Rainfall kinetic energy controlling erosion processes and sediment sorting on steep hillslopes: A case study of clay loam soil from the Loess Plateau, China

Rainfall kinetic energy (KE) can break down aggregates in the soil surface. A better understanding of sediment sorting associated with various KEs is essential for the development and verification of soil erosion models. A clay loam soil was used in the experiments. Six KEs were obtained (76, 90, 105, 160, 270, and 518J m(-2) h(-1)) by covering wire screens located above the soil surface with different apertures to change the size of raindrops falling on the soil surface, while maintaining the same rainfall intensity (90 +/- 3.5 mm h(-1)). For each rainfall simulation, runoff and sediment were collected at 3-min intervals to investigate the temporal variation of the sediment particle size distribution (PSD). Comparison of the sediment effective PSD (undispersed) and ultimate PSD (dispersed) was used to investigate the detachment and transport mechanisms involved in sediment mobilization. The effective-ultimate ratios of clay-sized particles were less than I, whereas that of sand-sized particles were greater than 1, suggesting that these particles were transported as aggregates. Under higher ICE, the effective-ultimate ratios were much closer to 1, indicating that sediments were more likely transported as primary particles at higher ICE owing to an increased severity of aggregate disaggregation for the clay loam soil. The percentage of clay-sized particles and the relative importance of suspension-saltation increased with increasing ICE when ICE was greater than 105 J m(-2) h(-1), while decreased with increasing ICE when ICE was less than 105 J m(-2) h(-1). A ICE of 105 J m(-2) h(-1) appeared to be a threshold level beyond which the disintegration of aggregates was severe and the influence of ICE on erosion processes and sediment sorting may change. Results of this study demonstrate the need for considering ICE-influenced sediment transport when predicting erosion. (C) 2014 Elsevier B.V. All rights reserved.