Abstract
Wind-driven rain (WDR) experiments were conducted to evaluate the interrill component of the Water Erosion Prediction Project model with a two-dimensional experimental set-up in a wind tunnel. Synchronized wind and rain simulations were applied to soil surfaces on windward and leeward slopes of 7, 15 and 20%. Since WDR fall trajectory varied with horizontal wind velocities of 6, 10, and 14 m s-1, magnitude of raindrop normal and lateral stresses on flow at the impact-flow boundary also changed and differentially directed lateral jets of raindrop splashes with respect to downward flows occurred. To account for interactions between raindrop impact and interrill shallow flow, a vector approach with kinetic energy fluxes of both raindrop splashes and flow were used and this resulted in greater correlations in predicting sediment delivery rates
Original language | English |
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Pages (from-to) | 548-557 |
Journal | Journal of Hydraulic Research |
Volume | 51 |
Issue number | 5 |
DOIs | |
Publication status | Published - 2013 |
Keywords
- sediment transport capacity
- splash-saltation
- water erosion
- sand detachment
- overland-flow
- soil-erosion
- impact
- prediction
- tunnel
- model