Abstract:A new apparatus for measuring the run off-on-out under simulated rai nfall conditions was used to study the soil infiltration capacity under differen t rainfall intensities and vegetations in loess hilly region of southern Ningxia , with the relationships between soil waterstable aggregate content and soil stable infiltration rate under different vegetations analyzed. The results showe d that the regression equations between rainfall duration and soil infiltration rate under different vegetations all followed y=a+be-cx, with R2 ranged from 0.9678 to 0.9969. With the increase of rainfall intensity, the soil stable infiltration rate on slope cropland decreased, while that on Medicago lupulina land, natural grassland, and Caragana korshinskii land increased. U nder the rainfall intensity of 20 mm·h-1, the rainfall infiltration trans lation rate (RITR) was decreased in the order ofM. lupulina land>slope cro pland>natural grassland>C. korshinskii land; while under the rainfall intens ity of 40 mm·h-1 and 56 mm·h-1, the RITR was in the sequence of M. lupulina land>natural grassland>slope cropland>C. korshinskii land, and dec reased with increasing rainfall intensity. After the reversion of cropland to gr assland and forest land, and with the increase of re-vegetation, the amount of >0.25 mm soil aggregates increased, and soil infiltration capacity improved. Th e re-vegetation in study area effectively improved soil structure and soil infi ltration capacity, and enhanced the utilization potential of rainfall on slope.