“…Ionic rare earth mine landslide belongs to shallow landslide and small landslide, mainly concentrated in high hilly terrain areas, landslide original terrain slope angle is concentrated in the range of 20 ~ 40 degrees, and the top of the landslide is mostly located in the foothill concave slope, the landslide is located in the strongly weathered residual accumulation and granite fully weathered layer, and the rainfall has a certain synchronization, the greater the rainfall with the injection of magnesium sulfate extraction solution, the bottom of the shallow well of liquid injection and fully weathered ore layer contact The stability of the slope on the datum surface is greatly affected and becomes landslide (Dianyu et al, 2023). In this paper, we monitored the earth pressure changes and fractures of two typical steep slopes, and the results showed that the steep slopes in magnesium sulfate extract leaching are easy to produce pushing landslides in the upper slope to the gentle slope system, and on the steep slopes with uniform slope, the intensity of magnesium sulfate extract is too large in the early stage is easy to produce pushing landslides, and the slope angle, slope height, the angle and the weight of internal friction of the fully weathered layer, during the magnesium sulfate extract leaching are taken as factors affecting the stability.…”