Soil erodibility reflects the soil effect on the detachment process by rainfall and runoff; an evaluation of this parameter for single storm events was carried out using natural runoff plot data collected for two rainfall seasons in northern Iraq. The region is characterized by a semiarid Mediterranean-type climate with normal rainfall intensity below 20 mm/h and dominant sheet erosion on agricultural land. The plots were three 30 × 3 m and three 10 × 3 m, in fallow, situated on a 6% uniform slope; the soil at the site has a silty clay loam texture and belongs to the Calciorthid suborder. Sheet erosion rate was assumed linearly proportional to the storm power and the sheet flow power; a steady-state turbulent and kinematic sheet flow was also assumed. The results indicated a dominant detachment by rainfall with a substantial variability in storm by storm calculated sheet erodibility. The two-parameter lognormal probability distribution fitted the obtained sheet erodibility values reasonably well. Using this probability distribution, a representative sheet erodibility value of 0.056 × 10−3kg/J was obtained for use at the experimental site.
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Research Article| January 16 2013
A sheet erodibility parameter for water erosion modeling in regions with low intensity rain
Mohammad H. Hussein
1Department of Soil and Water, College of Agriculture, Babylon University, Hilla-Iraq
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Hydrology Research (2013) 44 (6): 1013–1021.
January 28 2012
November 02 2012
Mohammad H. Hussein; A sheet erodibility parameter for water erosion modeling in regions with low intensity rain. Hydrology Research 1 December 2013; 44 (6): 1013–1021. doi: https://doi.org/10.2166/nh.2013.029
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