Raindrop and flow interactions for interrill erosion with wind-driven rain

被引:23
|
作者
Erpul, Gunay [1 ]
Gabriels, Donald [2 ,3 ]
Norton, L. Darrell [4 ]
Flanagan, Dennis C. [4 ]
Huang, Chi Hua [4 ]
Visser, Saskia [5 ]
机构
[1] Ankara Univ, Fac Agr, Dept Soil Sci & Plant Nutr, TR-06110 Ankara, Turkey
[2] Univ Ghent, Dept Soil Management, B-9000 Ghent, Belgium
[3] Univ Ghent, UNESCO Chair Eremol, B-9000 Ghent, Belgium
[4] Purdue Univ, USDA ARS, Natl Soil Eros Res Lab, W Lafayette, IN 47907 USA
[5] Dept Environm Sci, Land Degradat & Dev Grp, NL-6708 PB Wageningen Ur, Netherlands
关键词
Flow kinetic energy flux; interrill erosion; raindrop impact velocity vector; Water Erosion Prediction Project; wind-driven rain; SEDIMENT TRANSPORT CAPACITY; SPLASH-SALTATION; WATER EROSION; SAND DETACHMENT; OVERLAND-FLOW; SOIL-EROSION; IMPACT; PREDICTION; TUNNEL; MODEL;
D O I
10.1080/00221686.2013.778339
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
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 14m 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.
引用
收藏
页码:548 / 557
页数:10
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