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  • Ten experimental sites of entire slope and sub-watershed and 580 flood events at 3 locations in the hilly areas of the Chinese Loess Plateau are involved in this study. The analysis at the intra-event time scale shows that the instantaneous sediment
  • that a single proportional function is adequate to fit the flow–sediment relationship for any entire slope or sub-watershed, where eroded sediments are primarily sourced, over a considerable areal extent unless soil property has changed or check dams
  • at 3 spatial scales (plot, sub-watershed and watershed) and 3 timescales (intra-event, inter-event and annual) for hilly loess areas. For comparison between the loess Plateau and other regions, they also fit the flow-sediment relationship using power