Salinization of irrigation areas is a key environmental challenge faced by arid and semi-arid regions worldwide, and the complexity of natural environment and human activities increases the uncertainty of salinization distribution. This study takes the Xiaohaizi Irrigation Area in Kashgar, Xinjiang as the research location. Soil samples were collected before sowing and after harvesting in 2023 and analyzed. Using geostatistics and digital soil mapping techniques, the spatial distribution and temporal evolution of soil salinization in the region were finely characterized. The results showed that the soil salinization in Xiaohaizi Irrigation District was moderate to high, with mean salt contents of 8.29 g/kg in the 0-30 cm layer, 6.16 g/kg at 30-60 cm, and 4.80 g/kg at 60-100 cm before sowing, all indicating moderate to high salinity levels. The salt content showed a surface aggregation distribution with significant differences between different depths. The main ions that affect salinization are SO42-, Ca2+, Mg2+, Cl-, K+, and Na+. The 0-30 cm soil layer is mainly composed of mildly saline soil, and the degree of soil salinization decreases with the depth of the soil layer. After harvesting, the overall degree of salinization in the irrigation area intensified, and the spatial distribution of salinization was uneven. The degree of salinization was higher in the northwest and lower in the south. The impact of human activities on surface soil salinization is greater than that on deep soil. The areas where the degree of salinization in the 0-30, 30-60, and 60-100 cm soil layers undergoes transformation account for 57.18%, 33.15%, and 26.9%, respectively. This study reveals the complex dynamics of soil salinization in the Xiaohaizi irrigation area, providing scientific support for soil management and irrigation strategies in the region, and is of great significance for achieving sustainable development of oasis agriculture.