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A. Moss, P. Walker, J. Hutka (1980)
Movement of loose, sandy detritus by shallow water flows: An experimental studySedimentary Geology, 25
J. Savat (1977)
The hydraulics of sheet flow on a smooth surface and the effect of simulated rainfallEarth Surface Processes and Landforms, 2
W. David, C. Beer (1975)
Simulation of Soil Erosion — Part I. Development of a Mathematical Erosion ModelTransactions of the ASABE, 18
A. Moss, P. Green, J. Hutka (1982)
Small channels: Their experimental formation, nature, and significanceEarth Surface Processes and Landforms, 7
Dunne Dunne, Dietrich Dietrich (1980)
An experimental study of horton overland flow on tropical hillsopes: 1. Soil conditions, infiltration and frequency of runoffZeitschrift für Geomorphologie, Supplement Band, 35
G. Foster, L. Meyer, C. Onstad (1977)
A Runoff Erosivity Factor and Variable Slope Length Exponents for Soil Loss EstimatesTransactions of the ASABE, 20
M. Mosley (1974)
Experimental Study of Rill ErosionTransactions of the ASABE, 17
Foster Foster, Meyer Meyer, Onstad Onstad (1977)
An erosion equation derived from basic erosion principlesTransactions of the A. S. A. E., 20
Separation of rill and inter‐rill erosion is required in many of the soil erosion models currently being developed. The feasibility of basing the separation on the hydraulic properties of the flow and resultant sediment production is examined in a laboratory simulation of rill initiation and development. Four stages are identified in the process of rill formation; these are sheetflow, flowline development, micro‐rills, and micro‐rills with headcuts. There are significant differences in terms of flow characteristics between the stages, especially between sheetflow and flowlines, indicating the promise of this method for making a more precise distinction between rill and inter‐rill erosion.
Earth Surface Processes and Landforms – Wiley
Published: Sep 1, 1984
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