The paper aims to explore the crust types and the aggregates composition differences in micro-topographic soil attacked by raindrops. We studied the distribution characteristics, stability and soil erodibility of crust soil water-stable aggregates at different locations on slopes by simulated rainfall. The results showed that: (1) the water-stable aggregates of undisturbed soil, structural crust, sedimentary crust, transitional zone crust>0.25 mm were 37.28%, 43.58%, 36.69% and 40.34%, respectively; (2) taking the rainfall for 5 min as an example, the PAD of water-stable aggregates of undisturbed soil, structural crust, sedimentary crust and transitional zone crust were 51.49%, 46.00%, 62.76%, 51.02%, respectively; (3) the MWD of water-stable aggregates of undisturbed soil, structural crust, sedimentary crust and transitional zone crust were 0.15, 0.20, 0.14, 0.17 mm, respectively; (4) the erodibility K values of undisturbed soil, structural crust, sedimentary crust and transitional zone crust were 0.223, 0.200, 0.229, 0.205, respectively. The crust differences under micro-topography make the distribution of water-stable aggregates different, so the stability and erodibility of soil water-stable aggregates are different.