The characteristics of soil holding capacity for different shrub-grass patterns are important to research the mechanisms regulating vegetation on slopes. The objective of this study was to describe the characteristics and mecha-nisms of soil erosion and hydraulic parameters under differ-ent vegetation patterns in the Pisha sandstone area of Inner Mongolia on lands of 8° slope gradient. We carried out field scouring experiments on five different shrub-grass patterns as treatments, viz no shrubs (GL), shrubs on the upper part of the slope (SU), middle part of the slope (SM) and lower part of the slope (SL). We designated bare slope (BL) as the control. We employed three different water flow rates (15, 20, 30 L·min?1). Our results showed that the contribution of plant root systems to slope sediment reduction ranged from 64 to 84％. The root systems proved to be the main contributing factor to reduction of erosion by vegetation. The relationship between soil detachment rate, stream flow power, and flow unit stream power under different scour-ing discharge rates showed that soil detachment declined in rank order as: BL > GL > SU > SM > SL. The SL pat-tern had the lowest soil detachment rate (0.098 g·m?2·s?1), flow stream power (2.371 W·m?2), flow unit stream power (0.165 m·s?1) and flow shear stress (16.986 Pa), and proved to be the best erosion combating pattern. The results of deci-sion coefficient and path analysis showed that stream power was the most important hydraulic parameter for describing soil detachment rate. The combination of stream power and shear stress, namely Dr = 0.1ω ? 0.03τ ? 0.56 -(R2 = 0.924), most accurately simulated the soil detachment characteris-tics on slopes. Our study suggests that the risk of soil ero-sion can be reduced by planting shrub-grass mixes on these slopes. Under the conditions of limited water resources and economy, the benefit of sediment reduction can be maxi-mized by planting shrubbery on the lower parts of slopes.