Luk S H, Cai Q G. Laboratory experiments on curst and rainsplash erosion of loess soils, China. Catena, 1990, 17: 261~276.
[6]
De Ploey J, Savat J, Moeyersons J. The differential impact of some soil loss factors on flow, runoff creep and rainwash. Earth Surface Processes and Landforms, 1976, 1: 151~161.
[7]
Slattery M, Bryan R B. Hydraulic condition for rill incision under simulated rainfall: a laboratory experiment. Earth Surface Processes and Landforms, 1992, 17: 127~146.
[8]
Fox D M, Bryan R B, Price A G. The influence of slope angle on final infiltration rate for interrill conditions. Geoderma, 1997, 80: 181~194.
[9]
Mah M G C, Douglas L A, Ringrose-voase A J. Effects of crust development and surface slope on erosion by rainfall. Soil Science, 1992, 154: 37~43.
[10]
Yair A, Raz-Yassif N.Hydrological processes in a small arid catchment: scale effects of rainfall and slope length. Geomorphology, 2004,61: 155~169.
[11]
Van de Giesen N, Stomph T J, de Ridder N. Surface runoff scale effects in West African watersheds: modeling and management options. Agriculture Water Management, 2005, 72:109~130.
Liu B Y, Nearing M A, Shi P J, et al. Slope length effect on soil loss for steep slopes. In: Stott D E, Mohtar R H, Steinhardt G C (eds.), sustaining the global farm. Selected papers from the 10th international soil conservation organization meeting held May 24-29, 1999 at Purdue University and the USDA-ARS National Soil Erosion Research Laboratory. 2001. 784~788.
[19]
吴发启, 范文波. 坡耕地结皮形成的影响分析. 水土保持学报,2002,16(1):33~36.
[20]
Kirkby M J, Chorley R J. Overland flow, throughflow and erosion. Bulletin of the International Association Scientific Hydrology, 1967, 12: 5~21.
[21]
Morin J, Benyamini Y. Rainfall infiltration into bare soils. Water Resources Research, 1977, 13: 813~817.
[22]
Xu J X. Hyperconcentrated flows in the slope-channel systems in gullied gullied areas on the Loess Plateau, China. Geografiska Annaler, 2004, 86: 349~366.
[23]
Lal R. Soil degradative effects of slope length and tillage methods on alfisols in western Nigeria. I. Runoff, erosion and crop response. Land Degradation and Development, 1997, 8:201~219.
[24]
Joel A, Messing I, Seguel O, et al. Measurement of surface, water runoff from plots of two different sizes. Hydrological Processes, 2002, 16: 1467~1478.
[25]
Sharma K, Singh H, Pareek O. Rain water infiltration into a bar loamy sand. Hydrological Sciences Journal, 1983, 28: 417~24.
[26]
Esteves M, Lapetite J M. A multi-scale approach of runoff generation in a Sahelian gully catchment: a case study in Niger. Catena, 2003, 50: 255~271.
[27]
Julien Y P, Moglen G E.Similarity and length scale for spatial varied overland flow. Water Resources Research, 1990,26: 1819~1832.
[28]
Poesen J.The influence of slope angle on infiltration rate and Hortonian overland flow volume. Zeitschriftfur. Geomorphologie, 1984,49: 117~131.
[29]
Fox D M, Bryan R B, Price A G.The influence of slope angle on final infiltration rate for interrill conditions. Geoderma, 1997,80: 181~194.
[30]
Stomph T J, Ridder N D, Steenhuis T S, et al. Scale effect of hortonian flow and rainfall-runoff dynamics: laboratory validation of a process-based model. Earth Surface Processes and Landforms, 2002, 27: 847~855.
