To explore hydrodynamics characteristics of sand loess slope rill flow,scour experiments with three
slopes ( 3°、9°、15°) and five discharges ( 2. 4L /min、3. 6L /min、4. 8L /min、6. 0L /min、7. 2L /min) combination
were conducted. Results show that a power function relation is reasonable between the average flow velocity
and discharge in the range of slope in the experiments. The slope form of test belongs to the flat bed transition
zone,and Froude numbers roughly change between 0. 96 ~ 1. 30. The flow regime belongs to the rapids.
Reynolds numbers are mainly between 307 ~ 1,465,in the category of transition region. Flow regime is not
much related with slope,but is influenced by water infiltration,overland flow erosion. Analysis shows that
there was no significant relationship between resistance coefficient and Reynolds number,but mainly related to
slope median size or content of clay. Bed scour hole by the crust with the comprehensive roughness is the main
factors influencing the resistance.
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