Abstract: A new apparatus for measuring the run off-on-out under simulated rainfall conditions was used to study the soil infiltration capacity under different rainfall intensities and vegetations in loess hilly region of southern Ningxia, with the relationships between soil waterstable aggregate content and soil stable infiltration rate under different vegetations analyzed. The results showed 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. Under the rainfall intensity of 20 mm·h^-1, the rainfall infiltration translation rate (RITR) was decreased in the order ofM. lupulina land>slope cropland>natural grassland>C. korshinskii land; while under the rainfall intensity 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 decreased with increasing rainfall intensity. After the reversion of cropland to grassland and forest land, and with the increase of re-vegetation, the amount of >0.25 mm soil aggregates increased, and soil infiltration capacity improved. The re-vegetation in study area effectively improved soil structure and soil infiltration capacity, and enhanced the utilization potential of rainfall on slope.

Key words: spring maize, yield, water-fertilizer coupling, semi-arid region of western Liaoning Province, shallow-buried drip irrigation