall Simulation; Sediment Yield

  JOURNAL NAME: Journal of Water Resource and Protection, Vol.5 No.2, February 4, 2013

  ABSTRACT: Enumerating the relative proportions of soil losses due to rill erosion processes during monsoon and post-monsoon season 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 erosion processes and sediment discharge in relation to slope and rainfall intensity. Results showed a significant relationship 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 depressions amplified with time and were more prominent for escalating rainfall intensity for its steeper slopes. Information derived from the study could be applied to estimate longer-term erosion stirring over larger areas possessing parallel landforms.